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 into account when investigating the thermal regime of the atmosphere. The treatment of ...
The daily variation of temperature at a height of 1 km. over Berlin, deduced from 2232 observations made during the five years 1903-7, is given in degrees C. by where Tis the mean surface temperature, and the probable errors are deduced by the method of least squares. The most probable ...
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 ...
(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 ...
Weather, state of the atmosphere at a particular place during a short period of time. It involves such atmospheric phenomena as temperature, humidity, precipitation (type and amount), air pressure, wind, and cloud cover. Weather differs from climate in t
Evidence of the dependence of groundwater resources on extreme rainfall in East Africa (IOD) and the El Niño Southern Oscillation (ENSO), the dominant modes of coupled ocean–atmosphere interaction in the tropical global and Indian oceans... RG Taylor,MC Todd,L Kongola,... - 《Nature Clim...
The heat-trapping capacity of the atmosphere is popularly known as the “greenhouse effect”.Despite public controversy surrounding global warming,the natural greenhouse effect has been long established as a fact in the scientific community.Indeed,carbon dioxide,and other gases,the earth's natural ...
In subject area: Engineering The stability of the atmosphere is governed by the vertical temperature distribution resulting from radiative heating or cooling of the earth's surface and the subsequent convective mixing of the air adjacent to the surface. ...
as an example because electricity demand is projected to increase significantly (up to 60% from 2015 to 2050) in the coming decades28,29, and the U.S. is characterized by a wide variation in climate conditions and electricity fuel mixes. Additionally, a comprehensive understanding of temperature...
bioclimatology climate climatology Effective Temperature Index Kenya temperature climatic comfort conditions spatial variation seasonal variation diurnal variation season boundary layer classification zoning zone physio-climatic study/ A9260S Climatology A9330B Africa A9260K Temperature of the lower atmosphere DOI...