Climate change detection over different land surface vegetation classes

Biosystem variations may occur as a consequence of climate change. Analysis of both modern and paleo-proxy climate data indicates several places on Earth that show biosytem variations possibly resulting from changes in climate. In this thesis, a global land cover classification data set is used to p...

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Bibliographic Details
Main Author: Dang, Hongyan
Other Authors: Weaver, Andrew
Format: Thesis
Language:English
Published: 2005
Subjects:
Online Access:http://hdl.handle.net/1828/1775
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spelling ftuvicpubl:oai:dspace.library.uvic.ca:1828/1775 2023-05-15T13:49:38+02:00 Climate change detection over different land surface vegetation classes Dang, Hongyan Weaver, Andrew 2005 application/pdf http://hdl.handle.net/1828/1775 English en eng http://hdl.handle.net/1828/1775 Available to the World Wide Web climate change global warming UVic Subject Index::Sciences and Engineering::Earth and Ocean Sciences Thesis 2005 ftuvicpubl 2022-05-19T06:14:12Z Biosystem variations may occur as a consequence of climate change. Analysis of both modern and paleo-proxy climate data indicates several places on Earth that show biosytem variations possibly resulting from changes in climate. In this thesis, a global land cover classification data set is used to partition the globe into seven re¬gions to study surface temperature changes over different vegetation/surface classes. Statistically significant warming is found from the year 1900 over all regions (except for the ice sheets over Greenland and Antarctica). Outputs from three coupled cli¬mate models (CGCM2, HadCM2 and Parallel Climate Model) are then adopted to examine the detection and attribution of surface temperature trends over the vari¬ous vegetation classes for the past half century. An anthropogenic warming trend is detected in six of the seven regions, which means that anthropogenic activities may have caused detectable influences in the regional surface temperature changes of the past half century. Observed trends are consistent with those simulated in response to greenhouse gas and sulphate aerosol forcing except over tropical forest and water where the models overestimate the warming. The similarity between the resultant scaling factors for each region from the different models underscores the reliability of our detection results. Thesis Antarc* Antarctica Greenland University of Victoria (Canada): UVicDSpace Greenland
institution Open Polar
collection University of Victoria (Canada): UVicDSpace
op_collection_id ftuvicpubl
language English
topic climate change
global warming
UVic Subject Index::Sciences and Engineering::Earth and Ocean Sciences
spellingShingle climate change
global warming
UVic Subject Index::Sciences and Engineering::Earth and Ocean Sciences
Dang, Hongyan
Climate change detection over different land surface vegetation classes
topic_facet climate change
global warming
UVic Subject Index::Sciences and Engineering::Earth and Ocean Sciences
description Biosystem variations may occur as a consequence of climate change. Analysis of both modern and paleo-proxy climate data indicates several places on Earth that show biosytem variations possibly resulting from changes in climate. In this thesis, a global land cover classification data set is used to partition the globe into seven re¬gions to study surface temperature changes over different vegetation/surface classes. Statistically significant warming is found from the year 1900 over all regions (except for the ice sheets over Greenland and Antarctica). Outputs from three coupled cli¬mate models (CGCM2, HadCM2 and Parallel Climate Model) are then adopted to examine the detection and attribution of surface temperature trends over the vari¬ous vegetation classes for the past half century. An anthropogenic warming trend is detected in six of the seven regions, which means that anthropogenic activities may have caused detectable influences in the regional surface temperature changes of the past half century. Observed trends are consistent with those simulated in response to greenhouse gas and sulphate aerosol forcing except over tropical forest and water where the models overestimate the warming. The similarity between the resultant scaling factors for each region from the different models underscores the reliability of our detection results.
author2 Weaver, Andrew
format Thesis
author Dang, Hongyan
author_facet Dang, Hongyan
author_sort Dang, Hongyan
title Climate change detection over different land surface vegetation classes
title_short Climate change detection over different land surface vegetation classes
title_full Climate change detection over different land surface vegetation classes
title_fullStr Climate change detection over different land surface vegetation classes
title_full_unstemmed Climate change detection over different land surface vegetation classes
title_sort climate change detection over different land surface vegetation classes
publishDate 2005
url http://hdl.handle.net/1828/1775
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
genre_facet Antarc*
Antarctica
Greenland
op_relation http://hdl.handle.net/1828/1775
op_rights Available to the World Wide Web
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