solar radiation

Planetary albedo describes the percentage of incoming solar radiation that is reflected back into space after all interactions with the atmosphere and the surface of the Earth.

As clouds, depending on their type and height, both shield solar radiation and prevent heat from being radiated into space, they play a crucial role in the climate.

Aerosols reflect part of the solar radiation back into space and therefore reduce the heat retained by the Earth.

Existing methods for generating meteorological data do not adequately handle the interdependence of meteorological elements, such as solar radiation, air temperature, and absolute humidity, which are important for calculating energy usage and efficiency.

As the Arctic warms at a faster rate than the rest of the planet, Earth’s overall surface becomes less reflective and thereby increases the absorption of solar radiation.