2004
DOI: 10.1002/hyp.5754
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Hydrological regions in monsoon Asia

Abstract: Abstract:Monsoon Asia is characterized by its diversity of natural and social environments. These environments range from humid tropics to arid regions and there exist associated various hydrological phenomena. This paper attempts to characterize the hydrological regions of monsoon Asia based on the water budget calculated using grid-based global datasets. A map of hydrological regions is created by ranking the value of water surplus and deficit. A humid zone with large water surplus extending from Southeast A… Show more

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Cited by 14 publications
(13 citation statements)
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“…The total area of the drainage basin is 1.81 Â10 6 km 2 , or nearly 20% of the total area of China, and it alone sustains a population of 420 million. In the Changjiang basin, annual precipitation (1253 mm yr À1 ) greatly exceeds the evaporation loss (801 mm yr À1 ) (Kondoh et al, 2004). Because of the weathering of the abundant carbonate rocks in the drainage basin, Ca 2+ ($1.5 mM), Mg 2+ ($0.6 mM) and HCO 3 À ($1.9 mM) concentrations are rather high in the river water, while pH is slightly basic ($7.9).…”
Section: The Changjiang River Basinmentioning
confidence: 99%
“…The total area of the drainage basin is 1.81 Â10 6 km 2 , or nearly 20% of the total area of China, and it alone sustains a population of 420 million. In the Changjiang basin, annual precipitation (1253 mm yr À1 ) greatly exceeds the evaporation loss (801 mm yr À1 ) (Kondoh et al, 2004). Because of the weathering of the abundant carbonate rocks in the drainage basin, Ca 2+ ($1.5 mM), Mg 2+ ($0.6 mM) and HCO 3 À ($1.9 mM) concentrations are rather high in the river water, while pH is slightly basic ($7.9).…”
Section: The Changjiang River Basinmentioning
confidence: 99%
“…Most parts of Upper Changjiang basin lie in an area of water surplus, particularly in the north (Kondoh et al, 2004). The exception is its headwater zone on the Tibetan Plateau which is an area of water deficit.…”
Section: The Present Climatementioning
confidence: 99%
“…The result of monthly 0 E analysis has been used together with monthly precipitation and soil water holding capacity ( c W ) on the next step to calculate a E as shown in Figure 2 and the detail could be referred to Thornthwaite and Mather (1957) and Kondoh et al (2004).…”
Section: Actual Evapotranspiration Estimationmentioning
confidence: 99%