Changes in the role of Pacific decadal oscillation on East Asian winter surface temperature

The complex interaction between the Pacific decadal oscillation (PDO) and East Asian winter temperatures remains unclear. This study reveals that since the early 2000s, East Asia has experienced a strengthening of Aleutian low (AL) and Siberian high (SH) during negative PDO phases, leading to an int...

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Main Authors: Doo Young Lee, Sang-Wook Yeh, Hyein Jeong, Hyo-Seok Park
Format: Article
Language:English
Published: IOP Publishing 2025-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/adaf45
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author Doo Young Lee
Sang-Wook Yeh
Hyein Jeong
Hyo-Seok Park
author_facet Doo Young Lee
Sang-Wook Yeh
Hyein Jeong
Hyo-Seok Park
author_sort Doo Young Lee
collection DOAJ
description The complex interaction between the Pacific decadal oscillation (PDO) and East Asian winter temperatures remains unclear. This study reveals that since the early 2000s, East Asia has experienced a strengthening of Aleutian low (AL) and Siberian high (SH) during negative PDO phases, leading to an intensified East Asian winter monsoon (EAWM). The increased pressure gradient between the SH and the AL, driven by warming in the western Pacific associated with the negative PDO phase, has significantly contributed to a shift toward cooling in East Asia (105°–150° E, 20°–50° N) since the early 2000s. Observations and model simulations provide evidence that the enhanced tropical convection in the western Pacific under a negative PDO phase has intensified the atmospheric circulations associated with the EAWM since the early 2000s. Understanding these dynamics is crucial for improving winter temperature forecasts in East Asia.
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series Environmental Research Letters
spelling doaj-art-4ecaf721f4814db0a6a9aaecf71948e62025-02-07T10:33:57ZengIOP PublishingEnvironmental Research Letters1748-93262025-01-0120202406210.1088/1748-9326/adaf45Changes in the role of Pacific decadal oscillation on East Asian winter surface temperatureDoo Young Lee0https://orcid.org/0000-0002-6129-2241Sang-Wook Yeh1https://orcid.org/0000-0003-4549-1686Hyein Jeong2Hyo-Seok Park3Institute of Ocean and Atmospheric Science (IOAS), Hanyang University , Ansan, Republic of KoreaInstitute of Ocean and Atmospheric Science (IOAS), Hanyang University , Ansan, Republic of Korea; Department of Marine Science and Convergence Engineering, Hanyang University , Ansan, Republic of KoreaInstitute of Ocean and Atmospheric Science (IOAS), Hanyang University , Ansan, Republic of KoreaInstitute of Ocean and Atmospheric Science (IOAS), Hanyang University , Ansan, Republic of Korea; Department of Marine Science and Convergence Engineering, Hanyang University , Ansan, Republic of KoreaThe complex interaction between the Pacific decadal oscillation (PDO) and East Asian winter temperatures remains unclear. This study reveals that since the early 2000s, East Asia has experienced a strengthening of Aleutian low (AL) and Siberian high (SH) during negative PDO phases, leading to an intensified East Asian winter monsoon (EAWM). The increased pressure gradient between the SH and the AL, driven by warming in the western Pacific associated with the negative PDO phase, has significantly contributed to a shift toward cooling in East Asia (105°–150° E, 20°–50° N) since the early 2000s. Observations and model simulations provide evidence that the enhanced tropical convection in the western Pacific under a negative PDO phase has intensified the atmospheric circulations associated with the EAWM since the early 2000s. Understanding these dynamics is crucial for improving winter temperature forecasts in East Asia.https://doi.org/10.1088/1748-9326/adaf45Pacific decadal oscillationEast Asian winter temperaturesAleutian lowSiberian high
spellingShingle Doo Young Lee
Sang-Wook Yeh
Hyein Jeong
Hyo-Seok Park
Changes in the role of Pacific decadal oscillation on East Asian winter surface temperature
Environmental Research Letters
Pacific decadal oscillation
East Asian winter temperatures
Aleutian low
Siberian high
title Changes in the role of Pacific decadal oscillation on East Asian winter surface temperature
title_full Changes in the role of Pacific decadal oscillation on East Asian winter surface temperature
title_fullStr Changes in the role of Pacific decadal oscillation on East Asian winter surface temperature
title_full_unstemmed Changes in the role of Pacific decadal oscillation on East Asian winter surface temperature
title_short Changes in the role of Pacific decadal oscillation on East Asian winter surface temperature
title_sort changes in the role of pacific decadal oscillation on east asian winter surface temperature
topic Pacific decadal oscillation
East Asian winter temperatures
Aleutian low
Siberian high
url https://doi.org/10.1088/1748-9326/adaf45
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AT hyeinjeong changesintheroleofpacificdecadaloscillationoneastasianwintersurfacetemperature
AT hyoseokpark changesintheroleofpacificdecadaloscillationoneastasianwintersurfacetemperature