{"id":189732,"date":"2017-04-27T02:15:46","date_gmt":"2017-04-27T06:15:46","guid":{"rendered":"http:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/new-tool-for-understanding-landscape-evolution-in-drylands-eos\/"},"modified":"2017-04-27T02:15:46","modified_gmt":"2017-04-27T06:15:46","slug":"new-tool-for-understanding-landscape-evolution-in-drylands-eos","status":"publish","type":"post","link":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/evolution\/new-tool-for-understanding-landscape-evolution-in-drylands-eos\/","title":{"rendered":"New Tool for Understanding Landscape Evolution in Drylands &#8211; Eos"},"content":{"rendered":"<p><p>    Combining vegetation distribution models and sediment transport    models offers a better understanding of how dryland    environments change in response to different factors.  <\/p>\n<p>    Drylands compose more than 40% of Earths surface. Although they are    found on every continent and are tremendously diverse, a common    feature of drylands is sparse vegetation and expanses of bare    ground such as soil or sand. In such a context, the wind plays    a significant role in moving loose sediments and shaping the    landscape.  <\/p>\n<p>    Understanding the processes of landscape evolution is important    for the management of arid and semiarid areas upon which people    depend for their livelihoods. But a long-standing problem in    drylands research has been quantifying the transport of    sediment by wind in the presence of vegetation and how this    influences landscape evolution. For example, wind blowing toward a single tree, a    cluster of low shrubs, or an expanse of patchy grass will have    different effects in terms of the location and severity of    erosion and the location and shape of sediment deposition.  <\/p>\n<p>    However, predicting exactly what will happen is complex because    of the range of factors at play. There are natural variables    such as the distribution, type, and size of vegetation; the    direction, speed, and consistency of wind; and the frequency,    duration, and intensity of rainfall. Human influences are also    at play, including growing crops on the land, grazing animals,    and setting fire to vegetation, all of which change the    availability of sediment and the behavior of wind as it passes    over the landscape.  <\/p>\n<p>    Researchers use awide range of models to simulate what    would happen in different conditions, but these models have    limitations when scientists try to understandlocalized    variations. Mayaud et al. propose a new    approach combining two types of models: those that handle    vegetation distribution and those that handle sediment    transport. The authors describe the technical aspects of their    new Vegetation and Sediment Transport model (ViSTA) and the    verification tests carried out. These showed that the model    could accurately replicate different physical characteristics    of dryland environments at various scales and in response to    environmental changes such as fire and grazing.  <\/p>\n<p>    The next step was to carry out an experiment to test the model.    For this the authors chose a particular type of dryland    environment, a nebkha dune field. Using empirical field data on    rainfall and wind, they compared the landscape evolution    generated by the model with measurements at a field site on the    Skeleton Coast in Namibia. The size and spacing of landforms    produced by the model were found to accurately reflect real    features, thus suggesting the promising potential of this    model.  <\/p>\n<p>    Drylands are home to more than 2 billion people worldwide who    depend on the environment for their food and livelihoods.    However, many dryland environments are suffering from    degradation and desertification in the face of multiple    pressures, including population increase and pressure on water    resources, overfarming and soil depletion, and changing    precipitation patterns due to climate change.  <\/p>\n<p>    As we move toward the end of the United Nations Decade for Deserts and the Fight    Against Desertification (20102020), this research    contributes to a better understanding of dryland landscape    processes. The new model is a versatile tool that can be used    to simulate a variety of dryland environments and understand    the spatial effects of different environmental stresses,    whether natural or anthropogenic. (Journal of Geophysical    Research: Earth Surface, <a href=\"https:\/\/doi.org\/10.1002\/2016JF004096\" rel=\"nofollow\">https:\/\/doi.org\/10.1002\/2016JF004096<\/a>, 2017)  <\/p>\n<p>    Jenny Lunn, Contributing Writer  <\/p>\n<p><!-- Auto Generated --><\/p>\n<p>Go here to read the rest: <\/p>\n<p><a target=\"_blank\" rel=\"nofollow\" href=\"https:\/\/eos.org\/research-spotlights\/new-tool-for-understanding-landscape-evolution-in-drylands\" title=\"New Tool for Understanding Landscape Evolution in Drylands - Eos\">New Tool for Understanding Landscape Evolution in Drylands - Eos<\/a><\/p>\n","protected":false},"excerpt":{"rendered":"<p> Combining vegetation distribution models and sediment transport models offers a better understanding of how dryland environments change in response to different factors. Drylands compose more than 40% of Earths surface. Although they are found on every continent and are tremendously diverse, a common feature of drylands is sparse vegetation and expanses of bare ground such as soil or sand <a href=\"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/evolution\/new-tool-for-understanding-landscape-evolution-in-drylands-eos\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":6,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[187748],"tags":[],"class_list":["post-189732","post","type-post","status-publish","format-standard","hentry","category-evolution"],"_links":{"self":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/posts\/189732"}],"collection":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/users\/6"}],"replies":[{"embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/comments?post=189732"}],"version-history":[{"count":0,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/posts\/189732\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/media?parent=189732"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/categories?post=189732"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.euvolution.com\/prometheism-transhumanism-posthumanism\/wp-json\/wp\/v2\/tags?post=189732"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}