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Gridded fields of changes in discharge due to historical deforestation
and conversion to agriculture from Douglas et al. (2005). This
historical scenario compared discharge (Q) generated from pre-industrial
land cover with discharge derived from contemporary landcover. Change in
Q = difference between river discharge (Q) generated from pre-industrial
land cover (based on WWF Terrestrial Ecoregions of the World (Olson et
al., 2001) with river discharge derived from contemporary landcover.
Historical and contemporary Q was estimated from flow routed RO
generated by the UNH Water Systems Analysis Group Water Balance Model
(WBM) at a 30' (lat x long) spatial resolution (Fekete et al. 2002).
Citations in dataset history.
Data Provided By:
Vorosmarty, C.J.., Water Systems Analysis Group, University of New Hampshire, NH
Content date:
not specified
Citation:
Title: Historical Change In River Discharge due to Deforestation (km3/yr) Credits: Vorosmarty, C.J.., Water Systems Analysis Group, University of New Hampshire, NH Publication Date: 2005 Other Citation Info: Douglas, E. M., K. Sebastian, C. J. Vorosmarty and S. Wood, 2005. The role of tropical forests in supporting biodiversity and hydrologic integrity, Ecological Applications, in review.
Contact Organization:
Water Systems Analysis Group, Complex System Research Center, Institute for the Study of Earth, Oceans and Space, University of New Hampshire, USA
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The Conservation Biology Institute (CBI) provides scientific expertise to support the conservation and recovery of biological diversity in its natural state through applied research, education, planning, and community service.