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(2008) determined an overall increase of 2.6 W m–2 per decade over the 1990s, in line with model projections and the expectations of an increasing greenhouse effect.
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Downward thermal radiation observations started to become available during the early 1990s at a limited number of globally distributed terrestrial sites. Long-term measurements of the thermal surface components as well as surface net radiation are available at far fewer sites than SSR. Thermal radiation, also known as longwave, terrestrial or far-IR radiation is sensitive to changes in atmospheric GHGs, temperature and humidity.
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