Water-heat effects of vegetation cover change in southwest Karst areas - Gao, Jiangbo;Wang, Huan;Hou, Wenjuan
29,99 €
inkl. MwSt.
Versandkostenfrei*
Versandfertig in 6-10 Tagen
  • Broschiertes Buch

Vegetation cover, as an essential composition of terrestrial ecosystem and the principal part of soil-vegetation-atmosphere continuum, has been proved to be sensitive to climate and land-use changes. And further, variations in morphology and structure of vegetation cover can influence the land surface hydrothermal process, and then affect the material and energy cycle of ecosystem. The unique geological conditions and the binary hydrological structure of surface and ground aggravate the sensibility of ecosystem in Karst region of Southwestern China. Along with the prominent human-land…mehr

Andere Kunden interessierten sich auch für
Produktbeschreibung
Vegetation cover, as an essential composition of terrestrial ecosystem and the principal part of soil-vegetation-atmosphere continuum, has been proved to be sensitive to climate and land-use changes. And further, variations in morphology and structure of vegetation cover can influence the land surface hydrothermal process, and then affect the material and energy cycle of ecosystem. The unique geological conditions and the binary hydrological structure of surface and ground aggravate the sensibility of ecosystem in Karst region of Southwestern China. Along with the prominent human-land conflict, Karst rock desertification occurs consequently in this region. Based on the general idea of pattern-process-effect, the study was conducted to investigate the tempo-spatial variations in vegetation cover, the driving mechanism, and their hydrothermal effects. Specifically, the tempo-spatial variation in vegetation cover and their relationships with climatic factors and landscape structure of land use in the Karst region of Southwestern China were studied.
Autorenporträt
Jiangbo Gao, PhD, Major: Physical Geography, Chinese Academy of Sciences, mainly focus on the water and heat transfer in Karst region of southwest China and the land-atmosphere interaction in East Asia.