terrestrial radiation

Water is important for the absorption of solar and terrestrial radiation.

Terrestrial radiation, for the purpose of the table above, only includes sources that remain external to the body.

Shielding is an effective protective measure for terrestrial radiation workers.

However, these "signals" turned out to be terrestrial radiation.

All aerosols both absorb and scatter solar and terrestrial radiation.

T1170 Total radiation Sum of the solar and terrestrial radiation components.

A3000 Atmospheric window Spectral region in which the atmosphere absorbs very little terrestrial radiation.

A common example of terrestrial radiation source is radon gas, which comes from uranium in the soil and can accumulate in buildings.

This will occur when the incoming solar radiation balances the outgoing terrestrial radiation.

Presently the Martians discovered the sources of terrestrial radiation in the innumerable wireless transmitting stations.

Space, atmospheric, and terrestrial radiation environments.

T0310 Terrestrial radiation Long-wave radiation emitted by the Earth, including its atmosphere.

The major radionuclides of concern for terrestrial radiation are isotopes of potassium, uranium, and thorium.

But because the Earth has a much lower average surface temperature than the Sun, terrestrial radiation is emitted at longer wavelengths, mostly in the infrared range.

And on top of that, temperature and humidity readings are never corrected for environmental variables: wind-chill, precipitation, terrestrial radiation.

Conclusion The overall state of the of the global climate is determined by the balance of solar and terrestrial radiation budgets (see Figure 1.3).

The 48 units absorbed by the atmosphere (34 units from terrestrial radiation and 14 from insolation) are finally radiated back to space.

The reduction, is however, compensated for by an increase in diffuse radiation and by the absorption of outgoing terrestrial radiation (the greenhouse effect).

Their primary application has been on board spacecraft measuring atmospheric and terrestrial radiation, and they are mostly used for meteorological or oceanographic remote-sensing.

U0390 Upward terrestrial radiation Upward long-wave radiation emitted by the Earth's surface.

When the sky is clear, terrestrial radiation is not compensated by radiation emitted by clouds, which actually store and re-emit heat themselves.

D1020 Downward terrestrial radiation Atmospheric counter radiation Atmospheric radiation directed downwards.

The main sources of this radiation are cosmic radiation from the sun and outer space, and terrestrial radiation from radioactive elements in the earth's crust.

N0280 Net pyrgeometer Instrument for measuring the difference between the terrestrial radiation amounts received by both sides of a plane surface from the solid angle 2p, respectively.

Outgoing Radiation Consists of shortwave reflected solar radiation as well as longwave terrestrial radiation.