2012
DOI: 10.2747/0272-3646.33.6.561
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Topography-Controlled Soil Water Content and the Coexistence of Forest and Steppe in Northern China

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Cited by 46 publications
(32 citation statements)
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“…In addition to the MAP gradient, the amount of available water for plants has been shown to strongly depend on topography‐controlled evaporation as well as on the infiltration ability of soil (Dulamsuren & Hauck ; Liu et al. ). Despite the MAP gradient, available water for plants strongly depended on topography‐controlled evaporation as well as the infiltration ability of soil (Dulamsuren & Hauck ; Liu et al.…”
Section: Discussionmentioning
confidence: 99%
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“…In addition to the MAP gradient, the amount of available water for plants has been shown to strongly depend on topography‐controlled evaporation as well as on the infiltration ability of soil (Dulamsuren & Hauck ; Liu et al. ). Despite the MAP gradient, available water for plants strongly depended on topography‐controlled evaporation as well as the infiltration ability of soil (Dulamsuren & Hauck ; Liu et al.…”
Section: Discussionmentioning
confidence: 99%
“…Despite the MAP gradient, available water for plants strongly depended on topography‐controlled evaporation as well as the infiltration ability of soil (Dulamsuren & Hauck ; Liu et al. ).…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…In weathering, surface area is a fundamental determinant of process (e.g., Pope, 1995). In water resources, areal extent will affect quantities such as raindrop impacts per unit area, evaporation, surface interaction and infiltration rates, flow concentration, and channel density (e.g., Liu et al, 2012). The volume of soil for water storage and plant roots also is affected, but negligibly over long slopes.…”
Section: Introductionmentioning
confidence: 99%
“…The East Asia steppe (covering between roughly 36 • 7 N-50 • 48 N and 104 • 18 E-124 • 21 E), which spans Northern China, Eastern Mongolia, and Southern Siberia of Russia (Figure 1), is dominated by semi-arid grasslands with embedded forest and scrub patches [26]. It has a total area of approximately 805,000 km 2 with complex geomorphic types (e.g., treeless flatlands, gently rolling hills, wetlands, and mountains).…”
Section: The Study Areamentioning
confidence: 99%