ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait

Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring...
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Autor*in:	Zhang, Yimin [verfasserIn] Zhao, Zhonghua Liao, Enhui Jiang, Yuwu

Format:	Artikel
Sprache:	Englisch

Erschienen:	2022

Schlagwörter:	Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait

Anmerkung:	© The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022

Übergeordnetes Werk:	Enthalten in: Climate dynamics - Springer Berlin Heidelberg, 1986, 59(2022), 11-12 vom: 04. Juni, Seite 3359-3372
Übergeordnetes Werk:	volume:59 ; year:2022 ; number:11-12 ; day:04 ; month:06 ; pages:3359-3372

Links:	Volltext

DOI / URN:	10.1007/s00382-022-06270-9

Katalog-ID:	OLC2079853554

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520			\|a Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases.
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allfields	10.1007/s00382-022-06270-9 doi (DE-627)OLC2079853554 (DE-He213)s00382-022-06270-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Zhang, Yimin verfasserin aut ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait Zhao, Zhonghua aut Liao, Enhui aut Jiang, Yuwu aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 59(2022), 11-12 vom: 04. Juni, Seite 3359-3372 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:59 year:2022 number:11-12 day:04 month:06 pages:3359-3372 https://doi.org/10.1007/s00382-022-06270-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 59 2022 11-12 04 06 3359-3372
spelling	10.1007/s00382-022-06270-9 doi (DE-627)OLC2079853554 (DE-He213)s00382-022-06270-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Zhang, Yimin verfasserin aut ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait Zhao, Zhonghua aut Liao, Enhui aut Jiang, Yuwu aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 59(2022), 11-12 vom: 04. Juni, Seite 3359-3372 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:59 year:2022 number:11-12 day:04 month:06 pages:3359-3372 https://doi.org/10.1007/s00382-022-06270-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 59 2022 11-12 04 06 3359-3372
allfields_unstemmed	10.1007/s00382-022-06270-9 doi (DE-627)OLC2079853554 (DE-He213)s00382-022-06270-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Zhang, Yimin verfasserin aut ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait Zhao, Zhonghua aut Liao, Enhui aut Jiang, Yuwu aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 59(2022), 11-12 vom: 04. Juni, Seite 3359-3372 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:59 year:2022 number:11-12 day:04 month:06 pages:3359-3372 https://doi.org/10.1007/s00382-022-06270-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 59 2022 11-12 04 06 3359-3372
allfieldsGer	10.1007/s00382-022-06270-9 doi (DE-627)OLC2079853554 (DE-He213)s00382-022-06270-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Zhang, Yimin verfasserin aut ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait Zhao, Zhonghua aut Liao, Enhui aut Jiang, Yuwu aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 59(2022), 11-12 vom: 04. Juni, Seite 3359-3372 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:59 year:2022 number:11-12 day:04 month:06 pages:3359-3372 https://doi.org/10.1007/s00382-022-06270-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 59 2022 11-12 04 06 3359-3372
allfieldsSound	10.1007/s00382-022-06270-9 doi (DE-627)OLC2079853554 (DE-He213)s00382-022-06270-9-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Zhang, Yimin verfasserin aut ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022 Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait Zhao, Zhonghua aut Liao, Enhui aut Jiang, Yuwu aut Enthalten in Climate dynamics Springer Berlin Heidelberg, 1986 59(2022), 11-12 vom: 04. Juni, Seite 3359-3372 (DE-627)129932728 (DE-600)382992-3 (DE-576)015479005 0930-7575 nnns volume:59 year:2022 number:11-12 day:04 month:06 pages:3359-3372 https://doi.org/10.1007/s00382-022-06270-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_62 GBV_ILN_154 GBV_ILN_2018 GBV_ILN_4277 AR 59 2022 11-12 04 06 3359-3372
language	English
source	Enthalten in Climate dynamics 59(2022), 11-12 vom: 04. Juni, Seite 3359-3372 volume:59 year:2022 number:11-12 day:04 month:06 pages:3359-3372
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topic_facet	Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait
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author	Zhang, Yimin
spellingShingle	Zhang, Yimin ddc 550 ssgn 16,13 misc Sea surface temperature misc Pacific Decadal Oscillation misc El Niño–Southern Oscillation misc North Pacific Oscillation misc North Pacific Gyre Oscillation misc Taiwan Strait ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait
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topic_title	550 VZ 16,13 ssgn ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait Sea surface temperature Pacific Decadal Oscillation El Niño–Southern Oscillation North Pacific Oscillation North Pacific Gyre Oscillation Taiwan Strait
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title	ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait
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title_full	ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait
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author_browse	Zhang, Yimin Zhao, Zhonghua Liao, Enhui Jiang, Yuwu
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title_sort	enso and pdo-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait
title_auth	ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait
abstract	Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022
abstractGer	Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022
abstract_unstemmed	Abstract The Taiwan Strait has the largest temporal variability in the wintertime sea surface temperature (SST) along the China coast. The warming and cooling trends reach about ± 1 °C per decade in winter during 1982–1999 and 1999–2014, respectively, which are about 4 times larger than neighboring coastal area and open ocean. Previous studies have noted these opposite trends, but the cause remains unclear due to insufficient study on teleconnections of this local signals to large-scale climate signals (e.g., Pacific Decadal Oscillation, PDO; El Niño–Southern Oscillation, ENSO). Using different period filters, wintertime SST anomaly in the Taiwan Strait (TS-SSTa) of different timescales were separated and connected to the large-scale climate signals. Besides the impact of global warming, we also found that the interdecadal signal of PDO contribute significantly to the warming and cooling trends of the wintertime TS-SSTa during 1982–2014 (mostly the positive PDO phase). During the positive PDO phase, a sea level pressure (SLP) dipole develops at the North Pacific, leading to a northeasterly wind jet along the Eurasian eastern coast, and affecting the interdecadal wintertime TS-SSTa through the East Asia Winter Monsoon (EAWM) and North Pacific Subtropical Gyre. During the negative PDO phase, the influence from North Pacific weakens, and the tropical Pacific has a greater influence on the interannual wintertime TS-SSTa through the northward movement of the ENSO-related cyclone/anticyclone anomaly over East Asia. Thus, the influence from North Pacific (PDO) and tropical Pacific (ENSO) alternately control the TS-SSTa variation during the positive and negative PDO phases. © The Author(s), under exclusive licence to Springer-Verlag GmbH Germany, part of Springer Nature 2022
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title_short	ENSO and PDO-related interannual and interdecadal variations in the wintertime sea surface temperature in a typical subtropical strait
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