Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s

The western part of East/Japan Sea (WES) is an important area for understanding climate change processes and interactions between atmospheric and oceanic conditions. We analyzed the trends in recent oceanic conditions in the WES after the recent climate regime shift (CRS) that occurred in the late 1...

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Autores principales:	Hae-Kun Jung, S. M. Mustafizur Rahman, Hee-Chan Choi, Joo-Myun Park, Chung-Il Lee
Formato:	article
Lenguaje:	EN
Publicado:	MDPI AG 2021
Materias:	western part of East/Japan Sea climate regime shift Kuroshio extension Aleutian low pressure pressure gradient Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581
Acceso en línea:	https://doaj.org/article/79f6edb2d3744083ba07d73aec1431a5
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spelling	oai:doaj.org-article:79f6edb2d3744083ba07d73aec1431a52021-11-25T18:04:30ZRecent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s10.3390/jmse91112252077-1312https://doaj.org/article/79f6edb2d3744083ba07d73aec1431a52021-11-01T00:00:00Zhttps://www.mdpi.com/2077-1312/9/11/1225https://doaj.org/toc/2077-1312The western part of East/Japan Sea (WES) is an important area for understanding climate change processes and interactions between atmospheric and oceanic conditions. We analyzed the trends in recent oceanic conditions in the WES after the recent climate regime shift (CRS) that occurred in the late 1990s in the North Pacific. We explored the most important climate factors that affect oceanic conditions and determined their responses to changes in climate change. In the CRS that occurred in the late 1980s, changes in oceanic conditions in the WES were influenced by intensity changes in climate factors, and, in the late 1990s, it was by spatial changes in climate factors. The latitudinal shift of the Aleutian low (AL) pressure influences recent changes in oceanic and atmospheric conditions in the WES. The intensity of the Kuroshio Current and the sea level pressure in the Kuroshio extension region associated with the latitudinal shift of the AL pressure affects the volume of transport of the warm and saline water mass that flows into the WES and its atmospheric conditions. In addition, the fluctuations in the oceanic conditions of the WES affect various regions and depth layers differently, and these variations are evident even within the WES.Hae-Kun JungS. M. Mustafizur RahmanHee-Chan ChoiJoo-Myun ParkChung-Il LeeMDPI AGarticlewestern part of East/Japan Seaclimate regime shiftKuroshio extensionAleutian low pressurepressure gradientNaval architecture. Shipbuilding. Marine engineeringVM1-989OceanographyGC1-1581ENJournal of Marine Science and Engineering, Vol 9, Iss 1225, p 1225 (2021)
institution	DOAJ
collection	DOAJ
language	EN
topic	western part of East/Japan Sea climate regime shift Kuroshio extension Aleutian low pressure pressure gradient Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581
spellingShingle	western part of East/Japan Sea climate regime shift Kuroshio extension Aleutian low pressure pressure gradient Naval architecture. Shipbuilding. Marine engineering VM1-989 Oceanography GC1-1581 Hae-Kun Jung S. M. Mustafizur Rahman Hee-Chan Choi Joo-Myun Park Chung-Il Lee Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s
description	The western part of East/Japan Sea (WES) is an important area for understanding climate change processes and interactions between atmospheric and oceanic conditions. We analyzed the trends in recent oceanic conditions in the WES after the recent climate regime shift (CRS) that occurred in the late 1990s in the North Pacific. We explored the most important climate factors that affect oceanic conditions and determined their responses to changes in climate change. In the CRS that occurred in the late 1980s, changes in oceanic conditions in the WES were influenced by intensity changes in climate factors, and, in the late 1990s, it was by spatial changes in climate factors. The latitudinal shift of the Aleutian low (AL) pressure influences recent changes in oceanic and atmospheric conditions in the WES. The intensity of the Kuroshio Current and the sea level pressure in the Kuroshio extension region associated with the latitudinal shift of the AL pressure affects the volume of transport of the warm and saline water mass that flows into the WES and its atmospheric conditions. In addition, the fluctuations in the oceanic conditions of the WES affect various regions and depth layers differently, and these variations are evident even within the WES.
format	article
author	Hae-Kun Jung S. M. Mustafizur Rahman Hee-Chan Choi Joo-Myun Park Chung-Il Lee
author_facet	Hae-Kun Jung S. M. Mustafizur Rahman Hee-Chan Choi Joo-Myun Park Chung-Il Lee
author_sort	Hae-Kun Jung
title	Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s
title_short	Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s
title_full	Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s
title_fullStr	Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s
title_full_unstemmed	Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s
title_sort	recent trends in oceanic conditions in the western part of east/japan sea: an analysis of climate regime shift that occurred after the late 1990s
publisher	MDPI AG
publishDate	2021
url	https://doaj.org/article/79f6edb2d3744083ba07d73aec1431a5
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Recent Trends in Oceanic Conditions in the Western Part of East/Japan Sea: An Analysis of Climate Regime Shift That Occurred after the Late 1990s

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