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dc.contributor.authorFeddema, Johannes J.
dc.contributor.authorFreire, Sergio Carneiro
dc.date.accessioned2012-05-10T16:49:26Z
dc.date.available2012-05-10T16:49:26Z
dc.date.issued2001
dc.identifier.citationFeddema, J.J and S. Freire (2001): Soil degradation, global warming and climate impacts.  Climate Research 17(2): 209-216.en_US
dc.identifier.urihttp://hdl.handle.net/1808/9388
dc.description(c) Inter Research. Resale or republication not permitted without written consent of the publisher.en_US
dc.description.abstractA water balance model is used to assess the relative impacts of global warming and soil degradation scenarios on water resources in the future. Results indicate that overall global warming will have a more widespread and greater impact on climate change. However soil degradation could also play a significant role in water resource issues in the future. Based on the model results, wet and dry climate regions are particularly susceptible to impacts from soil degradation. In general, reduced water holding capacities will result in increased water runoff during wet periods, which will result in higher overland flow rates and reduced recharge rates to groundwater. Water lost to runoff will also increase deficits during dry periods, in effect increasing the duration and intensity of dry periods.en_US
dc.language.isoen_USen_US
dc.publisherInter Researchen_US
dc.relation.isversionofhttp://www.int-res.com/articles/cr/17/c017p209.pdf
dc.titleSoil degradation, global warming and climate impactsen_US
dc.typeArticle
kusw.kuauthorFeddema, Johannes J.
kusw.kudepartmentGeographyen_US
kusw.oaversionScholarly/refereed, publisher version
kusw.oapolicyThis item does not meet KU Open Access policy criteria.
dc.rights.accessrightsopenAccess


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