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MODELING SOIL EROSION BY WATER l 2 John Boardman and David Favis-Mortlock 1 School of Geography and Environmental Change Unit Mansfield Road University of Oxford Oxford OX1 3TB UK 2 Environmental Change Unit University of Oxford 5 South Parks Road Oxford OX1 3UB UK Introduction This volume is the Proceedings of the NATO Advanced Research Workshop 'Global Change: Modelling Soil Erosion by Water', which was held on I-14th September 1995, at the University of Oxford, UK. The meeting was also one of a series organised by the IGBP- 1 GCTE Soil Erosion Network, which is a component of GCTE's Land Degradation Task (3.3.2) (Ingram et aI., 1996; Valentin, this volume). One aim of the GCTE Soil Erosion Network is to evaluate the suitability of existing soil erosion models for predicting the possible impacts of global change upon soil erosion. 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The ice dome discharged its ice in all directions, northward into the deep Arctic Basin, southward and westward onto the mainland of west-central North Siberia, the northern Russian Plain, and over the Barents shelf into the Norwegian-Greenland Sea On the Barents shelf, the Kara ice dome merged with the Scandinavian ice dome. In the Arctic Basin the discharged ice floated and eventually coalesced with the floating glacier ice of the North-American provenance giving rise to the Central-Arctic ice shelf. Along its southern margin, the Kara ice dome impounded the northward flowing rivers, causing the formation of large proglaciallakes and their integration into a transcontinental meltwater drainage system. Despite the constant increase in corroborating evidence, the concept of a Kara ice dome is still considered debatable, and the ice dome itself problematic. As a result, a paleogeographic uncertainty takes place, which is aggravated by the fact that a great deal of existing knowledge, no matter how broadly accepted, is based on ambiguous interpretations of the data, most of which are published in Russian and, therefore, not easily available to western scientists.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52650672718097,"sku":"NLS9783642850189","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9783642850189.jpg?v=1762128601"},{"product_id":"soil-responses-to-climate-change-book-mark-da-rounsevell-9783642792205","title":"Soil Responses to Climate Change","description":"Soils will play a central role in mediating the impact of climate change on natural and managed ecosystems.  The book addresses the various responses of soil processes and properties to environmental change and highlights their contribution to the proper understanding of ecosystem behaviour. Topics include: Soil hydrology; landscape evolution; salinisation; desertification; soil nitrogen dynamics; soil carbon; soil microbiology; soil erosion; crop modelling.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52650690117905,"sku":"NLS9783642792205","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9783642792205.jpg?v=1762128650"},{"product_id":"tropospheric-chemistry-of-ozone-in-the-polar-regions-book-h-niki-9783642782138","title":"The Tropospheric Chemistry of Ozone in the Polar Regions","description":"The Arctic troposphere (0 to ca. 8 km) plays an important role in environmental concerns for global change. It is a unique chemical reactor influenced by human activity and the Arctic ocean. 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Between complete dark in February and complete light in April, a number of chemical changes in the lower troposphere take place.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52655406907665,"sku":"NLS9783642782138","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9783642782138.jpg?v=1762220435"},{"product_id":"long-term-climatic-variations-book-jean-claude-duplessy-9783642790683","title":"Long-Term Climatic Variations","description":"Climate is the most important component of the Earth's environment and climatic fluctuations have a strong impact on water supplies, vegetation, energy use etc. Thus our understanding of the climatic system is of utmost importance. Leading experts in the field of climate modelling and paleoclimatology present the most recent methods for reconstructing past climatic variations and for modelling the climatic system and its evolution. The first of three parts is devoted to the climatic system and the physical basis for its modelling; the second summarizes the evolution of the global atmosphere, the ocean, the continents, the biosphere, and the ice sheets during recent climatic cycles; the last part focusses on the understanding of past and future climatic changes.","brand":"WoB","offers":[{"title":"- \/ - \/ INTERNAL","offer_id":52655429386513,"sku":null,"price":0.0,"currency_code":"GBP","in_stock":true},{"title":"GB \/ NEW \/ INGRAM","offer_id":52655429845265,"sku":"NLS9783642790683","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9783642790683.jpg?v=1762220551"},{"product_id":"biodiversity-temperate-ecosystems-and-global-change-book-timothy-jb-boyle-9783642789748","title":"Biodiversity, Temperate Ecosystems, and Global Change","description":"Reviewed here is the current state of knowledge concerning the relationship between global change and biodiversity of temperate ecosystems. 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The present volume distinguishes itself from earlier publications by highlighting several interrelated environmental stresses that are changing in intensity as the climate warms in response to the accumulation of 'greenhouse' gases. The stresses examined at the NATO Advanced Research Workshop upon which this book is based include atmospheric pollutants, flooding and sub- mergence, drought and cold. In future, successful farming or landscape management will ultimately depend on strategies that offset the effects of these and other environmental constraints, while exploiting more favourable features. However, the to predicted speed of climate change may exceed the rate at which new approaches farming, forestry, landscape management and genetic conservation can be developed through experience and retroactive response. The alternative is to anticipate future needs and thus identify appropriate management and legislative strategies by research and discussion. 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However, many authors have taken care to emphasise that interactions between the changing combinations of stresses pose particular problems for plants and plant communities.","brand":"WoB","offers":[{"title":"GB \/ NEW \/ INGRAM","offer_id":52655974908177,"sku":"NLS9783642785351","price":0.0,"currency_code":"GBP","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0784\/4072\/6801\/files\/9783642785351.jpg?v=1762222884"}],"url":"https:\/\/www.worldofbooks.com\/collections\/nato-asi-subseries-i-book-series.oembed","provider":"World of Books ","version":"1.0","type":"link"}