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Titlebook: Linking Climate Change to Land Surface Change; Sue J. McLaren,Dominic R. Kniveton Book 2000 Springer Science+Business Media B.V. 2000 Clim

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Desiccation in the Sahelnd that the annual rainfall for the region was largely a product of poor sampling east to west until sufficient stations were reporting data from 1970. These results raise questions over the use of regional statistics such as rainfall anomalies and the fitting of regional trend lines to depict clima
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Hydrological Response of Desert Margins to Climatic Change: The Effect of Changing Surface Propertie can be expected to exercise strong influence on infiltration, runoff and soil moisture. An aspect not yet answered is how much sand or loess deposition is required to affect the hydrological regime and related water resources. In order to check the effect of thin topsoil sand or fine-grained layers
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Examining Links between Climate Change and Landslide Activity Using GCMS a significant activity decrease due to increasing winter temperature and reduced snow storage while precipitation changes do not show a clear trend. The projections for Wellington indicate fewer events of high landslide probability in the hemispherical winter due to decreased precipitation.
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Aeolian Geomorphic Response to Climate Change: An Example from the Estancia Valley, Central New Mexievailing westerly winds, consistent in direction, but marked by gustiness. Accumulation was episodic, punctuated by periods of stability with weak mollisol development. Charcoal from one mollisol dates to ca. 8,500 BP. After this time, the dome dunes attained their greatest relief and were capped by
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Relict Cryogenic Mounds in the UK as Evidence of Climate Changeorming. Many relict cryogenic mounds in the UK have been interpreted as the remains of hydraulic pingos, features which in contemporary cold climate areas indicate either discontinuous permafrost (mean annual air temperature (MAAT) of ≤ -3° C) or continuous permafrost (MAAT of ≤ -7° C). Some of thes
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