HomeProductsRadiation SensorsFour Component Net Radiometer for Solar Radiation Monitoring
  • Four component net radiometer for solar radiation monitoring

Four Component Net Radiometer for Solar Radiation Monitoring

Key Features

  • Simultaneous measurement of four independent radiation components
  • Measures downward and reflected shortwave radiation
  • Measures atmospheric and surface-emitted longwave radiation
  • Supports net shortwave, net longwave and total net radiation calculation
  • Supports surface albedo analysis
  • Shortwave spectral range from 0.3 to 3 μm
  • Longwave spectral range from 3.5 to 50 μm
  • Response time of 10 seconds or less
  • RS485 output for digital data acquisition
  • Pt100 temperature compensation for measurement stability
  • Precision double glass dome structure
  • Low-reflectance radiation-absorbing coating
  • Integrated two-axis leveling assembly
  • Suitable for long-term outdoor monitoring
  • Working temperature range from -40°C to 80°C
  • Suitable for environments with 0–100% relative humidity
  • Can be integrated with weather stations and cloud monitoring systems

Product Description

The JW-TBB-2L(LC27) Four-Component Net Radiometer is designed for professional solar radiation, surface energy balance and environmental monitoring.

It simultaneously measures four radiation components:

  • Downward shortwave radiation
  • Upward reflected shortwave radiation
  • Downward longwave radiation
  • Upward longwave radiation emitted by the surface

By separating these four components, the instrument provides more detailed radiation data than a conventional single-output net radiometer. The measurements can be used to calculate net shortwave radiation, net longwave radiation, total net radiation and surface albedo.

With RS485 communication, fast response and a durable outdoor structure, the radiometer can be integrated into automatic weather stations, agricultural monitoring systems, research stations, data loggers, RTUs and remote IoT monitoring platforms.

What Is a Four-Component Net Radiometer?

A four-component net radiometer is an instrument that separately measures incoming and outgoing shortwave and longwave radiation above a surface.

The four measurements are normally represented as:

  1. Downward shortwave radiation
    Solar radiation arriving from the sky and sun.
  2. Upward shortwave radiation
    Solar radiation reflected by soil, vegetation, snow, water, roofing materials or other surfaces.
  3. Downward longwave radiation
    Thermal infrared radiation emitted downward by the atmosphere and clouds.
  4. Upward longwave radiation
    Thermal infrared radiation emitted upward by the ground or monitored surface.

Because each component is recorded independently, researchers can analyze how solar and thermal radiation interact with the land surface, crops, water bodies, snow, buildings and photovoltaic sites.

How Is Net Radiation Calculated?

The radiometer provides the individual measurements required to calculate the surface radiation balance.

Net Shortwave Radiation

Net Shortwave Radiation = Downward Shortwave Radiation − Upward Shortwave Radiation

Net shortwave radiation represents the solar energy absorbed by the monitored surface after reflected solar radiation is deducted.

Net Longwave Radiation

Net Longwave Radiation = Downward Longwave Radiation − Upward Longwave Radiation

Net longwave radiation represents the balance between atmospheric thermal radiation and thermal radiation emitted by the surface.

Total Net Radiation

Total Net Radiation = Net Shortwave Radiation + Net Longwave Radiation

Total net radiation represents the net radiative energy available at the surface.

Depending on the project, this value can support evapotranspiration studies, heat-flux analysis, crop energy balance assessment, climate research and environmental modelling.

Surface Albedo

Albedo = Reflected Shortwave Radiation ÷ Downward Shortwave Radiation

Albedo describes the proportion of incoming solar radiation reflected by a surface.

Bright surfaces such as snow generally reflect more shortwave radiation, while darker soil, water and vegetation normally absorb a greater proportion of incoming radiation.

For projects that only require shortwave reflectance measurement, see the Albedo Sensor for Surface Reflectance Monitoring.

Four-Component Net Radiometer vs Conventional Net Radiometer

A conventional net radiometer normally provides one combined net radiation measurement. It is suitable when the monitoring system only needs the final radiation balance value.

A four-component radiometer measures the four individual radiation streams separately.

Measurement Requirement Conventional Net Radiometer Four-Component Net Radiometer
Combined net radiation Yes Yes, calculated
Downward shortwave radiation Usually not separate Yes
Reflected shortwave radiation Usually not separate Yes
Downward longwave radiation Usually not separate Yes
Upward longwave radiation Usually not separate Yes
Surface albedo analysis Limited Yes
Detailed energy balance research Limited Recommended
Basic weather station use Suitable Possible
Scientific surface radiation studies Limited Suitable

Choose a conventional net radiometer when a single net radiation value is sufficient.

Choose a four-component net radiometer when the project must distinguish between solar radiation, reflected radiation, atmospheric longwave radiation and surface-emitted longwave radiation.

For simpler net radiation monitoring, see the Net Radiation Sensor with RS485 for Climate Monitoring.

Four-Component Radiometer vs Pyranometer

A pyranometer normally measures shortwave solar irradiance from one direction. It does not independently measure longwave thermal radiation.

A four-component net radiometer combines upward- and downward-looking shortwave and longwave sensing channels.

Use a pyranometer when the main requirement is:

  • Global horizontal irradiance
  • Plane-of-array irradiance
  • Solar resource assessment
  • PV performance monitoring
  • General weather station radiation measurement

Use a four-component radiometer when the project requires:

  • Surface energy balance
  • Separate shortwave and longwave components
  • Incoming and outgoing radiation comparison
  • Albedo and thermal radiation analysis
  • Agricultural or climate research

For standalone solar irradiance measurement, see the Class A Pyranometer Solar Radiation Sensor.

You can also explore the complete JW-IoT Radiation Sensors range.

Measurement Components

Downward Shortwave Radiation

The upward-facing shortwave sensor measures solar radiation received from the hemisphere above the instrument.

This measurement includes direct and diffuse solar radiation reaching the monitoring surface.

Typical uses include:

  • Solar resource analysis
  • Agricultural radiation monitoring
  • Weather and climate studies
  • Surface energy input assessment
  • PV environmental monitoring

Reflected Shortwave Radiation

The downward-facing shortwave sensor measures the portion of incoming solar radiation reflected by the surface below.

The data can be compared with downward shortwave radiation to calculate surface albedo.

Typical monitored surfaces include:

  • Soil
  • Crops
  • Grassland
  • Forest canopy
  • Snow and ice
  • Water
  • Desert
  • Urban roofs
  • Photovoltaic arrays

Downward Longwave Radiation

The upward-facing longwave sensor measures thermal infrared radiation emitted by the atmosphere and clouds toward the surface.

This component is important for studying nighttime radiation balance, cloud effects and atmospheric heat exchange.

Upward Longwave Radiation

The downward-facing longwave sensor measures thermal radiation emitted by the monitored surface.

Surface temperature, material properties, soil moisture, vegetation, water conditions and solar heating can all influence upward longwave radiation.

Technical Specifications

Parameter Specification
Product Type Four Component Net Radiometer
Model JW-TBB-2L(LC27)
Measurement Elements Shortwave radiation, reflected shortwave radiation, longwave radiation, reflected longwave radiation, full wave radiation, net radiation
Solar Spectral Range 0.3 to 3 μm shortwave, 3.5 to 50 μm longwave
Shortwave Sensitivity 7 to 14 μV W¹ m²
Longwave Sensitivity 2 to 10 μV W¹ m²
Signal Output RS485
Annual Stability ≤ ±2%
Nonlinearity ≤ 4%
Measurement Accuracy ≤ ±5%
Measurement Range -2000 to 2000 W m²
Temperature Compensation Pt100
Response Time ≤ 10 s
Working Humidity 0% to 100% RH
Working Temperature -40°C to 80°C
Leveling Method Two axis leveling assembly
Weight 4.5 kg

Final specifications may vary according to the ordered configuration. Confirm the output protocol, power supply, cable length, mounting accessories and data logger compatibility before ordering.

RS485 Data Integration

The RS485 output enables the four-component radiometer to connect to common industrial and environmental monitoring equipment.

Typical connection devices include:

  • Automatic weather station controllers
  • Environmental data loggers
  • Agricultural RTUs
  • PLC systems
  • IoT sensor nodes
  • Modbus gateways
  • 4G communication terminals
  • LoRaWAN gateways
  • Local SCADA systems
  • Cloud monitoring platforms

A typical remote monitoring architecture is:

Four-Component Net Radiometer
→ RS485 Data Logger or RTU
→ 4G, Ethernet or LoRaWAN Gateway
→ Cloud Platform or Research Database

The data logger records the four independent radiation channels. The monitoring software can then calculate net radiation, albedo and long-term radiation balance indicators.

JW-IoT can provide compatible controllers, communication devices and platform integration according to the project architecture.

Typical Applications

Surface Energy Balance Research

Net radiation is an important component of the surface energy balance.

Four-component measurements allow researchers to separate absorbed solar energy from longwave thermal exchange, providing more complete input for energy balance models.

Agricultural Meteorology

The radiometer can be installed above cropland, orchards, grassland and experimental plots.

Typical research topics include:

  • Crop radiation interception
  • Canopy energy balance
  • Evapotranspiration
  • Soil–plant–atmosphere interaction
  • Irrigation research
  • Crop microclimate monitoring
  • Agricultural heat-stress studies

Evapotranspiration Studies

Net radiation is one of the key energy inputs used in many evapotranspiration studies.

When combined with air temperature, humidity, wind speed, soil heat flux and other meteorological measurements, the radiometer can support research into water and energy exchange.

Meteorological and Climate Research

The instrument can be integrated into professional weather stations for:

  • Radiation budget studies
  • Boundary-layer research
  • Cloud and atmospheric radiation analysis
  • Climate observation
  • Long-term environmental monitoring
  • Surface–atmosphere exchange studies

Snow and Ice Monitoring

Snow and ice have distinctive shortwave reflectance and thermal radiation characteristics.

The four-component radiometer can support:

  • Snow albedo monitoring
  • Glacier energy balance research
  • Snowmelt analysis
  • Alpine climate studies
  • Polar environmental observation

Water and Wetland Research

The instrument can be installed above lakes, reservoirs, wetlands and other water surfaces.

It can help evaluate:

  • Water-surface radiation balance
  • Evaporation conditions
  • Wetland energy exchange
  • Reservoir microclimate
  • Aquatic environmental processes

Solar Energy Research

Although PV projects often use a pyranometer for irradiance monitoring, a four-component radiometer provides additional reflected shortwave and thermal radiation data.

It can support:

  • PV site environmental studies
  • Module and ground albedo research
  • Bifacial PV analysis
  • Surface temperature studies
  • Floating solar environmental monitoring
  • Solar farm microclimate research

For conventional PV irradiance measurement, read Solar Irradiance Sensors for Accurate PV Performance Monitoring.

For a complete solar monitoring architecture, see the PV Plant Weather Station Solution.

Urban Surface Radiation Studies

The radiometer can also be used to compare the radiation characteristics of:

  • Concrete
  • Asphalt
  • Roofing materials
  • Green roofs
  • Building surfaces
  • Urban vegetation
  • Reflective coatings

This information can support urban heat-island and building-energy research.

Installation Recommendations

Select a Representative Location

Install the radiometer above a surface that represents the research objective.

For example:

  • Above a crop canopy for agricultural studies
  • Above bare soil for soil energy balance monitoring
  • Above snow for albedo and snowmelt research
  • Above water for evaporation studies
  • Above a roof for urban surface research

The downward-facing sensors should see a representative and sufficiently uniform surface.

Keep the Instrument Level

A four-component radiometer should normally be installed horizontally.

Use the integrated two-axis leveling mechanism to adjust the instrument. Check the level again after tightening the mounting hardware.

A tilted instrument may introduce directional errors and make data from different sites difficult to compare.

Avoid Obstructions and Shadows

Keep the radiometer away from:

  • Poles
  • Towers
  • Buildings
  • Trees
  • Solar panels
  • Cables
  • Fences
  • Other sensors

Nearby objects can block incoming radiation, reflect additional radiation or cast shadows on the sensor.

The mounting arm should minimize obstruction of the downward-facing field of view.

Maintain a Representative Field of View

The downward-facing sensors measure radiation from the surface below.

The mounting height and surrounding surface area should be selected so that the sensor primarily sees the intended target rather than unrelated objects.

For crop monitoring, also consider whether the plant canopy height will change during the growing season.

Route the Cable Carefully

Secure the cable to prevent movement in strong wind, but do not pull or sharply bend it near the sensor connector.

Use suitable cable protection, grounding and surge protection for long-term outdoor installations.

Clean the Optical Domes

Dust, pollen, bird droppings, frost, snow and water deposits may affect radiation measurements.

Inspect and clean the glass domes regularly using a soft, non-abrasive material and a cleaning method approved for optical surfaces.

Check Level and Mounting Stability

Regularly inspect:

  • Leveling position
  • Mounting bolts
  • Cable connectors
  • Surface contamination
  • Corrosion
  • Condensation
  • Physical damage

Maintenance frequency should be adjusted according to dust, rainfall, snow, pollution and site accessibility.

How to Choose the Right Radiation Sensor

Use the following questions before selecting a sensor.

Do You Need Four Separate Radiation Components?

Choose this four-component radiometer when the project requires independent shortwave and longwave measurements.

If only one combined net radiation output is required, a conventional net radiation sensor may be sufficient.

Do You Need Surface Albedo?

A four-component radiometer can calculate albedo from its shortwave channels.

When the project only requires incoming and reflected shortwave radiation, an albedo sensor may provide a simpler configuration.

Is the Project Focused Only on Solar Irradiance?

For PV performance monitoring, general weather stations or solar resource assessment, a pyranometer or dedicated solar irradiance sensor may be more appropriate.

See the Solar Irradiance Sensor for PV Monitoring Solution for complete PV monitoring options.

Do You Need Remote Data Transmission?

Specify whether the project requires:

  • Local RS485 collection
  • Modbus RTU
  • 4G communication
  • Ethernet
  • LoRaWAN
  • MQTT
  • HTTP
  • API integration
  • Cloud platform
  • Private server deployment

JW-IoT can help configure the sensor, data logger and communication architecture according to the project.

Recommended Supporting Sensors

A four-component net radiometer is often used together with other sensors.

Recommended measurements include:

  • Air temperature
  • Relative humidity
  • Wind speed
  • Wind direction
  • Rainfall
  • Atmospheric pressure
  • Soil temperature
  • Soil moisture
  • Soil heat flux
  • Surface temperature
  • Leaf wetness
  • Water level
  • PV module temperature

Combining multiple parameters gives researchers more context for interpreting changes in radiation balance.

Request a Four-Component Net Radiometer Configuration

Send JW-IoT your application, installation conditions, required radiation parameters, communication method and data acquisition requirements.

Our team will help configure a suitable four-component radiometer and field monitoring solution for your project.

Request a Quotation

Explore JW-IoT Radiation Sensors

FAQ

  • Q

    1. What does a four-component net radiometer measure?

    A

    It separately measures downward shortwave radiation, reflected upward shortwave radiation, downward atmospheric longwave radiation and upward longwave radiation emitted by the surface.

  • Q

    2. What is the difference between a four-component radiometer and a net radiometer?

    A

    A standard net radiometer normally provides one combined net radiation output. A four-component radiometer records four independent radiation streams, allowing users to calculate net shortwave, net longwave, total net radiation and albedo.

  • Q

    3. Can the radiometer calculate surface albedo?

    A

    Yes. Surface albedo can be calculated by dividing reflected shortwave radiation by downward shortwave radiation, provided the incoming radiation level and site conditions are suitable for the calculation.

  • Q

    4. Does the JW-IoT radiometer support RS485 output?

    A

    Yes. The JW-TBB-2L(LC27) supports RS485 output for integration with compatible data loggers, RTUs, weather stations and monitoring platforms.

  • Q

    5. Can it be used for evapotranspiration research?

    A

    Yes. Net radiation data is commonly used together with weather, soil and heat-flux measurements in evapotranspiration and surface energy balance studies.

  • Q

    6. Can the sensor be installed above crops?

    A

    Yes. It can be installed above crops or vegetation, provided the mounting height, field of view and surface representativeness are considered. The installation may need adjustment as the canopy height changes.

  • Q

    7. Is it suitable for snow and glacier monitoring?

    A

    Yes. Separate incoming and reflected shortwave measurements support snow albedo studies, while the longwave channels provide additional data for snow and ice energy balance research.

  • Q

    8. How should the radiometer be mounted?

    A

    The instrument should normally be mounted horizontally using the two-axis leveling assembly. The upper and lower sensors should remain unobstructed, and nearby structures should not cast shadows or create unwanted reflections.

  • Q

    9. How often should the optical domes be cleaned?

    A

    Cleaning frequency depends on dust, pollen, rainfall, snow, birds and local pollution. The domes should be inspected regularly and cleaned whenever contamination may affect the measurements.

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