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...
Published in: | Climate Dynamics |
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Main Authors: | , , , , , , , , |
Other Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Springer
2012
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Subjects: | |
Online Access: | https://oasis.postech.ac.kr/handle/2014.oak/15560 https://doi.org/10.1007/S00382-011-1142-X |
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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 |