2016
DOI: 10.1016/j.rse.2016.01.002
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The spatiotemporal patterns of vegetation coverage and biomass of the temperate deserts in Central Asia and their relationships with climate controls

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Cited by 165 publications
(73 citation statements)
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“…Recently, Zhang et al . () show that vast desert areas in western Central Asia have lost most of its surface biomass after a prolonged drought in the late 1990s. In such dry conditions, lack of recharge to the groundwater that has been the primary source of water supply for natural oases in foothills of mountains removes lifeline for surface vegetation and associated ecosystems.…”
Section: Introductionmentioning
confidence: 99%
“…Recently, Zhang et al . () show that vast desert areas in western Central Asia have lost most of its surface biomass after a prolonged drought in the late 1990s. In such dry conditions, lack of recharge to the groundwater that has been the primary source of water supply for natural oases in foothills of mountains removes lifeline for surface vegetation and associated ecosystems.…”
Section: Introductionmentioning
confidence: 99%
“…In doing so the aim is the identification of an analytical relationship between on-the-ground AGB estimates and spectral indices sensitive to photosynthetically active radiation and scaling with amount of biomass [39][40][41][42]. A vegetation index is generally derived from the spectral reflectance of two or more bands, and proportional to the value of biophysical parameters like leaf area index (LAI), net primary productivity (NPP), and absorbed photosynthetically active radiation (APAR) [43].…”
Section: Introductionmentioning
confidence: 99%
“…The reason for such discrepancy was that different vegetation types had very different spectral reflectances in the red and near-infrared wavebands, as defined in the NDVI34. Another underlying reason was that different vegetation types had different sensitivities to climate factors, and vegetation that was especially sensitive to hydrothermal conditions was likely to fluctuate markedly in NDVI and biomass35. For example, Li and Yang5 found that desert steppe was most strongly affected by warmer temperatures, hence the decreased NDVI that occurred mainly in drier summers (May and June) in inner Mongolia.…”
Section: Discussionmentioning
confidence: 99%