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Titel Trends in 20th Century Global Rainfall Interception as Simulated by a Dynamic Global Vegetation Model: Implications for Global Water Resources
VerfasserIn Steve Murray, Colin Prentice
Konferenz EGU General Assembly 2010
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 12 (2010)
Datensatznummer 250040435
 
Zusammenfassung
In order to monitor and forecast regions of potential freshwater stress and surplus, a comprehensive understanding and quantification of the global hydrological cycle and its components is needed. Such work should lead to better constrained estimates of freshwater fluxes and facilitate the identification of regions requiring enhanced water management. The research described here aims to quantify the contribution of climate- and CO2-induced changes in the physical properties of the land surface, mediated by biological processes. Global climate change is expected to bring about substantial latitudinal and altitudinal shifts in vegetation cover. Shifts in species distribution, the potential of increased leaf area index (LAI) but also reduced stomatal conductance in response to rising concentrations of CO2, and variability in precipitation, can all influence rates and spatial variability of the interception-throughfall balance. These effects will have implications for runoff generation and the partitioning between ‘green’ and ‘white’ water fluxes. The Land Processes eXchange Dynamic Global Vegetation Model (LPX-DGVM, a development of the LPJ model) was evaluated in terms of its interception component and used to simulate trends in global relative throughfall from 1901-2006, as this is directly relevant for runoff. We estimate that mean global annual runoff was reduced by 164 ±18 km3/year during the twentieth century as a result of biophysical changes controlling relative throughfall generation. Widespread decreases in relative throughfall of typically between 0 and -1% are evident between 1901-1953 and 1954-2006. Changes of up to