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{{Presenters presentation
{{Presenters presentation
|CSDMS meeting abstract presentation=In landscape evolution models, climate change is often assumed to be synonymous with changes in rainfall. In many climate changes, however, the dominant driver of landscape evolution is changes in vegetation cover. In this talk I review case studies that attempt to quantify the impact of vegetation changes on landscape evolution, including examples from hillslope/colluvial, fluvial, and aolian environments, spatial scales of ~10 m to whole continents, and time scales from decadal to millennial. Particular attention is paid to how to parameterize models using paleoclimatic and remote sensing data.
|CSDMS meeting abstract presentation=In landscape evolution models, climate change is often assumed to be synonymous with changes in rainfall. In many climate changes, however, the dominant driver of landscape evolution is changes in vegetation cover. In this talk I review case studies that attempt to quantify the impact of vegetation changes on landscape evolution, including examples from hillslope/colluvial, fluvial, and aolian environments, spatial scales of ~10 m to whole continents, and time scales from decadal to millennial. Particular attention is paid to how to parameterize models using paleoclimatic and remote sensing data.
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{{Presenters additional material
{{Presenters additional material
|Working group member=Terrestrial Working Group
|Working group member=Terrestrial Working Group
|CSDMS meeting presentation=Jon_Pelletier_CSDMS_2016_annual_meeting.pdf
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Latest revision as of 09:35, 7 August 2018

Joint CSDMS-SEN annual meeting 2016: Capturing Climate Change


Modeling the Impact of Vegetation Changes on Erosion Rates and Landscape Evolution



Jon Pelletier

University of Arizona, United States
jdpellet@email.arizona.edu

Abstract
In landscape evolution models, climate change is often assumed to be synonymous with changes in rainfall. In many climate changes, however, the dominant driver of landscape evolution is changes in vegetation cover. In this talk I review case studies that attempt to quantify the impact of vegetation changes on landscape evolution, including examples from hillslope/colluvial, fluvial, and aolian environments, spatial scales of ~10 m to whole continents, and time scales from decadal to millennial. Particular attention is paid to how to parameterize models using paleoclimatic and remote sensing data.



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Of interest for:
  • Terrestrial Working Group