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Master
Australie
Spatial and temporal variability of transpiration in the Gwydir and Namoi catchments from 2000-2004
Titre : Spatial and temporal variability of transpiration in the Gwydir and Namoi catchments from 2000-2004
Auteur : Weidemann, Stephanie Lyn
Université de soutenance : Australian National University
Grade : Master of Environmental Science 2006
Résumé
Vegetation links the atmosphere and the hydrologic cycle. Rapid advances in
satellite technology have allowed scientists to monitor changes in vegetation
productivity through time. Data from the moderate resolution imaging spectrometer
(MODIS) was used to estimate transpiration fluxes in the Gwydir and Namoi catchment
areas in northern New South Wales Australia from 6 April 2000 to 31December2004.
The MODIS NDVI imagery was used to compare differences in gross primary
productivity (GPP) and to estimate catchment scale transpiration fluxes between
croplands and non croplands. Two solar radiation parameters were estimated ; daily
solar irradiance (Rs) grids were created in ESOCLIM and the global solar irradiance
(R0 ) using Roderick (1999). These outputs were then used to estimate the diffuse
fraction of radiation (Rd/Rs) reaching the vegetation canopy. The fraction of
photosynthetic radiation (jP AR) was estimated from the MO DIS NDVI data. Then the
diffuse fraction of radiation was used to yield canopy efficiency (e) (mol C0 2 mor1
PAR). Canopy efficiency and the Rd/Rs were used to estimate GPP using a radiation use
efficiency approach. Monthly GPP grids were used to estimate monthly transpiration
fluxes from May 2000 to December 2004. Then the monthly transpiration grids were
summed to yield annual catchment scale transpiration fluxes from 2001-2004.
Temporal estimates of transpiration fluxes display characteristics of wet and dry years.
Transpiration fluxes increased with elevation. Vegetation on southerly aspects had
higher transpiration rates due to increased radiation received at the surface. Higher
annual transpiration fluxes were observed in non cropland pixels and lower annual
transpiration fluxes occurred in cropland pixels. Intra-annual and inter-annual patterns
of transpiration fluxes were detected from individual pixel analysis. Catchment scale
estimates of transpiration fluxes are useful in monitoring the state and productivity of
agricultural crops, observing the spatial arrangement of transpiration fluxes across
catchments, observing differences in transpiration fluxes for contrasting vegetation
types, and monitoring changes in water use efficiency of different vegetation types (e.g.
forest versus cropland). Estimates of catchment scale transpiration fluxes have
important implications for catchment management in that it provides an explicit
functional link between land use/land cover change and catchment-level water budgets.
Page publiée le 29 janvier 2021