This chapter discusses the temperature variation in the atmosphere because of radiative heat exchange. Radiative heat exchange in the atmosphere is connected with changes in air temperature, which must be taken
Seasonal and other temperature changes in the Antarctic atmosphere . Q. J. R. Meteorol. Soc. 85 : 196 – 208 .Seasonal and Other Temperature Changes in the Antarctic Atmosphere, ” Quarterly - Wexler - 1959Wexler, H. (1959), Seasonal and other temperature changes in the Antarctic atmosphere...
1a). At the end of the time series, the red curve is very close to the polynomial and at the beginning very close to the exponential function. The largest deviations in terms of the shape occur in the period between about 1940 and 1970. The aerosol loading in the atmosphere largely ...
The average variation of temperature with height in the Martian atmosphere is probably controlled by radiative and convective processes. With the use of a simple theoretical formulation in which it is assumed that convection will extend to that height above which the radiative equilibrium lapse rate ...
(2015). Long-term air temperature variation in the Karkonosze mountains accord- ing to atmospheric circulation. Theoretical and Applied Climatology, 125, 337-351.Migała K, Urban G, Tomczyński K (2016) Long-term air temperature variation in the Karkonosze mountains according to atmospheric ...
The thermal variation of the sediments and the energy balance components are computed for a sandy beach in the Claromeco estuary located in the South-East of the Buenos Aires province Argentina. The study covers a seven days period in March 1999. Soil, air and water temperatures were measure...
These temperature variations create forces that drive the atmosphere in its endless motions. Day-to-night (diurnal) variation of temperature Diurnal variation is the change in temperature from day to night brought about by the daily rotation of the Earth. Earth receives heat during the day from ...
Due to very thick and reflective atmosphere7,8,9,10, Venus surface absorbs about 2.5% of incident solar flux as compared to about 50% on Earth11. Therefore, the surface temperatures do no show a significant variation with latitudes. Relatively high temperatures in 0–90° longitudinal band ...
To facilitate correction of a temperature-dependent radiometric response, these instruments monitored the temperatures of their deployed radiation detectors. The accurate calibration of the temperature sensors, and their strong thermal coupling to the atmosphere, make it possible to deduce atmospheric ...
(Fig.3d). In addition, our reconstructions could be more robust for winter than for summer temperatures, because of its more contribution to vegetation variation according to Redundancy Analysis, and the better performance of the calibration for winter temperature indicated by cross-validations (see ...