Vegetation pattern and terrestrial carbon variation in past warm and cold climates

Understanding the transition of biosphere‐atmosphere carbon exchange between glacial and interglacial climates can constrain uncertainties in its future projections. Using an individual‐based dynamic vegetation model, we simulate vegetation distribution and terrestrial carbon cycling in past cold an...

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Published in:Geophysical Research Letters
Main Authors: Lu, Zhengyao, Miller, Paul A., Zhang, Qiong, Warlind, David, Nieradzik, Lars P., Sjolte, Jesper, Li, Qiang, Smith, Benjamin (R19508)
Other Authors: Hawkesbury Institute for the Environment (Host institution)
Format: Article in Journal/Newspaper
Language:English
Published: U.S., Wiley-Blackwell Publishing 2019
Subjects:
Online Access:https://doi.org/10.1029/2019GL083729
http://handle.westernsydney.edu.au:8081/1959.7/uws:52812
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spelling ftunivwestsyd:oai:researchdirect.westernsydney.edu.au:uws_52812 2023-05-15T17:57:44+02:00 Vegetation pattern and terrestrial carbon variation in past warm and cold climates Lu, Zhengyao Miller, Paul A. Zhang, Qiong Warlind, David Nieradzik, Lars P. Sjolte, Jesper Li, Qiang Smith, Benjamin (R19508) Hawkesbury Institute for the Environment (Host institution) 2019 print 11 https://doi.org/10.1029/2019GL083729 http://handle.westernsydney.edu.au:8081/1959.7/uws:52812 eng eng U.S., Wiley-Blackwell Publishing Geophysical Research Letters--0094-8276--1944-8007 Vol. 46 Issue. 14 No. pp: 8133-8143 XXXXXX - Unknown climate changes atmosphere carbon journal article 2019 ftunivwestsyd https://doi.org/10.1029/2019GL083729 2020-12-05T18:32:30Z Understanding the transition of biosphere‐atmosphere carbon exchange between glacial and interglacial climates can constrain uncertainties in its future projections. Using an individual‐based dynamic vegetation model, we simulate vegetation distribution and terrestrial carbon cycling in past cold and warm climates and elucidate the forcing effects of temperature, precipitation, atmospheric CO2 concentration (pCO2), and landmass. Results are consistent with proxy reconstructions and reveal that the vegetation extent is mainly determined by temperature anomalies, especially in a cold climate, while precipitation forcing effects on global‐scale vegetation patterns are marginal. The pCO2 change controls the global carbon balance with the fertilization effect of higher pCO2 linking to higher vegetation coverage, an enhanced terrestrial carbon sink, and increased terrestrial carbon storage. Our results indicate carbon transfer from ocean and permafrost/peat to the biosphere and atmosphere and highlight the importance of forest expansion as a driver of terrestrial ecosystem carbon stock from cold to warm climates. Article in Journal/Newspaper permafrost University of Western Sydney (UWS): Research Direct Geophysical Research Letters 46 14 8133 8143
institution Open Polar
collection University of Western Sydney (UWS): Research Direct
op_collection_id ftunivwestsyd
language English
topic XXXXXX - Unknown
climate changes
atmosphere
carbon
spellingShingle XXXXXX - Unknown
climate changes
atmosphere
carbon
Lu, Zhengyao
Miller, Paul A.
Zhang, Qiong
Warlind, David
Nieradzik, Lars P.
Sjolte, Jesper
Li, Qiang
Smith, Benjamin (R19508)
Vegetation pattern and terrestrial carbon variation in past warm and cold climates
topic_facet XXXXXX - Unknown
climate changes
atmosphere
carbon
description Understanding the transition of biosphere‐atmosphere carbon exchange between glacial and interglacial climates can constrain uncertainties in its future projections. Using an individual‐based dynamic vegetation model, we simulate vegetation distribution and terrestrial carbon cycling in past cold and warm climates and elucidate the forcing effects of temperature, precipitation, atmospheric CO2 concentration (pCO2), and landmass. Results are consistent with proxy reconstructions and reveal that the vegetation extent is mainly determined by temperature anomalies, especially in a cold climate, while precipitation forcing effects on global‐scale vegetation patterns are marginal. The pCO2 change controls the global carbon balance with the fertilization effect of higher pCO2 linking to higher vegetation coverage, an enhanced terrestrial carbon sink, and increased terrestrial carbon storage. Our results indicate carbon transfer from ocean and permafrost/peat to the biosphere and atmosphere and highlight the importance of forest expansion as a driver of terrestrial ecosystem carbon stock from cold to warm climates.
author2 Hawkesbury Institute for the Environment (Host institution)
format Article in Journal/Newspaper
author Lu, Zhengyao
Miller, Paul A.
Zhang, Qiong
Warlind, David
Nieradzik, Lars P.
Sjolte, Jesper
Li, Qiang
Smith, Benjamin (R19508)
author_facet Lu, Zhengyao
Miller, Paul A.
Zhang, Qiong
Warlind, David
Nieradzik, Lars P.
Sjolte, Jesper
Li, Qiang
Smith, Benjamin (R19508)
author_sort Lu, Zhengyao
title Vegetation pattern and terrestrial carbon variation in past warm and cold climates
title_short Vegetation pattern and terrestrial carbon variation in past warm and cold climates
title_full Vegetation pattern and terrestrial carbon variation in past warm and cold climates
title_fullStr Vegetation pattern and terrestrial carbon variation in past warm and cold climates
title_full_unstemmed Vegetation pattern and terrestrial carbon variation in past warm and cold climates
title_sort vegetation pattern and terrestrial carbon variation in past warm and cold climates
publisher U.S., Wiley-Blackwell Publishing
publishDate 2019
url https://doi.org/10.1029/2019GL083729
http://handle.westernsydney.edu.au:8081/1959.7/uws:52812
genre permafrost
genre_facet permafrost
op_relation Geophysical Research Letters--0094-8276--1944-8007 Vol. 46 Issue. 14 No. pp: 8133-8143
op_doi https://doi.org/10.1029/2019GL083729
container_title Geophysical Research Letters
container_volume 46
container_issue 14
container_start_page 8133
op_container_end_page 8143
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