Your search found 4 records
1 van den Hurk, B. J. J. M.; Bastiaanssen, W. G. M.; Pelgrum, H.; van Meijgaard, E. 1997. A new methodology for assimilation of initial soil moisture fields in weather prediction models using meteostat and NOAA data. Journal of Applied Meteorology and Climatology, September:1271-1283.
Remote sensing ; Satellite surveys ; Soil moisture ; Climate ; Forecasting ; Evaporation / Iberian Peninsula
(Location: IWMI-HQ Call no: P 5053 Record No: H023867)
(1.50 MB)
2 Mohamed, Yasir Abbas; Savenije, H. H.; Bastiaanssen, W. G. M.; van den Hurk, B. J. J. M.. 2006. New lessons on the Sudd hydrology learned from remote sensing and climate modeling. Hydrology and Earth System Sciences, 10(4):507-518.
(Location: IWMI-HQ Call no: IWMI 551.48 G146 MOH Record No: H039748)
http://www.hydrol-earth-syst-sci.net/10/507/2006/hess-10-507-2006.pdf
https://vlibrary.iwmi.org/pdf/H039748.pdf
https://vlibrary.iwmi.org/pdf/H039748.pdf
3 Mohamed, Yasir Abbas; van den Hurk, B. J. J. M.; Savenije, H. H. 2007. Moisture recycling over the Nile Basin. In Reducing the Vulnerability of Societies to Water Related Risks at the Basin Scale: Proceedings of the Third International Symposium on Integrated Water Resources Management, Bochum, Germany, 26-28 September 2006. IAHS publication 317. pp.18-23.
River basins ; Moisture content ; Recycling ; Evaporation ; Precipitation ; Climate ; Models ; Wetlands / Middle East / Nile Basin
(Location: IWMI-HQ Call no: IWMI 551.57 GG30 MOH Record No: H039749)
4 Mohamed, Y. A.; Bastiaanssen, W. G. M.; Savenije, H. H. G.; van den Hurk, B. J. J. M.; Finlayson, Max C. 2012. Wetland versus open water evaporation: an analysis and literature review. Physics and Chemistry of the Earth, 47-48:114-121. [doi: https://doi.org/10.1016/j.pce.2011.08.005]
Wetlands ; Evaporation ; Evapotranspiration ; Literature reviews ; Vegetation ; Climate change ; Water balance
(Location: IWMI HQ Call no: e-copy only Record No: H045933)
(1.33 MB)
Is the total evaporation from a wetland surface (including: open water evaporation, plant transpiration and wet/dry soil evaporation) similar, lower, or higher than evaporation from an open water surface under the same climatic conditions? This question has been the subject of long debate; the literature does not show a consensus. In this paper we contribute to the discussion in two steps. First, we analyse the evaporation from a wetland with emergent vegetation (Ea) versus open water evaporation (Ew) by applying the Penman–Monteith equation to identical climate input data, but with different biophysical characteristics of each surface. Second, we assess the variability of measured Ea/Ew through a literature review of selected wetlands around the globe.We demonstrate that the ratio Ea/Ew is site-specific, and a function of the biophysical properties of the wetland surface, which can also undergo temporal variability depending on local hydro-climate conditions. Second, we demonstrate that the Penman–Monteith model provides a suitable basis to interpret Ea/Ew variations. This implies that the assumption of wetland evaporation to behave similar to open water bodies is not correct. This has significant implications for the total water consumption and water allocation to wetlands in river basin management.
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