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The hydrologic cycle

The hydrologic cycle

Abstract

Hydrology is the science concerned with the occurrence and distribution of water on and under the earth. Meteorology is the science dealing with the atmosphere and the movement of water, both as vapour and as liquid, in the air. Both sciences are concerned with the hydrologic cycle - the circulation of water from oceans through the atmosphere back to the oceans or to the land and thence to the oceans by overland and subterranean routes. Water is constantly on the move. Evaporation takes place from a multitude of surfaces ranging from a free water surface on the ocean to the moisture on a leaf. Precipitation falls in various forms - snow, rain, hail. Also, moisture is deposited on the surface of the earth by the formation of dew and frost. Water is stored for varying lengths of time in a number of forms including atmospheric moisture, water in swamps and lakes, soil moisture, groundwater, ice in glaciers, and snow on the ground. Water is transferred from one environment to another by surface runoff,

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
0
Average
Average
Average
hybrid