Chapter 10. Sensors

Table of Contents

10.1. Sensors for Wind Resource Assessment and Wind Farm Monitoring
10.2. Sensors for Solar Resource Assessment
10.3. Other Sensors for Meteorological Purposes
10.4. Devices for Electrical Measurements
10.5. Research Applications
10.6. Anemometers
10.6.1. Thies First Class Advanced X
10.6.2. Propeller Anemometer Young
10.7. Wind Vanes
10.7.1. Digital Wind Vanes TMR
10.7.2. Wind Vanes with Potentiometer
10.7.3. Wind Vanes connected to RS485-M
10.8. Ultrasonic Anemometers
10.8.1. NMEA MWV V 2.0
10.8.2. Thies Ultrasonic Configuration Options
10.8.3. Lufft UMB Configuration Tool
10.8.4. Gill Wind Configuration Tool
10.9. Weather and Environmental Integrated Monitoring Stations
10.10. Temperature Humidity Sensors
10.10.1. Resistance Temperature Detectors (RTD) / Pt100 / Pt1000
10.10.2. Temperature Humidity Sensors connected to RS485-M
10.11. Barometric Pressure Sensors
10.11.1. Barometric Pressure Sensors connected to RS485-M
10.12. Solar Sensors
10.12.1. Pyranometers
10.12.2. Delta-T Sunshine SPN1
10.12.3. Pyrheliometers
10.12.4. Sunshine Duration Sensors
10.12.5. Solar Trackers
10.12.6. Rotating Shadowband Irradiometer
10.12.7. Reference Cell
10.12.8. RS485 communication specifications
10.13. Precipitation Sensors
10.13.1. Rain Gauge
10.13.2. Laser Precipitation Monitors
10.14. Multifunction Transducer, Power Meters and other Electrical Measurement Devices
10.14.1. Sineax CAM Measuring Unit
10.15. Remote Sensing
10.15.1. ZephIR 300 Lidar
10.16. Bats Detection
10.16.1. Song Meter SM3BAT
10.17. Lightning Detector
10.17.1. SG1000 Lightning Detector
10.18. Soil Water Content
10.19. Soiling Measurement
10.19.1. Atonometrics RDE300
10.19.2. Ammonit Soiling Measurement Kit SD2100
10.19.3. Kipp & Zonen DustIQ
10.20. Other RS485 Sensors
10.20.1. RS485 Multiplexer
10.20.2. Configuring generic Modbus RTU sensors

Meteo-40 data loggers are designed for installation in wind and solar measurement campaigns. Thus the data logger is compatible with all relevant sensor types. Depending on the data logger type a different number of sensors can be connected to analog voltage, pulse/counter, digital/serial/status as well as analog current, current source and RS485 channels. See also Chapter 11, Channels and Section 1.3, “Meteo-40 Series”.

Depending on the measurement campaign different sensors are required. Find below a list of measurement instruments for wind measurement and solar measurement purposes as well as a list of other meteorological sensors and different measurement devices.

[Note]Note

If the sensor, you want to connect, is not listed in this manual, refer for technical details and connection plans to the data sheets on the Ammonit website or contact our sales team (+49-30-6003188-0 or ).

10.1. Sensors for Wind Resource Assessment and Wind Farm Monitoring

In order to evaluate the wind conditions at a specific location, various measurements for wind resource assessment are required. According to IEC 61400-12-1 horizontal wind speed, wind direction as well as air density have to be measured. Wind energy is calculated as follows:

Equation 10.1. Calculation of Wind Energy [P]

P = 1/2ρ × A × v³

(where A is the area; ρ is the air density, ρ = p / (R • T), being p the air pressure, T the air temperature and R the gas constant; v is the wind speed)

Therefore, wind speed (v) is the most important parameter, as wind energy (P) is proportional to the cube of wind speed. Δ1% wind speed ≈ Δ3% wind energy

The following sensors are crucial for wind site assessment:

Table 10.1. Sensors for Wind Measurement

SensorDescriptionLink
Anemometer (wind speed)
  • Most important parameter for wind measurement

  • Wind energy is proportional to the cube of wind speed

  • Install calibrated cup anemometers or calibrated ultrasonic anemometers

  • Heated sensors are recommended for measurements in cold climates

[Note]Note

Vertical wind speed measurement for turbulence and wind turbine load analysis with 3D ultrasonic or propeller anemometer.

Section 10.6, “Anemometers”(Anemometers)

Section 10.8, “Ultrasonic Anemometers”(Ultrasonics)

Section 10.6.2, “Propeller Anemometer Young”(Propeller Anemometer)

Wind vane (wind direction)
  • Important parameter for wind farm micrositing

  • Ultrasonic anemometers also determine the wind direction

Section 10.7, “Wind Vanes”(Wind vanes)

Section 10.8, “Ultrasonic Anemometers”(Ultrasonics)

Temperature / Humidity sensor
  • Important parameters for air density calculation

  • Wind energy is linear proportional to the inverse of air temperature in K

  • Measurement of relative humidity recommended at high temperatures acc. to IEC

  • Combined air temperature and relative humidity sensors available

Section 10.10, “Temperature Humidity Sensors”

Barometric pressure sensor
  • Important parameter for air density calculation

  • Wind energy is linear proportional to air pressure

Section 10.11, “Barometric Pressure Sensors”
Ultrasonic anemometer
  • Evaluate horizontal wind speed and direction; 3D ultrasonics measure vertical wind speed for turbulence analysis

  • Recommended for measurements in cold climates, as ultrasonic anemometers do not have moving parts and can be fully heated

Section 10.8, “Ultrasonic Anemometers”

10.2. Sensors for Solar Resource Assessment

Certain solar measurements are necessary to design profitable solar power plants. Refer to the Ammonit website to learn more about solar measurement systems. Depending on application (e.g., PV, CSP, CPV) and size of the solar power plant different measurements are crucial.

Insolation combines Direct Normal Irradiation (DNI) and Diffuse Horizontal Irradiance (DHI). Both are linked according to the formula for Global Horizontal Irradiation (GHI):

Equation 10.2. Calculation of Global Horizontal Irradiation

GHI [W/m²]= DHI [W/m²]+ DNI [W/m²]× cos(θ)

(where θ is the solar zenith angle)

On a sunny day the insolation is 100 % GHI, 20 % DNI and 80 % DNI·cos(θ).

Table 10.2. Sensors for Solar Measurement

SensorDescriptionLink
Pyranometer
  • Measures GHI (Global Horizontal Irradiation), if installed horizontally

  • Measures GTI (Global Tilted Irradiation), if installed tilted as PV panel

  • Measures DHI (Diffuse Horizontal Irradiation), if shaded by a shadow ball or shadow ring (installation on sun tracker)

Section 10.12.1, “Pyranometers”
Pyrheliometer
  • Measures DNI (Direct Normal Irradiation) and has to be installed on a sun tracker to follow the position of the sun on the sky

Section 10.12.3, “Pyrheliometers”
Sunshine Duration sensor
  • Indicates the sunshine status as defined by WMO (sunshine = direct irradiation exceeds the level of 120 W/m²)

Section 10.12.4, “Sunshine Duration Sensors”

Solar Tracker
  • Capable to orient a payload towards the sun. Can be combined with different solar sensors to measure solar radiation global, direct and diffuse components.

Section 10.12.5, “Solar Trackers”

Soiling Measurement
  • Soiling and Irradiance Measurement Systems collect critical data for evaluating PV array performance.

Section 10.19, “Soiling Measurement”


Besides measuring the solar conditions at the site of the planned solar power plant, some additional measurements might be necessary to design the solar power plant, i.e., wind speed, wind direction, air temperature, relative humidity as well as air pressure (see Table 10.1, “Sensors for Wind Measurement”). In some cases soiling detectors and precipitation sensors are required.

10.3. Other Sensors for Meteorological Purposes

There are several sensors, which are not mandatory for wind and solar resource assessment, but provide important parameters for ground construction and other influential conditions, e.g., precipitation sensors.

Table 10.3. Sensors for Meteorological Purposes

SensorDescriptionLink
Precipitation Rain Gauge
  • Measures the amount of precipitation (rain gauge)

Section 10.13, “Precipitation Sensors”

Laser Precipitation Monitor
  • Calculates SYNOP code (Surface Synoptic Observations)

  • Measures intensity of total precipitation

  • Measures intensity of liquid precipitation

  • Measures intensity of solid precipitation

  • Calculates the amount of precipitation

Section 10.13.2, “Laser Precipitation Monitors”


10.4. Devices for Electrical Measurements

Meteo-40 can be used to connect power meters, multifunction transducers or other electrical measurement devices, e.g., for power curve measurement.

Table 10.4. Electrical Measurement Devices

DeviceDescriptionLink
Multifunction Transducer
  • Also power meters or measuring transducers

  • Measure average phase voltage, current, real and reactive power

Section 10.14, “Multifunction Transducer, Power Meters and other Electrical Measurement Devices”


10.5. Research Applications

Meteo-40 is also used for research applications. A large and always growing list of formulas, developed and tested in collaboration with specialists, is included in the Evaluation Helper. For a complete list of the available formulas see Section 5.3.1, “Evaluation Helper”. Thanks to the Evaluation Helper, it is possible to apply a linear formula to a live measured data for later calculation of the standard statistics on this value. Most formulas combine different measurements and constants, like the air density, the covariance or a plain additon. Some special statistics related to turbulences analysis like Obukhov lenght or turbulence intensity can also be configured. The resulting value will be included in the statistics files.

In some research projects, a higher measurement rate can be needed. Over the RS485 Master ( RS485-M) port, Meteo-40 offers the possibility to record data from one RS485 sensor with a maximum polling rate of 8 Hz. If more than one RS485 sensor is connected to RS485-M, a maximum polling rate of 1 Hz is available. For the analogue voltage channels Ax, analogue current ACx and digital channels Dx, the highest measurement rate is 8 Hz. Whereas for counter channels Cx and period measurement Px the maximum is 1 Hz.

10.6. Anemometers

Anemometers measure the horizontal wind speed (velocity). This parameter is crucial for any wind site assessment. Cup anemometers are the general standard type of anemometers. They are robust and resistant to turbulence and skew winds caused by masts and traverses. Each anemometer should be individually calibrated and equipped with a certified calibration report according to international standards (e.g., MEASNET). At least two anemometers have to be installed on a met mast. Most anemometers can be equipped with electronically regulated heating.

Refer to the Ammonit website to learn more about anemometer behavior and accuracy.

The wind speed (v) is determined by the linear function of the frequency (impulse) output (I):

Equation 10.3. Calculation of Wind Speed (v)

v [m/s]= slope [m]× I [(1/s)]+ offset [m/s]: I > 0; v [m/s]= 0 : I = 0

A counter value of 0 will always result in 0, i.e., the offset is ignored in this case.

For wind assessment campaigns it is required to perform an individual MEASNET calibration of each anemometer in a wind tunnel to achieve optimal accuracy. After calibration, use the values for slope and offset according to the calibration protocol.

Anemometers are connected to counter channels (Cx). Refer to Figure 13.11, “Electrical Connection Plan: Pulse Counter (Anemometer)” for the connection diagram. Further details about counter channels can be found in Section 11.2, “Connecting Sensors to Counter / Period Channels” and Section 12.2, “Electrical Characteristics”.

Anemometers can easily be configured in the Meteo-40 web interface via the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

Table 10.5. Overview Anemometers

SensorOrder-NoDescription
Thies Anemometer FCA X vibration extended - ModbusS11200 / S11200HSee Section 10.6.1, “Thies First Class Advanced X”
Thies Anemometer FCA X one-step calibration - Modbus See Section 10.6.1, “Thies First Class Advanced X”
Thies Anemometer FCA X inclination extended - ModbusS11200 / S11200HSee Section 10.6.1, “Thies First Class Advanced X”
Thies Anemometer FCA X - ModbusS11200 / S11200HSee Section 10.6.1, “Thies First Class Advanced X”
Thies Anemometer FCA X - ASCIIS11200 / S11200HSee Section 10.6.1, “Thies First Class Advanced X”
Thies Anemometer First Class AdvancedS11100/S11100H 
Thies Anemometer First ClassP6100H/P6100 
Thies Anemometer CompactS12100H 
Thies Anemometer ClassicP6121H 
Anemometer Vento First Class  
Vector L100 First ClassS14100/S14100H 
Risø P2546AS16100 
Vaisala Anemometer WAA 252S15100H 
Young Propeller Anemometer Model 27106TS17100See Section 10.6.2, “Propeller Anemometer Young”
NRG #40 AnemometerS18200C 
NRG #40 Anemometer linearS18200CPure linear formula
Second Wind C3  
Lambrecht Wind Professional 14522  
Young Wind MonitorS17200 
Met One 014 mini  
Generic Anemometer  
Generic Anemometer linear Pure linear formula for NRG anemometers
Generic Anemometer PM  

[Important]Important

If you plan to install anemometer NRG #40H (Hall Effect), anemometer Risø P2546A (Reed switch), anemometer Thies (if open drain is used), an external circuitry is needed. This can be solved by an external resistor or - more elegant - using an external module by Ammonit. The external modules allow adaption for many different types of sensors and provide stabilized and ripple-free voltage supply for the sensors. Refer to the data sheet and contact Ammonit for further details.

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

Meteo-40 saves all electrically measured values to the source data (see Section 6.7, “Access to Source Data”). The calculated wind speed in m/s is saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file contains for all active channels the electrical values according to the chosen statistical interval.

10.6.1. Thies First Class Advanced X

The anemometer Thies First Class Advanced X is a cups anemometer that can be connected to the RS485-M port and offers a list of aggregated informations like vibration frequency, inclination, corrected an uncorrected wind speed. Thanks to the digital communication over the RS485 bus, this suplementary information can synchronously be requested by Meteo-40.

The corrected wind speed (EC 61400-12-1 Edition 2.0 compliant) is the result of correcting the influence of the atmospheric pressure on the measured wind speed. Meteo-40 will acquire the measurement values of the lower table every second, including measured frequency, corrected and uncorrected wind speed and 3-axis vibration frequencies.

If a Modbus RTU implementation is used ('Thies FCA X - Modbus', 'Thies Anemometer FCA X vibration extended - Modbus' or 'Thies Anemometer FCA X inclination extended - Modbus'), the sensor will be uniquely identified on every CECS start by requesting its hardware ID, which will be written in the configuration file. The calibration table, applied to the measured frequency resulting on the uncorrected wind speed at the second position of the table, is requested and saved eitherways in the configuration file. If any changes are detected in either the hardware ID or the calibration table, it is reflected in the logbook, including the time stamp when the calibration was performed and the number of the calibration certificate.

[Important]Important

Due to the inherent time required in master/slave protocols like Modbus or Thies ASCII protocol, if you want to connect more than four RS485 sensors to the RS485-M bus and request the measurement value every second, it is not possible to request a long list of measurement data. Modbus protocol is optimizing the amount of data transmitted and you must use the plain version ('Thies FCA X - Modbus') in this case.

Table 10.6. Connecting Thies FCA X to Meteo-40

ModelChannel (Protocol)Measurement DataModbus Reg.Required Configuration
Thies FCA X vibration extended - Modbus RS485-M(Modbus RTU)

Wind speed corrected depending on the air pressure and calibration table (m/s)

Wind speed calculated with current calibration table (m/s)

Frequency (Hz)

Absolute atmospheric pressure (hPa)

Status byte

Vibration frequency X (Hz)

Vibration amplitude X (mg)

Vibration frequency Y (Hz)

Vibration amplitude Y (mg)

Vibration frequency Z (Hz)

Vibration amplitude Z (mg)

35013

35049

35049

35021

35025

35037

35039

35041

35043

35045

35047

serial settings, address
Thies FCA X one-step calibration - Modbus RS485-M(Modbus RTU)

Wind speed calculated from measured frequency (m/s)

Housing interior temperature (°C)

Absolute atmospheric pressure (hPa)

Status byte

Vibration frequency X (Hz)

Vibration amplitude X (mg)

Vibration frequency Y (Hz)

Vibration amplitude Y (mg)

Vibration frequency Z (Hz)

Vibration amplitude Z (mg)

35049

35019

35021

35025

35037

35039

35041

35043

35045

35047

serial settings, address
Thies FCA X inclination extended - Modbus RS485-M(Modbus RTU)

Wind speed corrected depending on the air pressure and calibration table (m/s)

Wind speed calculated with current calibration table (m/s)

Frequency (Hz)

Housing interior temperature (°C)

Absolute atmospheric pressure (hPa)

Status byte

Inclination angle θ (°)

Inclination angle ρ (°)

Inclination angle φ (°)

35013

35049

35049

35019

35021

35025

35031

35033

35035

serial settings, address
Thies FCA X - Modbus RS485-M(Modbus RTU)

Wind speed corrected depending on the air pressure and calibration table (m/s)

Housing interior temperature (°C)

Absolute atmospheric pressure (hPa)

Status byte

35013

35019

35021

35025

serial settings, address
Thies FCA X - ASCII RS485-M(Thies)

Wind speed calculated with current calibration table (m/s)

Wind speed calculated with standard curve (m/s)

Wind speed corrected depending on the air pressure and calibration table (m/s)

Telegram 2

serial settings, address
Generic AnemometerCounter

Wind speed corrected/calculated (m/s)

Parameter FO=4 (see sensor's manual)

[Note]Note

Amplitude vibration unit ist mg, where 1g=9,81m/s².

10.6.2. Propeller Anemometer Young

The Propeller Anemometer measures horizontal and vertical wind speed. However, it is not classified according to MEASNET and IEC. The anemometer is widely used to measure vertical wind speed to analyse turbulences and the wind load of a turbine.

The anemometer uses a transducer, which converts linearly the rotational speed into DC voltage levels. Connect the sensor to the analog voltage channels (Ax) of your Meteo-40 data logger.

The anemometer can easily be configured in the Meteo-40 web interface via the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

Table 10.7. Overview Propeller Anemometer

SensorOrder-No
Propeller Anemometer Young 27106TS17100

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

Meteo-40 stores all electrically measured values to the source data (see Section 6.7, “Access to Source Data”). The calculated wind speed in m/s is saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file contains for all active channels the electrical values according to the chosen statistical interval.

10.7. Wind Vanes

Wind vanes indicate the horizontal wind direction. The evaluation of the wind direction enables the best possible positioning of wind turbines. It is essential that a wind vane covers an entire 360° degree radius - without north gap.

Meteo-40 data loggers are capable of using different types of wind vanes: Digital Wind Vanes and Analog (potentiometric) Wind Vanes. The Meteo-40 data logger comprises digital interfaces to connect several Digital Wind Vanes.

In addition to Digital Wind Vanes Meteo-40 data loggers are capable to make use of classical Analog Wind Vanes using a potentiometer. Ammonit suggests to use a five wire setup with two analog voltage channels to eliminate measurement errors caused by cable length and voltage drops in the supply voltage of the wind vane.

Furthermore, wind direction can also be recorded using wind vanes with data transmission via RS485-M bus.

10.7.1. Digital Wind Vanes TMR

Ammonit recommends installing digital wind vanes TMR to determine the wind direction. Wind vanes TMR deliver higher precision and are less susceptible to mechanical wear because of their solid state design. Ammonit offers wind vane Thies First Class TMR 10-bit serial-synchron and wind vane Thies Compact TMR 10-bit serial-synchron.

Table 10.8. Comparison of Wind Vane Accuracy

Wind VaneAccuracy
Thies Compact TMR± 1°
Thies Compact POT± 2°
Thies First Class TMR± 0.5°
Thies First Class POT± 1°

Each wind vane TMR requires one digital channel, whereas potentiometer wind vanes require two analog voltage channels each. By installing wind vanes TMR instead of wind vanes POT, analog voltage channels are available for other analog sensors, e.g., barometric pressure sensor, temperature or humidity sensors.

[Tip]Tip

Considering a measurement system with wind vanes TMR a smaller Meteo-40 model with less channels can be sufficient - for example Meteo-40S with 10 channels (4 analog voltage, 4 counter and 2 digital channels).

Wind vanes TMR are connected to digital channels (Dx). Refer to Figure 13.13, “Electrical Connection Plan: Digital Serial for Serial Wind Vane (Thies TMR)” for the connection diagram. Further details about digital channels can be found in Section 11.3, “Connecting Sensors to Digital Channels” and Section 12.2, “Electrical Characteristics”.

Wind vanes can easily be configured in the Meteo-40 web interface via the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

Table 10.9. Overview Wind vanes TMR

SensorOrder-No
Thies First ClassS21100H
Thies CompactS22100 / S22100H

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

10.7.2. Wind Vanes with Potentiometer

To determine the wind direction with a potentiometer wind vane, e.g., Thies First Class and Thies Compact, Ammonit recommends to use a five wire connetion between data logger and wind vane. This five wire connection eliminates voltage drops accross the connection cables and also eliminates the negative impact of voltage drops in the sensor's supply. Select the Generic Analog Wind Vane sensor type to connect any wind vane using this equation with the voltage range -10 V–+10 V.

The five wire connection method makes use of two consecutive analog voltage channels of the Meteo-40 data logger: A n, A n+1. A n records the total voltage of the potentiometer (voltage between vane supply and Ground), A n+1 measures the voltage between wiper and Ground. The following equation shows the calculation of the wind direction (D).

Equation 10.4. Calculation of the Wind Direction (D)

D [°]= (U An+1[V]/ U An[V]) × 360° + offset [°]

The Offset[°] must be filled when the wind vane has not been precisely aligned to the north, e.g., when the wind vane has been aligned to the mast. The offset specifies the angle between the North and the point the wind vane has been aligned to.

The Offset for each wind vane is configured in the Sensor Helper( see Section 5.1.2, “Sensor Helper”) of the Meteo-40 web interface.

Refer to Figure 13.7, “Electrical Connection Plan: Analog Voltage (Potentiometric Wind Vane)” for the connection diagram. Further details about analog voltage channels can be found in Section 11.1, “Connecting Sensors to Analog Voltage Channels” and Section 12.2, “Electrical Characteristics”

Table 10.10. Parameters for the configuration of potentiometric wind vanes

SensorOrder-NoOffset
Thies First ClassS21200H0° (if aligned to the North)
Thies CompactS22200 / S22200H0° (if aligned to the North)

[Important]Important

If potentiometric wind vanes, e.g., Thies First Class, Thies Compact, Vector W200P, Vector W200P/L, NRG #200P additional resistors for current limitation have to be used in the wiring setup. Contact Ammonit regarding further details about the accessory module!

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

Meteo-40 stores all electrically measured values to the source data ( Section 6.7, “Access to Source Data”). The calculated wind direction in ° (degree) is saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file contains the electrical values according to the chosen statistical interval for all active measurement channels.

10.7.3. Wind Vanes connected to RS485-M

Certain wind vanes have an RS485 interface. Meteo-40 data loggers are capable to address up to eight smart sensors on the RS485-M bus.

[Important]Important

If you intend to connect more than one sensor via RS485-M, all connected sensors must use the same protocol and serial settings. Additionally, each ultrasonic sensor has to use a unique ID ( RS485 address), which has to be configured for the sensor. The transmission mode for all rs485-connected sensors has to be configured to half duplex. See Section 11.6, “Connecting Sensors to RS485-M”.

Wind vanes can easily be configured in the Meteo-40 web interface via the Sensor Helper(see Section 5.1.2, “Sensor Helper”). See Table 10.11, “Configuration of RS485 Wind Vanes” for the configuration of RS485 wind vanes.

Table 10.11. Configuration of RS485 Wind Vanes

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Thies Wind Vane TMR RS485ThiesTelegram 3

Mx_1: Wind direction

Serial settings, Address, Half duplex mode
Thies Wind Vane First Class RS485ThiesTelegram 3

Mx_1: Wind speed

Mx_2: Wind direction

Serial settings, Address, Half duplex mode
Thies Wind Vane 8-bit parallel via ICP DAS I7051DCONRS485 module to connect two Thies 8-bit parallel wind vanes

Mx_1: Wind direction vane DI: 0–7

Mx_2: Wind direction vane DI: 8–15

Same configuration as for Meteo-32 (Serial settings: 38400 8N1, Address: 6, Checksum: disabled)

Meteo-40 stores all measured values to the source data ( Section 6.7, “Access to Source Data”). The wind direction in ° (degree) is saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

10.8. Ultrasonic Anemometers

Ultrasonic anemometers must be connected to the RS485-M port (see Section 11.6, “Connecting Sensors to RS485-M”). 2D ultrasonic anemometers measure horizontal wind speed, wind direction and acoustic virtual temperature. 3D ultrasonic anemometers also measure the vertical wind velocity, which is important for turbulence and wind load calculations.

[Important]Important

If you intend to connect more than one sensor via RS485-M, all connected sensors must use the same protocol and serial settings. Additionally, each ultrasonic sensor has to use a unique ID ( RS485 address), which has to be configured for the sensor. The transmission mode for all rs485-connected sensors has to be configured to half duplex. See Section 11.6, “Connecting Sensors to RS485-M”.

The following ultrasonic anemometers are includded in the Meteo-40 sensor helper for easy configuration. More Modbus sensors can be configured as Other sensor.

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Thies 2D AnemometerThiesTelegram 3

Mx_1: Wind speed

Mx_2: Wind direction

Mx_3: Acoustic virtual temperature

serial settings, address, half duplex mode, scalar averaging over 1 s
Thies 3D AnemometerThiesTelegram 3

Mx_1: Wind speed azimuth

Mx_2: Wind direction azimuth

Mx_3: Wind speed elevation

Mx_4: Acoustic virtual temperature

serial settings, address, half duplex mode, scalar averaging over 1 s
NMEA - Thies Compact AnemometerNMEATelegram 3

Mx_1: Wind direction

Mx_2: Wind speed

serial settings, address, NMEA protocol, half duplex mode, scalar averaging over 1 s
Lufft 2D VENTUS-V200A-UMBModbus RTUinput registers 14 and 25

Mx_1: Wind direction

Mx_2: Wind speed

serial settings, address, Modbus RTU protocol, parity none
Gill Wind Master (Pro) 3D AnemometerGillMode 4

Mx_1: Wind direction azimuth

Mx_2: Wind speed azimuth

Mx_3: Wind speed elevation

Mx_4: Sonic temperature (if activated)

serial settings (B5: 38400 bps, 8N1), address (default Q), averaging inactive (G0), sampling rate 20 Hz (P8), polar polled (M4), output format CSV (O1), Sonic temperature activated (A3)
Gill Wind Observer / WindSonic 2D AnemometerGillMode 4

Mx_1: Wind direction azimuth

Mx_2: Wind speed azimuth

Mx_3: Sonic temperature (if activated)

serial settings (B5: 38400 bps, F1: default 8N1), address (default A), averaging inactive (G0), sampling rate 20 Hz (P8), polar polled (M4), output format CSV (O1), Sonic temperature optionally activated (A2)
Vaisala WMT700 NMEA MWVNMEAWMT700 NMEA MWV Data Message

Mx_1: Wind direction

Mx_2: Wind speed

autoSend = 0 (automatic messages disabled), com2_protocol = 11 (WMT700 NMEA profile for serial port COM2 MWV protocol), com2_interf = 0 (RS-485 interface for serial port COM2), com2_delay = 10, wndUnit = 0 (m/s wind speed unit), address = WI (Weather Instruments), device identifier = II

10.8.1. NMEA MWV V 2.0

Supported NMEA telegram: $WIMWV,<dir>,<ref>,<spd>,<uni>,<sta>*<chk><CR><LF>

  • <dir>: Wind direction xxx.x

  • <ref>: Reference R = relative

  • <spd>: wind speed xxx.x

  • <uni>: Wind speed unit M = m/s

  • <sta>: Status A = valid

  • <chk>: Checksum (8-bit XOR, excluding $ and *)

  • <CR>: Carriage return code, ASCII 0DH

  • <LF>: Line feed code, ASCII 0AH

10.8.2. Thies Ultrasonic Configuration Options

Before connecting any Thies sensor to the RS485-M port, it has to be configured. Three Thies ultrasonic types are available: 2D compact, 2D and 3D. You can use the Thies Device Utility software to configure your sensors ( Thies Device Utility software).

Ammonit recommends configuring Thies ultrasonic sensors as follows:

Required settings

  • Half duplex for transmission mode

  • Unique ID for each sensor connected to the bus

  • Heating ON/OFF

Further Thies-specific settings

  • Voltage threshold for heating suppression: 17 V (HC=17)

  • Serial settings: 38400 bps, 8N1 (data format)

  • Average mode: scalar-averaged velocity and vectorial-averaged angle (AM=2)

[Tip]Tip

For more information about Thies acoustic virtual temperature, see sensor's manual.

10.8.3. Lufft UMB Configuration Tool

Before connecting any Lufft sensor to Meteo-40, it has to be configured. Download and install the software UMB-Config-Tool and follow the next steps:

  1. Power on the sensor.

  2. Connect sensor's A-, B+ to your computer using RS485 to USB or RS232 adapter.

  3. Start Config-Software-UMB and setup the connection in the EditConnection settings menu.

  4. In order to configure the sensor, switch all sensors temporarily to UMB protocol in the Options menu (follow instructions).

  5. Add the new sensor in the EditSensor menu. Select the appropriate type from the list and ID (default 1). Do not exit this menu, press Configure to access the sensor configuration.

  6. Load the profile from the sensor (press the button again, if it does not respond). Select the tab with sensor type name and configure as described in the table above (see Section 10.8, “Ultrasonic Anemometers”).

  7. Store profile on sensor to apply the configuration changes to the sensor. Save the profile also to your disk to keep a copy of the sensor configuration.

  8. Close the configuration program, disconnect and power off the sensor. Connect the sensor to the data logger and power on the sensor.

  9. Add the sensor to the sensor list of the data logger in the MeasurementSensors menu, applying the same configuration.

10.8.4. Gill Wind Configuration Tool

Before connecting any Gill sensor to Meteo-40, it must be configured accordingly.

  1. Download and install Gill Wind Com.

  2. Use the Wizard tool to change from the default configuration all parameters specified in the upper table (see Section 10.8, “Ultrasonic Anemometers”).

  3. Use a different address for each unit connected to the RS485-M. It is recommended that letters A to F, K, M, N, and P are not used since they can appear in a data string and might result in erroneous poll responses.

  4. Do not forget to save the configuration report in the Tools menu.

  5. Close the configuration program, disconnect and power off the sensor. Connect the sensor to the data logger and power on the sensor.

  6. Add the sensor to Meteo-40 sensors list in the MeasurementSensors menu, applying the same configuration.

[Note]Note

Any wind magnitude lower than defined by sensor's parameter K (default 0.050 m/s) will omit the wind direction.

[Important]Important

Gill Wind Master sensors with firmware v7.01 can be networked with other Wind Master units on a 2-wire RS485 bus. Units with older versions cannot be networked.

10.9. Weather and Environmental Integrated Monitoring Stations

Weather and environmental stations are capable of measuring a large amount of athmospheric conditions in only one device. To acquire this data the preferred connection ist RS485. These sensors can be connected to the RS485-M port (see Section 11.6, “Connecting Sensors to RS485-M”).

[Important]Important

If you intend to connect more than one sensor via RS485-M, all connected sensors must use the same protocol and serial settings. Additionally, each ultrasonic sensor has to use a unique ID ( RS485 address), which has to be configured for the sensor. The transmission mode for all rs485-connected sensors has to be configured to half duplex. See Section 11.6, “Connecting Sensors to RS485-M”.

The following weather and environmental stations are includded in the Meteo-40 sensor helper for easy configuration. More Modbus sensors can be configured as Other sensor.

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Thies Clima Sensor USThiesTelegram 6

Mx_1: Wind speed

Mx_2: Wind direction

Mx_3: Temperature

Mx_4: Humidity

Mx_5: Air pressure

Mx_6: Brightness max. value

Mx_7: Direction of brightness

Mx_8: Precipitation status

Mx_9: Precipitation intensity

Mx_10: Precipitation sum

Mx_11: SYNOP

BR=384, DM=0, DT=0, TT=0, RD=5
Thies Clima Sensor US VDTHPThiesTelegram 2

Mx_1: Wind speed

Mx_2: Wind direction

Mx_3: Temperature

Mx_4: Humidity

Mx_5: Air pressure

BR=384, DM=0, DT=0, TT=0, RD=5
Lufft Weather station WSModbus RTU

input registers 10, 14, 22, 31 and 47

Mx_1: Relative humidity (act.)

Mx_2: Rel. air pressure (act.)

Mx_3: Wind direction fast

Mx_4: Air temperature (act.)

Mx_5: Wind speed fast

serial settings (38400 bps), address, Modbus RTU protocol, parity none
Lufft Weather station WS 502Modbus RTU

input registers 10, 14, 22, 27, 31 and 47

Mx_1: Relative humidity (act.)

Mx_2: Rel. air pressure (act.)

Mx_3: Wind direction fast

Mx_4: Global radiation (act.)

Mx_5: Air temperature (act.)

Mx_6: Wind speed fast

serial settings (38400 bps), address, Modbus RTU protocol, parity none
Lufft Weather station WS 300Modbus RTU

input registers 10, 14 and 31

Mx_1: Relative humidity (act.)

Mx_2: Rel. air pressure (act.)

Mx_3: Air temperature (act.)

serial settings (38400 bps), address, Modbus RTU protocol, parity none
Gill MaxiMet GMX600Modbus RTUregisters 2 to 20

Mx_1: Wind direction

Mx_2: Wind speed

Mx_3: Wind direction corrected

Mx_4: Air pressure

Mx_5: Humidity

Mx_6: Temperature

Mx_7: Dew point

Mx_8: Precipitation sum

Mx_9: Precipitation intensity

serial settings, address
TWS100 integrated dust monitoring sensorModbus RTUregisters 1 to 14

Mx_1: Wind direction

Mx_2: Wind speed

Mx_3: Temperature

Mx_4: Humidity

Mx_5: Air pressure

Mx_6: Precipitation sum

Mx_7: Global irradiance

Mx_8: UV Index

Mx_9: Noise

Mx_10: Particulate Matter PM₂.₅

Mx_11: Particulate Matter PM₁₀

averaging interval 1s, serial settings, address

10.10. Temperature Humidity Sensors

Temperature sensors measure the air temperature, while humidity sensors measure the air humidity. Both sensors are often applied in combination to reduce cost.

Temperature humidity sensors, e.g., Galltec Active KP, Galltec Active TP, have to be connected to analog voltage channels (Ax). Refer to Figure 13.4, “Electrical Connection Plan: Analog Voltage (Temperature + Humidity Sensor)” for the connection diagram.

The output signal (U) from the temperature sensor is proportional to the temperature (T) in °C.

Equation 10.5. Calculation of Temperature (T)

T [°C]= slope [°C/V]× U [V]+ offset [°C]

The output signal (U) from the humidity sensor is proportional to the humidity (RH) in %.

Equation 10.6. Calculation of Humidity (RH)

H [%]= slope [%/V] x U [V]

Slope and Offset are internal parameters of the sensor, which are important to calculate temperature (T) in °C and humidity (RH) in %. Both values are pre-configured in the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

[Note]Note

For more flexibility, when connecting the combined Galltec temperature and humidity sensor to Meteo-40, two different Galltec Active KP sensors are listed in the Sensor Helper(see Section 5.1.2, “Sensor Helper”). Two analog channels are needed and thus the order of the signals to be connected is selectable. "Galltec Thermo-Hygro Active KP" assigns the first analog channel to temperature and the second to humidity. As opposite, "Galltec Hygro-Thermo Active KP" assigns the first channel to humidity and the second to temperature.

Table 10.12. Parameters for the configuration of temperature humidity sensors

SensorOrder-NoSlopeOffset
Galltec Active KP (Temperature + Humidity)S52100
100 %/V (Humidity)
100 °C/V (Temperature)
0 % (Humidity)
-30 °C(Temperature)
Galltec Active TP (Temperature)S42100
100 °C/V
-30 °C

[Important]Important

If you install calibrated sensors, enter the values given in the calibration protocol.

Meteo-40 saves all electrically measured values in V to the source data ( Section 6.7, “Access to Source Data”). The calculated values for temperature (°C) and humidity (%) are saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file also contains for all active channels the electrical values according to the chosen statistical interval.

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

10.10.1. Resistance Temperature Detectors (RTD) / Pt100 / Pt1000

RTDs measure the temperature by correlating the resistance of the RTD element with temperature. Those sensors provide high accuracy and repeatability; the sensors are suitable for precision applications. RTDs use electrical resistance and require a power source to operate.

Platinum Resistance Thermometers (Pt100 / Pt1000) are classified according to DIN EN 60751 - see tolerance classes below.

Table 10.13. Tolerance Classes - Platinum Resistance Thermometers (Pt100)

Tolerance ClassTolerance in K
Class B1/3 DIN±(0.10 K + 0.0017 × [t])
Class A±(0.15 K + 0.002 × [t])
Class B±(0.30 K + 0.005 × [t])
Class 0.5±(0.50 K + 0.006 × [t])

Pt100 / Pt1000 sensors have to be connected to the analog voltage channel and the current source of Meteo-40 data loggers. The sensors can easily be configured via the Sensor Helper(see Section 5.1.2, “Sensor Helper”) in the Meteo-40 web interface.

Meteo-40 saves all electrically measured values in V to the source data ( Section 6.7, “Access to Source Data”). The calculated value for temperature ( °C) is saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file also contains for all active channels the electrical values according to the chosen statistical interval.

10.10.2. Temperature Humidity Sensors connected to RS485-M

Some available temperature humidity sensors have to be connected to the RS485-M bus of the Meteo-40 data logger. The sensors can easily be configured in the Meteo-40 web interface via the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

[Important]Important

If you intend to connect more than one sensor via RS485-M, all connected sensors must use the same protocol and serial settings. Additionally, each ultrasonic sensor has to use a unique ID ( RS485 address), which has to be configured for the sensor. The transmission mode for all rs485-connected sensors has to be configured to half duplex. See Section 11.6, “Connecting Sensors to RS485-M”.

Table 10.14. Data request for RS485 Temperature Humidity Sensors

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Galltec Thermo/Hygro KPC.MSModbus RTUregisters 0, 1, 3, 4

Mx_1: Temperature

Mx_2: Humidity

Fixed serial settings (19200 8N1)
Campbell Hygro/Thermo CS215SDI-12D0

Mx_1: Temperature

Mx_2: Humidity

External module needed (address, 19200 8N1, 120Ω termination). See SDI-12.

Meteo-40 saves all measured values to the source data ( Section 6.7, “Access to Source Data”). The values for temperature (°C) and humidity (%) are saved to the CSV file ( see Section 6.6.1, “Ammonit Meteo-40 specific details”).

10.11. Barometric Pressure Sensors

Barometric pressure sensors measure the air pressure. Air pressure and air temperature should be evaluated for an accurate wind site assessment. It is recommended including an air pressure sensor as part of a measuring system.

Barometric pressure sensors, e.g., AB60, AB100 and Vaisala PTB110, have to be connected to analog voltage channels (Ax). Refer to Figure 13.3, “Electrical Connection Plan: Analog Voltage (Temperature / Barometric Pressure Sensor)” for the connection diagram.

The output signal (U) from the barometric pressure sensor is proportional to the air pressure (P).

Equation 10.7. Calculation of Air Pressure (P)

P [mbar]= slope [mbar/V]× U [V]+ offset [mbar]

Slope and Offset are internal parameters of the sensor, which are important to calculate the air pressure in hPa. Both values are pre-configured for sensors listed in the library of the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

Table 10.15. Parameters for the configuration of barometric pressure sensors

SensorOrder-NoSlopeOffset
Ammonit AB60S3110060 mbar/V800 mbar
Ammonit AB100S31200100 mbar/V600 mbar
Vaisala PTB110.1S32300120 mbar/V500 mbar
Vaisala PTB110.2S32200100_mbar/V600_mbar
Vaisala PTB110.3S3210060 mbar/V800 mbar

PTB 110.1: pressure range 500..110hPa, output signal 0..5V

PTB 110.2: pressure range 600..110hPa, output signal 0..5V

PTB 110.3: pressure range 800..110hPa, output signal 0..5V

[Important]Important

If you install calibrated sensors, enter the values given in the calibration protocol.

Meteo-40 saves all electrically measured values in V to the source data ( Section 6.7, “Access to Source Data”). The calculated air pressure value in mbar is saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file contains for all active channels the electrical values according to the chosen statistical interval.

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

10.11.1. Barometric Pressure Sensors connected to RS485-M

Certain barometric pressure sensors have to be connected to the RS485-M bus of the Meteo-40 data logger. The sensors can easily be configured in the Meteo-40 web interface via the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

[Important]Important

If you intend to connect more than one sensor via RS485-M, all connected sensors must use the same protocol and serial settings. Additionally, each ultrasonic sensor has to use a unique ID ( RS485 address), which has to be configured for the sensor. The transmission mode for all rs485-connected sensors has to be configured to half duplex. See Section 11.6, “Connecting Sensors to RS485-M”.

Table 10.16. Data request for RS485 Barometric Pressure Sensors

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Thies Baro TransmitterThiesTelegramm 1

Mx_1: Air pressure

Mx_2: Temperature

serial settings, address

Meteo-40 saves all measured values to the source data ( Section 6.7, “Access to Source Data”). The air pressure value in hPa is saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

10.12. Solar Sensors

10.12.1. Pyranometers

Pyranometers measure the global horizontal radiation. They are also used as reference instruments thanks to their measurement precision. The use of this sensor is crucial for measurements with solar-powered applications.

Meteo-40 indicates for pyranometers the global horizontal irradiation (GHI).

Pyranometers, e.g., MS series of EKO Instruments or CMP series of Kipp & Zonen, have to be connected to analog voltage channels (Ax). Refer to Figure 13.2, “Electrical Connection Plan: Analog Voltage (Pyranometer)” for the connection diagram.

The output signal (U) from the pyranometer is proportional to the solar irradiance (E) in W/m².

Equation 10.8. Calculation of Solar Irradiance (E)

E [W/m²]= U [μV]/ Sensitivity [μV/[W/m²]]

Sensitivity is an internal parameter of the sensor, which is important to calculate the radiation in W/m². The value is given in the calibration certificate of the sensor.

[Note]Note

Some EKO pyranometers allow the internal configuration of the sensitivity value. In that case, you must introduce a sentivity of 1 μV/[W/m²] at the sensor helper.

Table 10.17. Pyranometers

SensorOrder-No
CMP 3S61100
CMP 6S61110
CMP 10S61130
CMP 11S61120
EKO ML-01S64350
EKO MS-40S64111
EKO MS-57S64211
EKO MS-60M ( RS485)S64160
EKO MS-80AS64150
EKO MS-80A over shuntS64150 and S82402
EKO MS-80M ( RS485)S64160
EKO MS-202 
EKO MS-802S64120
EKO MS-410S64130
EKO MS-602S64110
Kipp & Zonen CMP11S61120
Kipp & Zonen CMP6S61110
Kipp & Zonen CMP3S61100
Kipp & Zonen SMP10 ( RS485)S61430 / S61420
Hukseflux Pyranometer LP 02S63100
Hukseflux Pyranometer SR 11S63120
Hukseflux Pyranometer SR30 ( RS485) 
SP Lite2S61180
Silicon Irradiance Sensor MT 0-1VS68310 / S68320 / S68330
Silicon Irradiance Sensor MT 0-10VS68100
Silicon Irradiance Sensor MT 4-20mAS68110 / S68210
Silicon Irradiance Sensor SiS-13TC-TS68250
Li-Cor LI-200SZ 
ISET Solar Radiation Sensor 
Datasol MET Reference Cell ( RS485) 

Meteo-40 saves all electrically measured values in V to the source data ( Section 6.7, “Access to Source Data”). The calculated values for solar radiation are saved in W/m² to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file also contains for all active channels the electrical values according to the chosen statistical interval.

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

10.12.2. Delta-T Sunshine SPN1

The pyranometer Delta-T Sunshine SPN1 measures global horizontal and diffuse irradiation in W/m². It provides 2 analogue voltage outputs (Ax) for global and diffuse irradiation, and 1 digital output (Dx) for sunshine duration.

Additionally, Meteo-40 estimates the direct normal irradiation based on the values of global horizontal and diffuse irradiation according to the general formula: Global Horizontal Irradiation = Diffuse Horizontal Irradiation + Direct Normal Irradiation ⋅ cos(θ), where θ is the solar zenith angle

The order number for Delta-T Sunshine SPN1 is S65100.

[Important]Important

In order to estimate direct normal irradiation (DNI) and sun status, latitude and longitude of the measurement station have to be entered in the SystemAdministration menu (see also Section 4.2, “System Administration”).

If any estimated values should be included in the CSV statistics file, the values have to be selected in the DataStatistics menu under Select statistics(see also Section 6.3.1, “Configuring Statistics and CSV files”).

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

10.12.3. Pyrheliometers

Pyrheliometers are used to measure the direct irradiance emitted by the sun in a 5 degree angle. The sensors have to be connected to the analog voltage channels (Ax) of Meteo-40.

The output signal (U) from the pyrheliometer is proportional to the solar irradiance (E) in W/m².

Equation 10.9. Calculation of Direct Solar Irradiation (E)

E [W/m²]= U [μV]/ Sensitivity [μV/[W/m²]]

Sensitivity is an internal parameter of the sensor, which is important to calculate the irradiation in W/m². The value is given in the calibration certificate of the sensor.

The direct normal irradiation is the basic measurement from pyrheliometers. Additionally, Meteo-40 estimates DNI ⋅ cos(θ) and sun status based on the recorded values for direct normal irradiation. Sun status is calculated as defined by WMO (sun status is 1 if direct normal irradiation exceeds the level of 120 W/m², else 0). In order to estimate sun status and DNI ⋅ cos(θ), latitude and longitude of the measurement station must be entered in the SystemAdministration menu (see also Section 4.2, “System Administration”).

These sensors often include with built-in Pt100 sensor and a thermistor. The Pt100 sensor can be connected to a current source (see Section 11.5, “Connecting Sensors to Current Source”) of Meteo-40.

If the built-in Pt100 sensor should be connected to Meteo-40, pyrheliometer and Pt100 sensor have to be configured separately in the Sensor Helper: Pyrheliometer via sensor type Solar Sensors and Pt100 via sensor type Hygro/Thermo.

[Important]Important

Do not connect the thermistor to Meteo-40!

Table 10.18. Pyrheliometers

SensorOrder-No
EKO MS-56S64210
Kipp & Zonen CPH1S62210

[Important]Important

In order to estimate sun status and direct normal irradiation [DNI ⋅ cos(θ)], latitude and longitude of the measurement station must be entered in the SystemAdministration menu (see also Section 4.2, “System Administration”).

If any estimated values should be included in the CSV statistics file, the values have to be selected in the DataStatistics menu under Select statistics(see also Section 6.3.1, “Configuring Statistics and CSV files”).

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

10.12.4. Sunshine Duration Sensors

Sunshine duration sensors indicate the sunshine status as defined by the WMO (sunshine = irradiation exceeds the level of 120 W/m²). The sensor measures the irradiation and switches the output voltage high or low to indicate sunny or not sunny conditions.

Sunshine duration sensors, e.g., Kipp & Zonen CSD 3, have to be connected to analog voltage channels (Ax). If direct irradiation should be measured, connect this output also to another analog voltage channel (Ax). Refer to Figure 13.2, “Electrical Connection Plan: Analog Voltage (Pyranometer)” for the connection diagram.

The output signal (V) indicates sunshine or no sunshine. Additionally, the calculated direct irradiation can be measured. The output signal (mV) for direct irradiation is proportional to the direct irradiation (W/m²).

Equation 10.10. Calculation of Solar Irradiation (E)

E [W/m²]= U [μV]/ Sensitivity [μV/[W/m²]]

Sensitivity is an internal parameter of the sensor, which is important to calculate the radiation in W/m². The value is given in the calibration certificate of the sensor.

Meteo-40 saves all electrically measured values in V to the source data ( Section 6.7, “Access to Source Data”). The calculated values for direct irradiation are saved in W/m² to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

Table 10.19. Sunshine Duration Sensors

SensorOrder-No
Kipp & Zonen CSD 3S61910

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

Meteo-40 saves all electrically measured values to the source data ( Section 6.7, “Access to Source Data”). The calculated direct irradiation in W/m² and the current sun status are saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file contains for all active channels the electrical values according to the chosen statistical interval.

10.12.5. Solar Trackers

EKO Instruments high precision STR Sun Tracker provide high tracking reliability, enhanced functionality with fully automated set up procedure through a built in GPS receiver. The compact sun trackers are suited to support all kinds of measurement sensors to measure Global, Diffuse and Direct Radiation.

EKO Sun Trackers must be connected to RS485-M port by means of an RS232 to RS485 adapter .

Date, time and location are acquired from the sensor by means of commands TM and LO. If the data logger values are significantly different, Meteo-40 will get automatically synchronized and the changes will be logged in the logbook. This syncronization happens in two cases: when configuring the sensor and on every CECS reboot. If you want to trigger the syncronisation routine, you can access the configured EKO Sun Tracker for editing and save it again without changeing the configuration.

According to the configured polling rate, which is 1 s per default, the calculated angle according to the GPS information and the current angle are requested and recorded.

[Important]Important

Make sure that no other method to synchronize date and time is active ( Section 4.2, “System Administration”).

Table 10.20. Data request for RS485 Sun Tracker

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
EKO Sun TrackerEKOCommands MR and CR

M1_1: Azimuth calculated (CR)

M1_2: Altitude calculated (CR)

M2_1: Azimuth (MR)

M2_2: Altitude (MR)

serial settings

10.12.6. Rotating Shadowband Irradiometer

Measure Global, Diffuse and Direct Radiation from two LiCor sensors as well as the temperature. The average values from both sensors are also calculated.

Table 10.21. Configuration of RS485 CSPS RSI

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
CSPS RSIModbus RTURegisters 0 to 20

M1_1: Global Horizontal Irradiance (GHI)

M1_2: Difuse Horizontal Irradiance (DHI)

M1_3: Direct Normal Irradiance (DNI)

M1_4: Temperature

M1_5: GHI LiCor 1

M1_6: DHI LiCor 1

M1_7: DNI LiCor 1

M1_8: GHI LiCor 2

M1_9: DHI LiCor 2

M1_10: DNI LiCor 2

Serial settings

10.12.7. Reference Cell

Table 10.22. Configuration details for RS485 Reference Cell

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration 
Datasol MET Reference CellModbus RTUregisters 96 to 108

Mx_1: Solar irradiance Avg. (W/m²)

Mx_2: Solar irradiance 1 (W/m²)

Mx_3: Solar irradiance 2 (W/m²)

Mx_4: Wind Speed (m/s)

Mx_5: Temperature Air (°C)

Mx_6: Temperature Panel (°C)

Serial settings, address 

10.12.8. RS485 communication specifications

Some pyranometers can or must be connected to the RS485-M port. For EKO pyranometers, it is also possible to use the M-Box RS485 Modbus RTU adapter and connect analog pyranometers to the RS485-M bus. If more than one sensor is connected to the RS485-M bus, they must be configured with a unique Modbus ID and they must all share the same protocol and serial settings (see Section 11.6, “Connecting Sensors to RS485-M”).

Table 10.23. Data request for RS485 pyranometer

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
EKO MS-60MModbus RTUregisters 19 to 24

M1_1: Measuring Voltage (mv)

M1_2: Global Irradiance (W/m²)

M1_3: Internal Temperature (°C)

serial settings (9600, 8N2)
EKO MS-80MModbus RTUregisters 19 to 24

M1_1: Measuring Voltage (mv)

M1_2: Global Irradiance (W/m²)

M1_3: Internal Temperature (°C)

serial settings (9600, 8N2)
EKO M-BoxModbus RTUregisters 19 to 24

M1_1: Measuring Voltage (mv)

M1_2: Global Irradiance (W/m²)

M1_3: Internal Temperature (°C)

serial settings (9600, 8N2)
EKO SMP10Modbus RTUregisters 5 to 10

M1_1: Solar Irradiance (W/m²)

M1_2: Solar Irradiance Long (W/m²)

M1_3: Temperature (°C)

serial settings (19200, 8E1)
Datasol MET Reference CellModbus RTUregisters 96 to 108

M1_1: Solar Irradiance Average (W/m²)

M1_2: Solar Irradiance 1 (W/m²)

M1_3: Solar Irradiance 2 (W/m²)

M1_4: Wind Speed (m/s)

M1_3: Temperature Air (°C)

M1_3: Temperature Panel (°C)

serial settings
Hukseflux SR30Modbus RTUregisters 2 to 6

M1_1: Irradiance(temperature compensated signal)(W/m²)

M1_2: Irradiance(temperature uncompensated signal)(W/m²)

M1_3: Sensor body temperature (°C)

serial settings (19200, 8E2)

10.13. Precipitation Sensors

10.13.1. Rain Gauge

Precipitation sensors are designed to measure the quantity and intensity of precipitation striking the earth’s surface. Precipitation is best measured with a tipping bucket device. Precipitation, collected over a surface of 200 cm², is conducted through an inflow sieve into a tipping bucket. When the bucket has collected 2 cm³ = 0.1 mm of precipitation, it tips over. This measurement principle is based on the “Guide to Meteorological Instruments No 8, WMO”. Precipitation sensors are typically applied for meteorological assessments.

Precipitation sensors, e.g., Young precipitation sensor, have to connected to counter channels (Cx). Refer to Figure 13.12, “Electrical Connection Plan: Pulse Counter with Pull-up Module for Precipitation Measurement” for the connection diagram.

The output signal (I) from the sensor is proportional to the precipitation quantity (N).

Equation 10.11. Calculation of Precipitation Quantity (N)

N [μm]= slope [μm/pulse] x I [pulse]

Slope is an internal parameter of the sensor, which is important to calculate the precipitation quantity according to the measurement rate set in the sensor configuration. The value is pre-configured in the Sensor Helper(see Section 5.1.2, “Sensor Helper”).

Table 10.24. Parameters for the configuration of precipitation sensors

SensorOrder-NoSlopeOffset
Thies Precipitation SensorS71100H0.1 mm/I0 mm
Young Precipitation SensorS73100 / S73100H0.1 mm/I0 mm

[Important]Important

If you install calibrated sensors, enter the values given in the calibration protocol.

Meteo-40 saves all electrically measured values in Pulse [I] to the source data ( Section 6.7, “Access to Source Data”). The calculated values are saved to the CSV file (see Section 6.6.1, “Ammonit Meteo-40 specific details”).

[Note]Note

The CSV file also contains for all active channels the electrical values according to the chosen statistical interval.

[Important]Important

If you plan to install precipitation sensor Thies or Young, you have to implement an accessory module! Refer to the data sheet and contact Ammonit for further details.

[Note]Note

For technical details and electrical characteristics of sensors, refer to the data sheets, which can be downloaded from the Ammonit website.

10.13.2. Laser Precipitation Monitors

Laser precipitation monitors measure various precipitation details, i.e., intensity of total, liquid and solid precipitation as well as the precipitation amount and the SYNOP parameter.

Thies Laser Precipitation Monitor (LPM) sensor performs a new calculation every minute, after the first 5 minutes of operation. Meteo-40 requests data with a 1 s rate in order to guarantee a valid measurement per minute with a working sensor.

Thies LPM has to be connected to RS485-M port.

Table 10.25. Configuration of RS485 Laser Precipitation Monitor Sensors

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Thies Laser Precipitation MonitorThiesTelegram 8

Mx_1: SYNOP

Mx_2: Intensity total precipitation

Mx_3: Intensity liquid precipitation

Mx_4: Intensity solid precipitation

Mx_5: Precipitation amount

Serial settings, address, half duplex mode, no automatic telegram sending

[Note]Note

SYNOP (surface synoptic observations) is a numerical code used for reporting weather observations, also called FM-12 by the World Meteorological Organization. Refer to Thies LPM sensor's manual for more information.

10.14. Multifunction Transducer, Power Meters and other Electrical Measurement Devices

Meteo-40 can be used to connect power meters, multifunction transducers or other electrical measurement devices, e.g., for power curve measurement. The devices are connected to the RS485-M of Meteo-40 (see Section 11.6, “Connecting Sensors to RS485-M”).

ModelProtocolDescriptionChannels and Evaluated dataSensor's previous configuration needed 

Sineax CAM (see Section 10.14.1, “Sineax CAM Measuring Unit”)

Modbus RTU

Actual values

(registers 40100, 40118 to 40122, 40134 to 40142)

Mx_1: Average phase Voltage U

Mx_2: Current I1

Mx_3: Current I2

Mx_4: Current I3

Mx_5: Real Power P1

Mx_6: Real Power P2

Mx_7: Real Power P3

Mx_8: Total Real Power P

Mx_9: Total Reactive Power Q

Serial settings, address 

Iskra MT540 (see Iskra manuals download)

Modbus RTU

Normalized actual values

(registers 804, 809 to 811, 816 to 819, 823)

Mx_1: Average phase Voltage U

Mx_2: Current I1

Mx_3: Current I2

Mx_4: Current I3

Mx_5: Real Power P1

Mx_6: Real Power P2

Mx_7: Real Power P3

Mx_8: Total Real Power P

Mx_9: Total Reactive Power Q

Serial settings, address 
GD2000 Multi-function Power AnalyzerModbus RTUregisters 56 to 63

Mx_1: Active power

Mx_2: Power factor

Mx_3: Reactive power

Mx_4: Apparent power

Serial settings (19200 bps), address 

10.14.1. Sineax CAM Measuring Unit

Sineax CAM is a universal measuring unit for heavy current variables. Actual measurements for average phase voltage, current, real and reactive power are requested from this sensor. For more information refer to Gossen Metrawatt Sineax CAM documentation.

10.15. Remote Sensing

10.15.1. ZephIR 300 Lidar

Meteo-40 can acquire ZephIR 300 live and averaged wind data measurements and include them in the measurement CSV files or share them over SCADA. You can select 'ZephIR 300' for averaged data or 'ZephIR 300 Live' for live data from the sensors list under 'Other Sensor'.

Before adding a ZephIR 300 to the list, it must be powered and connected to Meteo-40's RS485-M port. The configured heights will be automatically requested and for each height, a RS485 channel (M1 to M8) will be configured. If both live and averaged data are requested, a maximum of 4 heights can be configured at ZephIR 300.

[Note]Note

For more information about how to electrically connect ZephIR 300 and Meteo-40 please contact us.

[Important]Important

Measurement polling interval for averaged data is 1 minute per default. To ensure a valid measurement per interval it must always be lower than the statistics time interval (see Section 6.3, “Statistic Data Files”).

Table 10.26. Requested values

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
ZephIR 300Modbus RTUAveraged wind data per height

Mx_1: Reference

Mx_2: Wind Speed

Mx_3: Vertical Wind Speed

Mx_4: Wind Direction

Mx_5: Temperature

Mx_6: Air Pressure

Mx_7: Humidity

Mx_8: Wind Speed Max

Mx_9: TI

Serial settings, address
ZephIR 300 LiveModbus RTUAveraged wind data per height

Mx_1: Reference

Mx_2: Wind Speed

Mx_3: Vertical Wind Speed

Mx_4: Wind Direction

Mx_5: Temperature

Mx_6: Air Pressure

Mx_7: Humidity

Serial settings, address

10.16. Bats Detection

10.16.1. Song Meter SM3BAT

It is possible to connect the Wildlife Acustics Song Meter SM3BAT to the RS485-M interface. This allows a real time monitoring of bat passes and pulses, as well as of the status of the SM3BAT flash memory card and power supply.

[Note]Note

An external RS232 to RS485 adapter is required.

Table 10.27. Requested values

ModelProtocolDescriptionChannels / Evaluated Data
SM3BATASCII(compatible with Thies)

Mx_1: Internal Voltage (V)

Mx_2: Internal Temperature (°C)

Mx_3: Flash memory level (%)

Mx_4: Bat passes Mic0

Mx_5: Bat pulses Mic0

Mx_6: Bat passes Mic1

Mx_7: Bat pulses Mic1


Scheduling: The SM3BAT can be programmed to monitor during specific periods of the day, and “sleep” during other parts of the day to conserve power. When the SM3BAT is sleeping, it will not respond to Meteo-40 messages. Thus, the SM3BAT needs to be programmed when to be monitoring for bats e.g. 24 hours or just at night, etc.

Recording: The SM3BAT normally records the ultrasonic echolocation audio data on up to 4 SDHC or SDXC flash cards. Full spectrum recordings can typically consume 1-2GB of card space per night depending on bat activity. The flash cards will eventually fill up. Normally, the SM3BAT would shut down if it is no longer able to make recordings. However, for this application, it is desirable to continue monitoring, updating bat counters, and responding to requests. If the interface to Meteo-40 is detected, then the SM3BAT will continue monitoring for bats even if the flash cards are full, but no new bat activity data will be recorded. This condition is indicated by the flash card 100% full indication in the response messages.

Bat Activity: Echolocating bats typically produce individual ultrasonic “pulses” continuously while they fly for navigation, avoiding obstacles, and hunting for food. The frequencies, bandwidth and duration of pulses varies from species to species and with the functional needs of the bat at the time (e.g. many bats will increase bandwidth and decrease duration as they close in on prey). The SM3BAT can be configured to recognize pulses that may be tuned to specific bats in a given area. This includes specifying the minimum and maximum frequencies and minimum and maximum durations of a pulse. These parameters can be tuned to recognize echolocating bats while avoiding false positives from other ultrasonic noise sources such as wind, rain, and insects. The optimum parameters will depend on the specific bats and insects likely occurring in a given area. A “bat pass” refers to a series of pulses recorded as a bat flies by the microphone. Additional parameters in SM3BAT help define what a bat pass is including the maximum trigger duration and the maximum time between pulses (the trigger window). A bat pass begins with the first detected pulse, and ends when either no pulses have been detected after the maximum time between pulses has occurred, or when the maximum trigger duration has been reached. SM3BAT will not count a bat pass unless it contains at least two pulses. In this way, the SM3BAT can count passes and pulses detected on an ongoing basis and report these counts to the customer equipment.

10.17. Lightning Detector

10.17.1. SG1000 Lightning Detector

[Note]Note

This sensor can only be connected to data loggers produced after 2017-06, which can register the digital signal period (see Section 11.2, “Connecting Sensors to Counter / Period Channels”).

The SkyScan SG1000 lightning detector can detect the presence of lightning/thunderstorm activity occurring within 64 km of your location. It detects the characteristic electromagnetic emissions from individual lightning strokes and uses patented technology to determine the distance to the detected stroke. The distances are indicated in four ranges: 0-5 km; 5-13 km; 13-32 km; and 32-64 km. This allows you to track the approach of dangerous storm activity.

[Note]Note

More than one range can be detected simultaneously.

SG1000 may also identify certain types of especially strong storms. These storms can produce dangerous winds, heavy rains or tornadoes. When SG1000 detects lightning patterns indicating the presence of these storms, it activates the Severe thunderstorm alarm.

Four digital signals with complementary information are supplied by this lightning detector: Alarm, Error, Battery power and Baseline (see Table 10.28, “SG1000 status signals”).

Table 10.28. SG1000 status signals

SignalDescription
0-5kmDistance range 0-5 km
5-13kmDistance range 5-13 km
13-32kmDistance range 13-32 km
32-64kmDistance range 32-64 km
SevereSevere thunderstrom alarm
AlarmLightning activity has moved within range
ErrorThere is a system error that needs to be addressed (error code is indicated by the status LED on the unit)
Battery powerMains power has been interrupted and system is operating on battery backup
BaselineEnsures that there is activity on the digital output (i.e. can be used as a heartbeat to confirm system is up-and-running)

[Important]Important

If the period of the digital output signal of the sensor is changed, it is necessary to configure the measurement rate at Meteo-40 accordingly. The period of the digital output signal can be set to a value between 2.0 and 4.8 seconds, being the default value 2.0. The measurement rate configured at the data logger for this sensor must be at least twice as long as the period duration of the digital output, in order to guarantee that a complete period is catched. The default measurement rate is 5 seconds.

10.18. Soil Water Content

Measuring the water content, electrical conductivity (EC), and temperature of soil is a main topic for any agricultural project. Meteo-40 supports several volumetric water content (VWC) sensors, connected to an analog channel or to the RS485-M interface.

Table 10.29. Soil Moisture Sensors

Sensor 
Decagon EC-20, EC-10, EC-5 Soil Moisture Sensors 

Table 10.30. RS485 Soil Water Content Sensors

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration 
Campbell Reflectometer CS650SDI-12D0

Mx_1: Volumetric water content

Mx_2: Electrical conductivity

External module needed (address, 19200 8N1, 120Ω termination). See SDI-12. 

10.19. Soiling Measurement

Soiling is the accumulation of dust, dirt and other contaminants on the surfaces of PV modules. The amount of dust is extremely dependent on the location of the PV power plant, e.g., desert valley with sand storms. In absence of sig- nificant rain events or regular cleaning, production losses due to soiling effects increase. Measuring soiling effects provides important details about the PV power plant production, e.g., how much dust can be on the modules before any problem occurs and how does the dust affect transparency and efficiency of the modules.

10.19.1. Atonometrics RDE300

Soiling and Irradiance Measurement Systems with the Atonometrics RDE300 Series measurement and control unit collect critical data for evaluating PV array performance. The systems can be used at operating PV power plants and pre-construction site survey locations.

Table 10.31. Data request for RDE300 RS485 Soiling Measurement

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Atonometrics RDE300Modbus RTU 

M1_1: Global Irradiance PV1

M1_2: Analog Current PV1

M1_3: Temperature PV1

M1_4: Active Power PV1

M2_1: Global Irradiance PV2

M2_2: Analog Current PV2

M2_3: Temperature PV2

M2_4: Active Power PV2

M2_5: Soiling Ratio

M2_6: Soiling Ratio Isc

M2_7: Soiling Ratio Pmax

M3_1: Event Code

M4_1: Status Fluid

M5_1: Status Pump

Serial settings, address

10.19.2. Ammonit Soiling Measurement Kit SD2100

The Ammonit soiling measurement kit compares the estimated plane-of-array solar (POA) irradiance of a naturally-soiled PV module with a clean reference PV module. The measurement station determines the short-circuit current output as well as the module surface temperature from the backside of each PV module. Based on these measurements the POA irradiance can be determined for each module.

Equation 10.12. Calculation of POA Irradiation

G = G 0 x I SC x (1 - TK Isc x (T - T 0)) / I SC0

Where G : POA irradiance reaching the solar cells, G0 : reference condition irradiance, Isc : measured short circuit current, Isc0 : short circuit current at reference condition, T : measured surface temperature, T0 : surface temperature at reference condition, TK Isc : temperature coefficient of short circuit current.

Two standard metrics for the effects of soiling on energy production are availabe at the Evaluation Helper(see Section 5.3.1, “Evaluation Helper”). The Soiling Ratio Isc index (SR Isc), which equals 1 when both modules are clean, and the Soiling Loss Index (SLI), expressed as a percentage.

Equation 10.13. Calculation of SR Isc

SR Isc = I SC Soiled/ (I SC0 x (1 + TK Isc x (T Soiled- T 0)) x (G / G 0))

Where G is the POA irradiance from the clean module, Isc Soiled is the measured short-circuit current of the soiled module and T Soiled is the measured temperature of the soiled module.

Equation 10.14. Calculation of SLI

SLI = (1 - G Clean/ G Soiled) x 100

Where G Clean : POA irradiance of the clean PV module and G Soiled : POA irradiance of the reference PV module.

The Ammonit soiling measurement kit includes the following components: Ammonit I-U Conversion Box, Surface Temperature Sensor and a 30 W Photovoltaic (PV) Module.

Configure an Ampere meter from the sensors list for each of the I-U Conversion Boxes. In order to achieve best match to the output voltage, the appropriate voltage range must be selected. If you are using CM8281, with a shunt resistor of 50 mΩ, you must select the ±1.0 V range.

10.19.3. Kipp & Zonen DustIQ

The DustIQ is an instrument meant to measure and report the transmission loss (TL) and soiling ratio (SR) caused by light being blocked and reflected and subsequently not getting through the glass of the panel due to soiling of the panel.

Table 10.32. Data request for DustIQ RS485 Soiling Measurement

ModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Kipp & Zonen DustIQModbus RTU 

M1_1: Soiling Ratio 1

M1_2: Transmission Loss 1

M1_3: Soiling Ratio 2

M1_4: Transmission Loss 2

Serial settings, address

10.20. Other RS485 Sensors

In addition to meteorological sensors, further RS485-compatible sensors or devices can be connected to the RS485-M bus (see Section 11.6, “Connecting Sensors to RS485-M”). The following list includes some sensors and their configuration.

10.20.1. RS485 Multiplexer

Table 10.33. Configuration details for other RS485 Sensors / Devices

Sensor typeModelProtocolDescriptionChannels / Evaluated DataRequired Configuration
Multi Channel Voltage ModuleGantner e.bloxx A1Modbus RTUregisters 17 to 32

Mx_1: Analog Voltage AI1

Mx_2: Analog Voltage AI2

Mx_3: Analog Voltage AI3

Mx_4: Analog Voltage AI4

Mx_5: Analog Voltage AI5

Mx_6: Analog Voltage AI6

Mx_7: Analog Voltage AI7

Mx_8: Analog Voltage AI8

Serial settings, address, protocol, channels definition
Multi Channel Voltage ModuleGantner e.bloxx A3-1Modbus RTUregisters 17 to 26

Mx_1: Analog Voltage 1

Mx_2: Analog Voltage 2

Mx_3: Analog Voltage 3

Mx_4: Analog Voltage 4

Mx_5: Digital status

Serial settings, address, protocol, channels definition
Multi Channel Digital ModuleGantner e.bloxx D1-1Modbus RTUregisters 0 to 7

Mx_1: Digital status 1

Mx_2: Digital status 2

Mx_3: Digital status 3

Mx_4: Digital status 4

Mx_5: Digital status 5

Mx_6: Digital status 6

Mx_7: Digital status 7

Mx_8: Digital status 8

Serial settings, address, protocol, channels definition

10.20.2. Configuring generic Modbus RTU sensors

It is possible to connect up to 8 Modbus RTU sensors to RS485-M port (see Section 11.6, “Connecting Sensors to RS485-M”). They can be combined with other Modbus RTU sensors implemented in Meteo-40 like Lufft sensors, but not with other protocols like Thies or Gill.

Figure 10.1. Generic Modbus RTU sensor configuration

Screenshot of the generic Modbus RTU sensor configuration

The maximum quantity of consecutive registers that can be read from each sensor is 20. It is necessary to specify the first register (PDU addressing, first reference is 0) and the amount of registers. The function code is selectable between '03' (read holding registers) and '04' (read input registers).

Read registers will be evaluated according to the selected data type (see Table 10.34, “Data types available”). If a 32-bit data type is selected, each two registers will be merged. For each registers pair (if 32-bit data type selected) or each individual register (if 16-bit data type selected), an evaluation is generated. E.g. reading 10 registers on RS485 channel M1 will generate 10 evaluations if a 16-bit data type is selected (M1_1 to M1_10) and 5 evaluations if a 32-bit data type is selected (M1_1 to M1_5).

The resulting evaluations have no unit or evaluation type. You can create a new evaluation on top of each original evaluation by means of the linear equation from the Evaluation Helper(see Section 5.3.1, “Evaluation Helper”). Finally, it is necessary to properly select the evaluations to be included in the CSV statistics files in the DataStatistics(see Figure 6.4, “Statistics Configuration Page”).

Table 10.34. Data types available

Data TypeDescription
short (16-bit)16-bit integer
ushort (16-bit)16-bit unsigned integer
long (32-bit)32-bit integer
ulong (32-bit)32-bit unsigned integer
float (IEEE754 32-bit)32-bit single precision binary floating point
32-bit unsigned (8-bit exp)8-bit signed decade exponent, 24-bit uint
32-bit signed (8-bit exp)8-bit signed decade exponent, 24-bit signed int