Solar Radiation Instruments Information
Image credit: TES Electrical Electronic Corp. | RainWise, Inc.
Solar radiation instruments measure the spectral range of radiation, including global solar radiation, net radiation, and photosynthetic light.
Types of Solar Radiation
Solar radiation instruments may be produced to measure different types of solar energy. When sunlight encounters the Earth's atmosphere, some of it is absorbed or scattered by water vapor, aerosols, clouds, and other air molecules. The radiation which penetrates to the Earth's surface is termed direct solar radiation. Conversely, the radiation which scatters out of the direct beam is referred to as diffuse radiation. The sum of direct and diffuse solar radiation is global solar radiation. Global solar radiation is sometimes referred to as "sun+sky" radiation.
Typical solar activity on Earth.
Image credit: GlobalGreenhouseWarming
Net solar radiation refers to the surface radiation after subtracting the radiation reflected by the ground surface.
In the image above, then, the global solar radiation would be 198 W·m2, while the net radiation (penetrating radiation - reflected radiation) is 168 W·m2.
Solar radiation instruments are used to measure and record solar irradiance, which is one of several variables to consider when discussing radiometry. Being a unit of power, irradiance is measured and discussed using watts per square meter of surface (W·m2). When using solar radiation instruments, the "surface" being discussed is typically the surface of the Earth or a solar panel.
The irradiance of a beam of monochromatic light can be manually calculated using the formula below.
E = complex altitude of the wave's electric field
n = refractive index of the surface
c = speed of light within a vacuum
ε0 = vacuum permeability
The graph below shows the typical irradiance of two types of sunlight: the sunlight above the atmosphere (yellow) and the surface radiation at sea level (red). Note that irradiance peaks within the visible spectrum and decreases at higher and lower wavelengths.
The solar radiation spectrum.
Image credit: Wikimedia
Solar radiation is measured by some type of radiometer. Meteorologists and climatologists use various types of radiometers depending upon the type of solar radiation they intend to measure.
Pyranometers measure hemispherical solar irradiance, or broadband solar radiation within a 180-degree field of view; this may be considered the global solar radiation of a given hemisphere.
A typical analog pyranometer does not require power to operate and consists of a thermopile sensor beneath a glass dome. The thermopile absorbs all the solar radiation which encounters it and generates a small, proportional output voltage. Pyranometers are typically used on or near solar panels to facilitate optimum panel positioning.
A typical thermoelectric pyranometer.
Image credit: Kipp & Zonen
Digital pyranometers are used to record and analyze irradiation data. They are typically capable of ouputting data in serial form. As shown in the image below, digital pyranometers may be handheld for taking field measurements.
A handheld digital pyranometer.
Image credit: DJB Microtech
Pyrheliometers are similar to pyranometers, but they are designed to measure only direct beam solar irradiance. To this end they are occasionally used in identical pyranometer applications, but are also used with solar tracking systems to ensure the system is consistently aimed toward the sun. The device itself is often mounted directly on the tracking system so that it is always measuring direct beam sunlight.
Sunlight enters pyrheliometers through an integral lens, which projects sunlight onto a thermocouple within the device. Most pyrheliometers can convert a thermopile's small voltage output into watts per square meter and either output or record this data.
The cross-section of a typical pyrheliometer; this device would be mounted on a tracking system.
Image credit: eoPortal
Quantum sensors are specialized devices which measure the quantity of photosynthetically active radiation — or the portion of the visible spectrum which can be used by photosynthetic organisms — within a band of solar radiation. Specifically, quantum sensors measure the photosynthetic photon flux density (PPFD) of sunlight. This measurement is useful in agriculture for choosing productive farmland locations or maintaining growhouses, and is also used in oceanography to calculate the boundaries of an ocean's sunlight zone. (For the latter reason, quantum sensors are often built with waterproof housing.)
Quantum sensors typically use photovoltaic technology to generate a potential output.
A quantum sensor attached to a light meter.
Image credit: University of Helsinki
Instruments used to measure solar radiation may be governed in production, use, and testing by various standards. A few example standards are listed below. The ISO 9060 standard is a commonly-used document for classifying and using pyranometers.
ISO 9060 - Specification and classification of instrument for measuring hemispherical solar and direct solar radiation
ASTM E816 - Standard test method for calibration of pyrheliometers by comparison to reference pyrheliometers
ISO 9059 - Calibration of field pyrheliometers by comparison to a reference pyrheliometer
Institute for Earth Science Research and Education - Build your own pyranometer