Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3

We investigated changes in tropical climate and vegetation cover associated with abrupt climate change during Heinrich Event 1 (HE1, ca. 17.5 ka BP) using two different global climate models: the University of Victoria Earth System-Climate Model (UVic ESCM) and the Community Climate System Model ver...

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Published in:Climate of the Past
Main Authors: D. Handiani, A. Paul, M. Prange, U. Merkel, L. Dupont, X. Zhang
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2013
Subjects:
Online Access:https://doi.org/10.5194/cp-9-1683-2013
https://doaj.org/article/88d6b23204724fb5b04b2c5d3405a305
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spelling ftdoajarticles:oai:doaj.org/article:88d6b23204724fb5b04b2c5d3405a305 2023-05-15T17:31:35+02:00 Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3 D. Handiani A. Paul M. Prange U. Merkel L. Dupont X. Zhang 2013-07-01T00:00:00Z https://doi.org/10.5194/cp-9-1683-2013 https://doaj.org/article/88d6b23204724fb5b04b2c5d3405a305 EN eng Copernicus Publications http://www.clim-past.net/9/1683/2013/cp-9-1683-2013.pdf https://doaj.org/toc/1814-9324 https://doaj.org/toc/1814-9332 doi:10.5194/cp-9-1683-2013 1814-9324 1814-9332 https://doaj.org/article/88d6b23204724fb5b04b2c5d3405a305 Climate of the Past, Vol 9, Iss 4, Pp 1683-1696 (2013) Environmental pollution TD172-193.5 Environmental protection TD169-171.8 Environmental sciences GE1-350 article 2013 ftdoajarticles https://doi.org/10.5194/cp-9-1683-2013 2022-12-31T11:21:32Z We investigated changes in tropical climate and vegetation cover associated with abrupt climate change during Heinrich Event 1 (HE1, ca. 17.5 ka BP) using two different global climate models: the University of Victoria Earth System-Climate Model (UVic ESCM) and the Community Climate System Model version 3 (CCSM3). Tropical South American and African pollen records suggest that the cooling of the North Atlantic Ocean during HE1 influenced the tropics through a southward shift of the rain belt. In this study, we simulated the HE1 by applying a freshwater perturbation to the North Atlantic Ocean. The resulting slowdown of the Atlantic Meridional Overturning Circulation was followed by a temperature seesaw between the Northern and Southern Hemispheres, as well as a southward shift of the tropical rain belt. The shift and the response pattern of the tropical vegetation around the Atlantic Ocean were more pronounced in the CCSM3 than in the UVic ESCM simulation. For tropical South America, opposite changes in tree and grass cover were modeled around 10° S in the CCSM3 but not in the UVic ESCM. In tropical Africa, the grass cover increased and the tree cover decreased around 15° N in the UVic ESCM and around 10° N in the CCSM3. In the CCSM3 model, the tree and grass cover in tropical Southeast Asia responded to the abrupt climate change during the HE1, which could not be found in the UVic ESCM. The biome distributions derived from both models corroborate findings from pollen records in southwestern and equatorial western Africa as well as northeastern Brazil. Article in Journal/Newspaper North Atlantic Directory of Open Access Journals: DOAJ Articles Climate of the Past 9 4 1683 1696
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
spellingShingle Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
D. Handiani
A. Paul
M. Prange
U. Merkel
L. Dupont
X. Zhang
Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3
topic_facet Environmental pollution
TD172-193.5
Environmental protection
TD169-171.8
Environmental sciences
GE1-350
description We investigated changes in tropical climate and vegetation cover associated with abrupt climate change during Heinrich Event 1 (HE1, ca. 17.5 ka BP) using two different global climate models: the University of Victoria Earth System-Climate Model (UVic ESCM) and the Community Climate System Model version 3 (CCSM3). Tropical South American and African pollen records suggest that the cooling of the North Atlantic Ocean during HE1 influenced the tropics through a southward shift of the rain belt. In this study, we simulated the HE1 by applying a freshwater perturbation to the North Atlantic Ocean. The resulting slowdown of the Atlantic Meridional Overturning Circulation was followed by a temperature seesaw between the Northern and Southern Hemispheres, as well as a southward shift of the tropical rain belt. The shift and the response pattern of the tropical vegetation around the Atlantic Ocean were more pronounced in the CCSM3 than in the UVic ESCM simulation. For tropical South America, opposite changes in tree and grass cover were modeled around 10° S in the CCSM3 but not in the UVic ESCM. In tropical Africa, the grass cover increased and the tree cover decreased around 15° N in the UVic ESCM and around 10° N in the CCSM3. In the CCSM3 model, the tree and grass cover in tropical Southeast Asia responded to the abrupt climate change during the HE1, which could not be found in the UVic ESCM. The biome distributions derived from both models corroborate findings from pollen records in southwestern and equatorial western Africa as well as northeastern Brazil.
format Article in Journal/Newspaper
author D. Handiani
A. Paul
M. Prange
U. Merkel
L. Dupont
X. Zhang
author_facet D. Handiani
A. Paul
M. Prange
U. Merkel
L. Dupont
X. Zhang
author_sort D. Handiani
title Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3
title_short Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3
title_full Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3
title_fullStr Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3
title_full_unstemmed Tropical vegetation response to Heinrich Event 1 as simulated with the UVic ESCM and CCSM3
title_sort tropical vegetation response to heinrich event 1 as simulated with the uvic escm and ccsm3
publisher Copernicus Publications
publishDate 2013
url https://doi.org/10.5194/cp-9-1683-2013
https://doaj.org/article/88d6b23204724fb5b04b2c5d3405a305
genre North Atlantic
genre_facet North Atlantic
op_source Climate of the Past, Vol 9, Iss 4, Pp 1683-1696 (2013)
op_relation http://www.clim-past.net/9/1683/2013/cp-9-1683-2013.pdf
https://doaj.org/toc/1814-9324
https://doaj.org/toc/1814-9332
doi:10.5194/cp-9-1683-2013
1814-9324
1814-9332
https://doaj.org/article/88d6b23204724fb5b04b2c5d3405a305
op_doi https://doi.org/10.5194/cp-9-1683-2013
container_title Climate of the Past
container_volume 9
container_issue 4
container_start_page 1683
op_container_end_page 1696
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