Greening in the circumpolar high-latitude may amplify warming in the growing season

We present a study that suggests greening in the circumpolar high-latitude regions amplifies surface warming in the growing season (May-September) under enhanced greenhouse conditions. The investigation used a series of climate simulations with the Community Atmospheric Model version 3-which incorpo...

Full description

Bibliographic Details
Published in:Climate Dynamics
Main Authors: Jeong, JH, Kug, JS, Kim, BM, Min, SK, Linderholm, HW, Ho, CH, Rayner, D, Chen, DL, Jun, SY
Other Authors: 환경공학부, 11198091
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2012
Subjects:
Online Access:https://oasis.postech.ac.kr/handle/2014.oak/15560
https://doi.org/10.1007/S00382-011-1142-X
_version_ 1821797416132673536
author Jeong, JH
Kug, JS
Kim, BM
Min, SK
Linderholm, HW
Ho, CH
Rayner, D
Chen, DL
Jun, SY
author2 환경공학부
11198091
Min, SK
author_facet Jeong, JH
Kug, JS
Kim, BM
Min, SK
Linderholm, HW
Ho, CH
Rayner, D
Chen, DL
Jun, SY
author_sort Jeong, JH
collection Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS)
container_issue 7-8
container_start_page 1421
container_title Climate Dynamics
container_volume 38
description We present a study that suggests greening in the circumpolar high-latitude regions amplifies surface warming in the growing season (May-September) under enhanced greenhouse conditions. The investigation used a series of climate simulations with the Community Atmospheric Model version 3-which incorporates a coupled, dynamic global vegetation model-with and without vegetation feedback, under both present and doubled CO2 concentrations. Results indicate that climate warming and associated changes promote circumpolar greening with northward expansion and enhanced greenness of both the Arctic tundra and boreal forest regions. This leads to additional surface warming in the high-latitudes in the growing season, primarily through more absorption of incoming solar radiation. The resulting surface and tropospheric warming in the high-latitude and Arctic regions weakens prevailing tropospheric westerlies over 45-70N, leading to the formation of anticyclonic pressure anomalies in the Arctic regions. These pressure anomalies resemble the anomalous circulation pattern during the negative phase of winter Arctic Oscillation. It is suggested that these circulation anomalies reinforce the high-latitude and Arctic warming in the growing season. X 1 1 13 13 scie scopus
format Article in Journal/Newspaper
genre Arctic Greening
Arctic
Climate change
Ice
permafrost
Tundra
genre_facet Arctic Greening
Arctic
Climate change
Ice
permafrost
Tundra
geographic Arctic
geographic_facet Arctic
id ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/15560
institution Open Polar
language English
op_collection_id ftponangunivst
op_container_end_page 1431
op_doi https://doi.org/10.1007/S00382-011-1142-X
op_relation CLIMATE DYNAMICS
38
7-8
1421
1431
SCI급, SCOPUS 등재논문
SCI
Meteorology & Atmospheric Sciences
0930-7575
2012-OAK-0000027493
https://oasis.postech.ac.kr/handle/2014.oak/15560
doi:10.1007/S00382-011-1142-X
13524
CLIMATE DYNAMICS, v.38, no.7-8, pp.1421 - 1431
000302247000011
2-s2.0-84859002194
publishDate 2012
publisher Springer
record_format openpolar
spelling ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/15560 2025-01-16T20:01:05+00:00 Greening in the circumpolar high-latitude may amplify warming in the growing season Jeong, JH Kug, JS Kim, BM Min, SK Linderholm, HW Ho, CH Rayner, D Chen, DL Jun, SY 환경공학부 11198091 Min, SK 2012-04 https://oasis.postech.ac.kr/handle/2014.oak/15560 https://doi.org/10.1007/S00382-011-1142-X English eng Springer CLIMATE DYNAMICS 38 7-8 1421 1431 SCI급, SCOPUS 등재논문 SCI Meteorology & Atmospheric Sciences 0930-7575 2012-OAK-0000027493 https://oasis.postech.ac.kr/handle/2014.oak/15560 doi:10.1007/S00382-011-1142-X 13524 CLIMATE DYNAMICS, v.38, no.7-8, pp.1421 - 1431 000302247000011 2-s2.0-84859002194 Vegetation Arctic warming Arctic greening Climate model Future climate Atmospheric circulation Surface energy budget GLOBAL VEGETATION MODEL CLIMATE-CHANGE ATMOSPHERIC RESPONSE ARCTIC TEMPERATURE BOREAL FOREST ICE FEEDBACKS CARBON SENSITIVITY PERMAFROST GLOBAL VEGETATION MODEL INDEX Article ART 2012 ftponangunivst https://doi.org/10.1007/S00382-011-1142-X 2022-10-20T20:09:58Z We present a study that suggests greening in the circumpolar high-latitude regions amplifies surface warming in the growing season (May-September) under enhanced greenhouse conditions. The investigation used a series of climate simulations with the Community Atmospheric Model version 3-which incorporates a coupled, dynamic global vegetation model-with and without vegetation feedback, under both present and doubled CO2 concentrations. Results indicate that climate warming and associated changes promote circumpolar greening with northward expansion and enhanced greenness of both the Arctic tundra and boreal forest regions. This leads to additional surface warming in the high-latitudes in the growing season, primarily through more absorption of incoming solar radiation. The resulting surface and tropospheric warming in the high-latitude and Arctic regions weakens prevailing tropospheric westerlies over 45-70N, leading to the formation of anticyclonic pressure anomalies in the Arctic regions. These pressure anomalies resemble the anomalous circulation pattern during the negative phase of winter Arctic Oscillation. It is suggested that these circulation anomalies reinforce the high-latitude and Arctic warming in the growing season. X 1 1 13 13 scie scopus Article in Journal/Newspaper Arctic Greening Arctic Climate change Ice permafrost Tundra Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Arctic Climate Dynamics 38 7-8 1421 1431
spellingShingle Vegetation
Arctic warming
Arctic greening
Climate model
Future climate
Atmospheric circulation
Surface energy budget
GLOBAL VEGETATION MODEL
CLIMATE-CHANGE
ATMOSPHERIC RESPONSE
ARCTIC TEMPERATURE
BOREAL FOREST
ICE
FEEDBACKS
CARBON
SENSITIVITY
PERMAFROST
GLOBAL VEGETATION
MODEL
INDEX
Jeong, JH
Kug, JS
Kim, BM
Min, SK
Linderholm, HW
Ho, CH
Rayner, D
Chen, DL
Jun, SY
Greening in the circumpolar high-latitude may amplify warming in the growing season
title Greening in the circumpolar high-latitude may amplify warming in the growing season
title_full Greening in the circumpolar high-latitude may amplify warming in the growing season
title_fullStr Greening in the circumpolar high-latitude may amplify warming in the growing season
title_full_unstemmed Greening in the circumpolar high-latitude may amplify warming in the growing season
title_short Greening in the circumpolar high-latitude may amplify warming in the growing season
title_sort greening in the circumpolar high-latitude may amplify warming in the growing season
topic Vegetation
Arctic warming
Arctic greening
Climate model
Future climate
Atmospheric circulation
Surface energy budget
GLOBAL VEGETATION MODEL
CLIMATE-CHANGE
ATMOSPHERIC RESPONSE
ARCTIC TEMPERATURE
BOREAL FOREST
ICE
FEEDBACKS
CARBON
SENSITIVITY
PERMAFROST
GLOBAL VEGETATION
MODEL
INDEX
topic_facet Vegetation
Arctic warming
Arctic greening
Climate model
Future climate
Atmospheric circulation
Surface energy budget
GLOBAL VEGETATION MODEL
CLIMATE-CHANGE
ATMOSPHERIC RESPONSE
ARCTIC TEMPERATURE
BOREAL FOREST
ICE
FEEDBACKS
CARBON
SENSITIVITY
PERMAFROST
GLOBAL VEGETATION
MODEL
INDEX
url https://oasis.postech.ac.kr/handle/2014.oak/15560
https://doi.org/10.1007/S00382-011-1142-X