Global EcologyProgress Publishers, 1980 - Всего страниц: 322 |
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Стр. 51
... areas that are not dealt with in literature are represented by shaded areas . It may be seen from Figure 4 that the yearly magnitudes of total radiation change substantially within a range of less than 60 kcal / cm2 . year and values ...
... areas that are not dealt with in literature are represented by shaded areas . It may be seen from Figure 4 that the yearly magnitudes of total radiation change substantially within a range of less than 60 kcal / cm2 . year and values ...
Стр. 128
... areas large enough to be compared with the geographical zones . In the case of small areas , river run - off may change substantially as a result of local conditions of a nonclimatic nature . 3. The Water Exchange in the Atmosphere ...
... areas large enough to be compared with the geographical zones . In the case of small areas , river run - off may change substantially as a result of local conditions of a nonclimatic nature . 3. The Water Exchange in the Atmosphere ...
Стр. 253
... areas . The influence of human activities on the hydrological regime of land areas has been increasing rapidly . The run - off of many large rivers as well as of small ones has been sub- stantially altered as a result of the creation of ...
... areas . The influence of human activities on the hydrological regime of land areas has been increasing rapidly . The run - off of many large rivers as well as of small ones has been sub- stantially altered as a result of the creation of ...
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activities aerosols air temperature albedo anthropogenic approximately areas atmosphere autotrophic autotrophic plants average temperature biomass biosphere boundary Budyko calculations carbon dioxide cent changes in climate climatic conditions coefficient components concentration of carbon continents corresponding declines dependence direct radiation Earth-atmosphere system Earth's surface ecological systems energy balance environment equation evaporation evolution existence extinction factors flow fluctuations forests formula geographical zones glaciation global ecological heat balance herbivorous high latitudes hydrosphere ice cover increases inflow of heat influence kcal/cm² layer lithosphere living organisms magnitude major man's meteorological middle latitudes Northern Hemisphere noted numerical models oceans organic matter oxygen period Phanerozoic photosynthesis photosynthetically active radiation Pleistocene population possible precipitation processes quantity radiation balance reduction regions relation relatively represents reptiles result run-off soil solar constant solar energy solar radiation species stratosphere studies substantially thermal regime tion total radiation tropical Upper Paleolithic values various volume water balance water exchange water vapour zonality