Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex

The authors investigate the circulation change during the life cycle of a weak stratospheric polar vortex (WSV) event and its impact on temperature variation over East Asia. The lower-tropospheric temperature over East Asia strongly fluctuates despite the slow decay of stratospheric circulation and...

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Published in:Journal of Climate
Main Authors: Woo, SH, Kim, BM, Kug, JS
Format: Article in Journal/Newspaper
Language:English
Published: AMER METEOROLOGICAL SOC 2015
Subjects:
Online Access:https://oasis.postech.ac.kr/handle/2014.oak/35278
https://doi.org/10.1175/JCLI-D-14-00790.1
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spelling ftponangunivst:oai:oasis.postech.ac.kr:2014.oak/35278 2023-05-15T14:59:58+02:00 Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex Woo, SH Kim, BM Kug, JS Kug, JS 2015-10-01 https://oasis.postech.ac.kr/handle/2014.oak/35278 https://doi.org/10.1175/JCLI-D-14-00790.1 English eng AMER METEOROLOGICAL SOC JOURNAL OF CLIMATE Meteorology & Atmospheric Sciences 0894-8755 https://oasis.postech.ac.kr/handle/2014.oak/35278 doi:10.1175/JCLI-D-14-00790.1 17955 JOURNAL OF CLIMATE, v.28, no.14, pp.5857 - 5872 000359637800021 2-s2.0-84942898757 SURFACE AIR-TEMPERATURE NORTHERN ANNULAR MODE WINTER MONSOON ARCTIC OSCILLATION SUDDEN WARMINGS WEATHER REGIMES CLIMATE-CHANGE COLD SURGES PART I HEMISPHERE Article ART 2015 ftponangunivst https://doi.org/10.1175/JCLI-D-14-00790.1 2022-10-20T20:21:19Z The authors investigate the circulation change during the life cycle of a weak stratospheric polar vortex (WSV) event and its impact on temperature variation over East Asia. The lower-tropospheric temperature over East Asia strongly fluctuates despite the slow decay of stratospheric circulation and the continuously negative Arctic Oscillation (AO) pattern during the WSV event. The temperature fluctuation is critically influenced by the variation of the East Asian upper-level coastal trough (EAT), which may be coupled to the stratospheric circulation during the WSV events. The EAT is deepened anomalously during the Peak phase (from lag -5 to lag 5 day) of the WSV, and East Asian temperature is lowest during this phase. During the next period (Decay-1 phase: from lag 6 to lag 16 day), in spite of the slowly decaying WSV condition, the cold temperature anomaly over East Asia is suddenly weakened; this change is caused by a westward-propagating signal of an anticyclonic anomaly from the North Pacific to East Asia. After about two weeks (Decay-2 phase: from lag 17 to lag 27 day), the cold conditions over East Asia are restrengthened by an intensification of EAT, which is related to the eastward propagation of a large-scale wave packet originating from a negative North Atlantic Oscillation (NAO)-type structure in the Decay-1 phase and its delayed influence on the East Asia region. 1 1 9 2 scie scopus Article in Journal/Newspaper Arctic Climate change North Atlantic North Atlantic oscillation Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS) Arctic Pacific Journal of Climate 28 14 5857 5872
institution Open Polar
collection Pohang University of Science and Technology (POSTECH): Open Access System for Information Sharing (OASIS)
op_collection_id ftponangunivst
language English
topic SURFACE AIR-TEMPERATURE
NORTHERN ANNULAR MODE
WINTER MONSOON
ARCTIC OSCILLATION
SUDDEN WARMINGS
WEATHER REGIMES
CLIMATE-CHANGE
COLD SURGES
PART I
HEMISPHERE
spellingShingle SURFACE AIR-TEMPERATURE
NORTHERN ANNULAR MODE
WINTER MONSOON
ARCTIC OSCILLATION
SUDDEN WARMINGS
WEATHER REGIMES
CLIMATE-CHANGE
COLD SURGES
PART I
HEMISPHERE
Woo, SH
Kim, BM
Kug, JS
Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex
topic_facet SURFACE AIR-TEMPERATURE
NORTHERN ANNULAR MODE
WINTER MONSOON
ARCTIC OSCILLATION
SUDDEN WARMINGS
WEATHER REGIMES
CLIMATE-CHANGE
COLD SURGES
PART I
HEMISPHERE
description The authors investigate the circulation change during the life cycle of a weak stratospheric polar vortex (WSV) event and its impact on temperature variation over East Asia. The lower-tropospheric temperature over East Asia strongly fluctuates despite the slow decay of stratospheric circulation and the continuously negative Arctic Oscillation (AO) pattern during the WSV event. The temperature fluctuation is critically influenced by the variation of the East Asian upper-level coastal trough (EAT), which may be coupled to the stratospheric circulation during the WSV events. The EAT is deepened anomalously during the Peak phase (from lag -5 to lag 5 day) of the WSV, and East Asian temperature is lowest during this phase. During the next period (Decay-1 phase: from lag 6 to lag 16 day), in spite of the slowly decaying WSV condition, the cold temperature anomaly over East Asia is suddenly weakened; this change is caused by a westward-propagating signal of an anticyclonic anomaly from the North Pacific to East Asia. After about two weeks (Decay-2 phase: from lag 17 to lag 27 day), the cold conditions over East Asia are restrengthened by an intensification of EAT, which is related to the eastward propagation of a large-scale wave packet originating from a negative North Atlantic Oscillation (NAO)-type structure in the Decay-1 phase and its delayed influence on the East Asia region. 1 1 9 2 scie scopus
author2 Kug, JS
format Article in Journal/Newspaper
author Woo, SH
Kim, BM
Kug, JS
author_facet Woo, SH
Kim, BM
Kug, JS
author_sort Woo, SH
title Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex
title_short Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex
title_full Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex
title_fullStr Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex
title_full_unstemmed Temperature Variation over East Asia during the Lifecycle of Weak Stratospheric Polar Vortex
title_sort temperature variation over east asia during the lifecycle of weak stratospheric polar vortex
publisher AMER METEOROLOGICAL SOC
publishDate 2015
url https://oasis.postech.ac.kr/handle/2014.oak/35278
https://doi.org/10.1175/JCLI-D-14-00790.1
geographic Arctic
Pacific
geographic_facet Arctic
Pacific
genre Arctic
Climate change
North Atlantic
North Atlantic oscillation
genre_facet Arctic
Climate change
North Atlantic
North Atlantic oscillation
op_relation JOURNAL OF CLIMATE
Meteorology & Atmospheric Sciences
0894-8755
https://oasis.postech.ac.kr/handle/2014.oak/35278
doi:10.1175/JCLI-D-14-00790.1
17955
JOURNAL OF CLIMATE, v.28, no.14, pp.5857 - 5872
000359637800021
2-s2.0-84942898757
op_doi https://doi.org/10.1175/JCLI-D-14-00790.1
container_title Journal of Climate
container_volume 28
container_issue 14
container_start_page 5857
op_container_end_page 5872
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