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The water regime variability in most catchments is frequently influenced not only by the changes of the vegetation cover in the annual cycle but also by its development in the time span of decades.
Regional hydrological processes have been greatly influenced by human activities and climatevariability. The inflow of Panjiakou Reservoir, which is the largest reservoir located on the Lu...
The irrigated areas in the northern region of China are important food production areas. Therefore, studies on the variability of he carbon balance in these agro-ecosystems are fundamental for the man...
The covered-ice breakup in subarctic to arctic rivers in the early snowmelt season often gives any damage to instruments monitoring physical and chemical factors of water. The serious condition has br...
The complementary relationship (CR) between potential evaporation (LEp) and actual evaporation (LE) is widely used to explainthe evaporation paradox and to estimate LE, in which wet environment evapor...
Understanding the interactions among climate,vegetation cover and the water cycle lies at the heart of thestudy of watershed ecohydrology. Recently, considerableattention is being paid to the effect o...
This paper is premised on the hypothesis that the amount of rainfall in Nigeria decreases with increasing distance from the coastal areas to the north semi arid lands. This belief widely held in some ...
Miyun Reservoir is the main raw water source for Beijing’s domestic water supply. Flow discharge toMiyun Reservoir decreased drastically over a 50-year period, from 1956 to 2005, and had seriouslyaffe...
In the complementary relationship (CR) between actual and potential evapotranspiration, wet environment evapotranspiration (Ew) is usually calculatedusing the Priestley-Taylor (P-T) equation. Based on...
On the basis of long time series of climate and discharge in 108 nonhumid catchmentsin China this study analyzes the spatial and temporal variability of annual water-energybalance using the Budyko hyp...
Most physically-based hydrological models rely on either spatially distributed or lumped characterizations oftopography and other spatial variations. Three disturbed hydrological models with di€e...

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