Titlebook: Surface Water; Robert Bowen Book 1982 Applied Science Publishers Ltd. 1982 DDT.air.controlling.erosion.groundwater.hydrology.ocean.oceanic

charter

書目名稱Surface Water影響因子(影響力)




書目名稱Surface Water影響因子(影響力)學(xué)科排名




書目名稱Surface Water網(wǎng)絡(luò)公開度




書目名稱Surface Water網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Surface Water被引頻次




書目名稱Surface Water被引頻次學(xué)科排名




書目名稱Surface Water年度引用




書目名稱Surface Water年度引用學(xué)科排名




書目名稱Surface Water讀者反饋




書目名稱Surface Water讀者反饋學(xué)科排名

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獨(dú)特性

FLAG

Perigee

The Hydrologic Cycle,is spread out evenly throughout the year and does not prevent a severe drought arising at least once quinquennially. Many countries are much wetter and often have monsoonal rainfall whereas in other parts of the world extremely dry regimens are to be found. Of course rainfall is only one aspect of a

Slit-Lamp

The Atmosphere,sphere which is probably unique in the solar system because it contains water vapour, most of this being near its saturation point as a result of which cloudless conditions can change rapidly to obscure ones. Atmospheric water amounts to only 0–1% of the total quantity of water on the planetary surf

膠狀

Rivers,e determination of discharge, the volume of water passing through a given cross-section during a particular time interval. Units of measurement of discharge include cumecs (cubic metres per second) and for small flows litres per second. Earlier measurements may be given in cubic feet per second or c

GRUEL

Lakes and Other Surface Water Manifestations,o the sea or having such access solely by means of rivers. They occupy depressions into the zone of saturation in the environmental soil and rock, derive their water from rain, melted snow, ice, etc. and are small scale agents of erosion in which waves may develop, controlled by the same factors gov

隱語

The Oceans,ee Chapter 1, Table 1.10). This table also gives the volume of the oceans as l.37×l0.km. and since the rate of supply of water by rivers is approximately 36 × 10.g/year (or, as the density of water is about 1, 36 × 10. ml/year or 36 × 10.km. annually) the theoretical time interval required for ‘fill

Ingratiate

The Hydrologic Cycle, by the sun which gives rise to evaporation. A humid mass of air is created above the water surface and, becoming further warmed by it, ascends into the atmosphere due to its being lighter than the overlying cold air. The study of water and its various modes of occurrence on and in the planet constitutes the science of hydrology.