Overview of the multi-layer circulation in the South China Sea

The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Zhu, Yaohua [verfasserIn] Sun, Junchuan [verfasserIn] Wang, Yonggang [verfasserIn] Li, Shujiang [verfasserIn] Xu, Tengfei [verfasserIn] Wei, Zexun [verfasserIn] Qu, Tangdong [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Übergeordnetes Werk:	Enthalten in: Progress in oceanography - Amsterdam [u.a.] : Elsevier Science, 1963, 175, Seite 171-182
Übergeordnetes Werk:	volume:175 ; pages:171-182

DOI / URN:	10.1016/j.pocean.2019.04.001

Katalog-ID:	ELV002414171

Internformat


LEADER	01000caa a22002652 4500
001	ELV002414171
003	DE-627
005	20230524143313.0
007	cr uuu---uuuuu
008	230429s2019 xx \|\|\|\|\|o 00\| \|\|eng c
024	7		\|a 10.1016/j.pocean.2019.04.001 \|2 doi
035			\|a (DE-627)ELV002414171
035			\|a (ELSEVIER)S0079-6611(18)30108-3
040			\|a DE-627 \|b ger \|c DE-627 \|e rda
041			\|a eng
082	0	4	\|a 550 \|q DE-600
084			\|a 38.90 \|2 bkl
100	1		\|a Zhu, Yaohua \|e verfasserin \|4 aut
245	1	0	\|a Overview of the multi-layer circulation in the South China Sea
264		1	\|c 2019
336			\|a nicht spezifiziert \|b zzz \|2 rdacontent
337			\|a Computermedien \|b c \|2 rdamedia
338			\|a Online-Ressource \|b cr \|2 rdacarrier
520			\|a The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation.
700	1		\|a Sun, Junchuan \|e verfasserin \|4 aut
700	1		\|a Wang, Yonggang \|e verfasserin \|4 aut
700	1		\|a Li, Shujiang \|e verfasserin \|4 aut
700	1		\|a Xu, Tengfei \|e verfasserin \|4 aut
700	1		\|a Wei, Zexun \|e verfasserin \|4 aut
700	1		\|a Qu, Tangdong \|e verfasserin \|4 aut
773	0	8	\|i Enthalten in \|t Progress in oceanography \|d Amsterdam [u.a.] : Elsevier Science, 1963 \|g 175, Seite 171-182 \|h Online-Ressource \|w (DE-627)306364816 \|w (DE-600)1497436-8 \|w (DE-576)259484113 \|x 0079-6611 \|7 nnns
773	1	8	\|g volume:175 \|g pages:171-182
912			\|a GBV_USEFLAG_U
912			\|a SYSFLAG_U
912			\|a GBV_ELV
912			\|a SSG-OPC-GGO
912			\|a GBV_ILN_20
912			\|a GBV_ILN_22
912			\|a GBV_ILN_23
912			\|a GBV_ILN_24
912			\|a GBV_ILN_31
912			\|a GBV_ILN_32
912			\|a GBV_ILN_40
912			\|a GBV_ILN_60
912			\|a GBV_ILN_62
912			\|a GBV_ILN_63
912			\|a GBV_ILN_65
912			\|a GBV_ILN_69
912			\|a GBV_ILN_70
912			\|a GBV_ILN_73
912			\|a GBV_ILN_74
912			\|a GBV_ILN_90
912			\|a GBV_ILN_95
912			\|a GBV_ILN_100
912			\|a GBV_ILN_105
912			\|a GBV_ILN_110
912			\|a GBV_ILN_150
912			\|a GBV_ILN_151
912			\|a GBV_ILN_224
912			\|a GBV_ILN_370
912			\|a GBV_ILN_602
912			\|a GBV_ILN_702
912			\|a GBV_ILN_2003
912			\|a GBV_ILN_2004
912			\|a GBV_ILN_2005
912			\|a GBV_ILN_2011
912			\|a GBV_ILN_2014
912			\|a GBV_ILN_2015
912			\|a GBV_ILN_2020
912			\|a GBV_ILN_2021
912			\|a GBV_ILN_2025
912			\|a GBV_ILN_2027
912			\|a GBV_ILN_2034
912			\|a GBV_ILN_2038
912			\|a GBV_ILN_2044
912			\|a GBV_ILN_2048
912			\|a GBV_ILN_2049
912			\|a GBV_ILN_2050
912			\|a GBV_ILN_2056
912			\|a GBV_ILN_2059
912			\|a GBV_ILN_2061
912			\|a GBV_ILN_2064
912			\|a GBV_ILN_2065
912			\|a GBV_ILN_2068
912			\|a GBV_ILN_2111
912			\|a GBV_ILN_2112
912			\|a GBV_ILN_2113
912			\|a GBV_ILN_2118
912			\|a GBV_ILN_2122
912			\|a GBV_ILN_2129
912			\|a GBV_ILN_2143
912			\|a GBV_ILN_2147
912			\|a GBV_ILN_2148
912			\|a GBV_ILN_2152
912			\|a GBV_ILN_2153
912			\|a GBV_ILN_2190
912			\|a GBV_ILN_2336
912			\|a GBV_ILN_2507
912			\|a GBV_ILN_2522
912			\|a GBV_ILN_4035
912			\|a GBV_ILN_4037
912			\|a GBV_ILN_4112
912			\|a GBV_ILN_4125
912			\|a GBV_ILN_4126
912			\|a GBV_ILN_4242
912			\|a GBV_ILN_4251
912			\|a GBV_ILN_4305
912			\|a GBV_ILN_4313
912			\|a GBV_ILN_4323
912			\|a GBV_ILN_4324
912			\|a GBV_ILN_4326
912			\|a GBV_ILN_4333
912			\|a GBV_ILN_4334
912			\|a GBV_ILN_4335
912			\|a GBV_ILN_4338
912			\|a GBV_ILN_4393
936	b	k	\|a 38.90 \|j Ozeanologie \|j Ozeanographie
951			\|a AR
952			\|d 175 \|h 171-182

Indexfelder

author_variant	y z yz j s js y w yw s l sl t x tx z w zw t q tq
matchkey_str	article:00796611:2019----::vriwfhmliaecruainnh
hierarchy_sort_str	2019
bklnumber	38.90
publishDate	2019
allfields	10.1016/j.pocean.2019.04.001 doi (DE-627)ELV002414171 (ELSEVIER)S0079-6611(18)30108-3 DE-627 ger DE-627 rda eng 550 DE-600 38.90 bkl Zhu, Yaohua verfasserin aut Overview of the multi-layer circulation in the South China Sea 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation. Sun, Junchuan verfasserin aut Wang, Yonggang verfasserin aut Li, Shujiang verfasserin aut Xu, Tengfei verfasserin aut Wei, Zexun verfasserin aut Qu, Tangdong verfasserin aut Enthalten in Progress in oceanography Amsterdam [u.a.] : Elsevier Science, 1963 175, Seite 171-182 Online-Ressource (DE-627)306364816 (DE-600)1497436-8 (DE-576)259484113 0079-6611 nnns volume:175 pages:171-182 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie AR 175 171-182
spelling	10.1016/j.pocean.2019.04.001 doi (DE-627)ELV002414171 (ELSEVIER)S0079-6611(18)30108-3 DE-627 ger DE-627 rda eng 550 DE-600 38.90 bkl Zhu, Yaohua verfasserin aut Overview of the multi-layer circulation in the South China Sea 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation. Sun, Junchuan verfasserin aut Wang, Yonggang verfasserin aut Li, Shujiang verfasserin aut Xu, Tengfei verfasserin aut Wei, Zexun verfasserin aut Qu, Tangdong verfasserin aut Enthalten in Progress in oceanography Amsterdam [u.a.] : Elsevier Science, 1963 175, Seite 171-182 Online-Ressource (DE-627)306364816 (DE-600)1497436-8 (DE-576)259484113 0079-6611 nnns volume:175 pages:171-182 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie AR 175 171-182
allfields_unstemmed	10.1016/j.pocean.2019.04.001 doi (DE-627)ELV002414171 (ELSEVIER)S0079-6611(18)30108-3 DE-627 ger DE-627 rda eng 550 DE-600 38.90 bkl Zhu, Yaohua verfasserin aut Overview of the multi-layer circulation in the South China Sea 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation. Sun, Junchuan verfasserin aut Wang, Yonggang verfasserin aut Li, Shujiang verfasserin aut Xu, Tengfei verfasserin aut Wei, Zexun verfasserin aut Qu, Tangdong verfasserin aut Enthalten in Progress in oceanography Amsterdam [u.a.] : Elsevier Science, 1963 175, Seite 171-182 Online-Ressource (DE-627)306364816 (DE-600)1497436-8 (DE-576)259484113 0079-6611 nnns volume:175 pages:171-182 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie AR 175 171-182
allfieldsGer	10.1016/j.pocean.2019.04.001 doi (DE-627)ELV002414171 (ELSEVIER)S0079-6611(18)30108-3 DE-627 ger DE-627 rda eng 550 DE-600 38.90 bkl Zhu, Yaohua verfasserin aut Overview of the multi-layer circulation in the South China Sea 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation. Sun, Junchuan verfasserin aut Wang, Yonggang verfasserin aut Li, Shujiang verfasserin aut Xu, Tengfei verfasserin aut Wei, Zexun verfasserin aut Qu, Tangdong verfasserin aut Enthalten in Progress in oceanography Amsterdam [u.a.] : Elsevier Science, 1963 175, Seite 171-182 Online-Ressource (DE-627)306364816 (DE-600)1497436-8 (DE-576)259484113 0079-6611 nnns volume:175 pages:171-182 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie AR 175 171-182
allfieldsSound	10.1016/j.pocean.2019.04.001 doi (DE-627)ELV002414171 (ELSEVIER)S0079-6611(18)30108-3 DE-627 ger DE-627 rda eng 550 DE-600 38.90 bkl Zhu, Yaohua verfasserin aut Overview of the multi-layer circulation in the South China Sea 2019 nicht spezifiziert zzz rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation. Sun, Junchuan verfasserin aut Wang, Yonggang verfasserin aut Li, Shujiang verfasserin aut Xu, Tengfei verfasserin aut Wei, Zexun verfasserin aut Qu, Tangdong verfasserin aut Enthalten in Progress in oceanography Amsterdam [u.a.] : Elsevier Science, 1963 175, Seite 171-182 Online-Ressource (DE-627)306364816 (DE-600)1497436-8 (DE-576)259484113 0079-6611 nnns volume:175 pages:171-182 GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393 38.90 Ozeanologie Ozeanographie AR 175 171-182
language	English
source	Enthalten in Progress in oceanography 175, Seite 171-182 volume:175 pages:171-182
sourceStr	Enthalten in Progress in oceanography 175, Seite 171-182 volume:175 pages:171-182
format_phy_str_mv	Article
bklname	Ozeanologie Ozeanographie
institution	findex.gbv.de
dewey-raw	550
isfreeaccess_bool	false
container_title	Progress in oceanography
authorswithroles_txt_mv	Zhu, Yaohua @@aut@@ Sun, Junchuan @@aut@@ Wang, Yonggang @@aut@@ Li, Shujiang @@aut@@ Xu, Tengfei @@aut@@ Wei, Zexun @@aut@@ Qu, Tangdong @@aut@@
publishDateDaySort_date	2019-01-01T00:00:00Z
hierarchy_top_id	306364816
dewey-sort	3550
id	ELV002414171
language_de	englisch
fullrecord	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV002414171</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230524143313.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230429s2019 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.pocean.2019.04.001</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV002414171</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0079-6611(18)30108-3</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.90</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhu, Yaohua</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Overview of the multi-layer circulation in the South China Sea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sun, Junchuan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Yonggang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Shujiang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Tengfei</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wei, Zexun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Qu, Tangdong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Progress in oceanography</subfield><subfield code="d">Amsterdam [u.a.] : Elsevier Science, 1963</subfield><subfield code="g">175, Seite 171-182</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)306364816</subfield><subfield code="w">(DE-600)1497436-8</subfield><subfield code="w">(DE-576)259484113</subfield><subfield code="x">0079-6611</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:175</subfield><subfield code="g">pages:171-182</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.90</subfield><subfield code="j">Ozeanologie</subfield><subfield code="j">Ozeanographie</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">175</subfield><subfield code="h">171-182</subfield></datafield></record></collection>
author	Zhu, Yaohua
spellingShingle	Zhu, Yaohua ddc 550 bkl 38.90 Overview of the multi-layer circulation in the South China Sea
authorStr	Zhu, Yaohua
ppnlink_with_tag_str_mv	@@773@@(DE-627)306364816
format	electronic Article
dewey-ones	550 - Earth sciences
delete_txt_mv	keep
author_role	aut aut aut aut aut aut aut
collection	elsevier
remote_str	true
illustrated	Not Illustrated
issn	0079-6611
topic_title	550 DE-600 38.90 bkl Overview of the multi-layer circulation in the South China Sea
topic	ddc 550 bkl 38.90
topic_unstemmed	ddc 550 bkl 38.90
topic_browse	ddc 550 bkl 38.90
format_facet	Elektronische Aufsätze Aufsätze Elektronische Ressource
format_main_str_mv	Text Zeitschrift/Artikel
carriertype_str_mv	cr
hierarchy_parent_title	Progress in oceanography
hierarchy_parent_id	306364816
dewey-tens	550 - Earth sciences & geology
hierarchy_top_title	Progress in oceanography
isfreeaccess_txt	false
familylinks_str_mv	(DE-627)306364816 (DE-600)1497436-8 (DE-576)259484113
title	Overview of the multi-layer circulation in the South China Sea
ctrlnum	(DE-627)ELV002414171 (ELSEVIER)S0079-6611(18)30108-3
title_full	Overview of the multi-layer circulation in the South China Sea
author_sort	Zhu, Yaohua
journal	Progress in oceanography
journalStr	Progress in oceanography
lang_code	eng
isOA_bool	false
dewey-hundreds	500 - Science
recordtype	marc
publishDateSort	2019
contenttype_str_mv	zzz
container_start_page	171
author_browse	Zhu, Yaohua Sun, Junchuan Wang, Yonggang Li, Shujiang Xu, Tengfei Wei, Zexun Qu, Tangdong
container_volume	175
class	550 DE-600 38.90 bkl
format_se	Elektronische Aufsätze
author-letter	Zhu, Yaohua
doi_str_mv	10.1016/j.pocean.2019.04.001
dewey-full	550
author2-role	verfasserin
title_sort	overview of the multi-layer circulation in the south china sea
title_auth	Overview of the multi-layer circulation in the South China Sea
abstract	The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation.
abstractGer	The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation.
abstract_unstemmed	The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation.
collection_details	GBV_USEFLAG_U SYSFLAG_U GBV_ELV SSG-OPC-GGO GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_150 GBV_ILN_151 GBV_ILN_224 GBV_ILN_370 GBV_ILN_602 GBV_ILN_702 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2027 GBV_ILN_2034 GBV_ILN_2038 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2056 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2190 GBV_ILN_2336 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4313 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4393
title_short	Overview of the multi-layer circulation in the South China Sea
remote_bool	true
author2	Sun, Junchuan Wang, Yonggang Li, Shujiang Xu, Tengfei Wei, Zexun Qu, Tangdong
author2Str	Sun, Junchuan Wang, Yonggang Li, Shujiang Xu, Tengfei Wei, Zexun Qu, Tangdong
ppnlink	306364816
mediatype_str_mv	c
isOA_txt	false
hochschulschrift_bool	false
doi_str	10.1016/j.pocean.2019.04.001
up_date	2024-07-07T00:38:54.586Z
_version_	1803878645984395264
fullrecord_marcxml	<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">ELV002414171</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230524143313.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">230429s2019 xx \|\|\|\|\|o 00\| \|\|eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1016/j.pocean.2019.04.001</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)ELV002414171</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(ELSEVIER)S0079-6611(18)30108-3</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rda</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">DE-600</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">38.90</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Zhu, Yaohua</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Overview of the multi-layer circulation in the South China Sea</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2019</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">nicht spezifiziert</subfield><subfield code="b">zzz</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">The South China Sea (SCS) is a semi-enclosed ocean basin, with its sole deepwater renewal channel in the northeast, the Luzon Strait, connected to the northwestern Pacific. The circulation in the SCS is endowed with a distinctive multi-layer structure, which is influenced by the seasonally reversing Southeast Asian monsoon at the surface, modulated Kuroshio intrusion in the upper layer, and enhanced diapycnal mixing and persistent Luzon Strait deepwater overflow in the deep layer. After being diapycnally mixed by energetic internal tides, internal waves, and mesoscale eddies, waters entering the SCS in the upper and deep layers through the Luzon Strait are returned to the northwestern Pacific in the intermediate layer. This inflow-outflow-inflow structure in vertical induces net inflows of potential vorticity in the upper and deep layers and a net outflow of potential vorticity in the intermediate layer of the Luzon Strait, which are believed to be closely related with the circulation structure in the SCS. A sandwiched circulation in the SCS, namely, anticyclonic in the intermediate layer and cyclonic in the upper and deeper layers, was recently reported, but controversial issues still remain on its spatial pattern and temporal variability. To ascertain this sandwiched circulation and reveal its driving mechanism is of much scientific interest to the on-going discussion on the SCS circulation and its role in regional climate. Different from previous review articles focusing on eddies or circulation in a specific layer or area, we overview the full-depth circulation of the SCS layer-by-layer and outline its possible forcing mechanisms, and furthermore, provide perspectives for further investigation.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Sun, Junchuan</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Yonggang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Li, Shujiang</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Xu, Tengfei</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wei, Zexun</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Qu, Tangdong</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Progress in oceanography</subfield><subfield code="d">Amsterdam [u.a.] : Elsevier Science, 1963</subfield><subfield code="g">175, Seite 171-182</subfield><subfield code="h">Online-Ressource</subfield><subfield code="w">(DE-627)306364816</subfield><subfield code="w">(DE-600)1497436-8</subfield><subfield code="w">(DE-576)259484113</subfield><subfield code="x">0079-6611</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:175</subfield><subfield code="g">pages:171-182</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_U</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ELV</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_20</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_22</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_23</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_24</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_31</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_32</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_40</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_60</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_62</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_63</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_65</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_69</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_73</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_74</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_90</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_95</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_100</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_105</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_110</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_150</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_151</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_224</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_370</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_602</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_702</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2003</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2004</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2005</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2011</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2014</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2015</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2020</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2021</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2025</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2027</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2034</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2038</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2044</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2048</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2049</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2050</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2056</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2059</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2061</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2064</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2065</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2068</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2111</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2113</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2118</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2122</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2129</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2143</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2147</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2148</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2152</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2153</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2190</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2336</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2507</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2522</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4035</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4037</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4112</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4125</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4126</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4242</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4251</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4305</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4313</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4323</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4324</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4326</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4333</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4334</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4335</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4338</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4393</subfield></datafield><datafield tag="936" ind1="b" ind2="k"><subfield code="a">38.90</subfield><subfield code="j">Ozeanologie</subfield><subfield code="j">Ozeanographie</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">175</subfield><subfield code="h">171-182</subfield></datafield></record></collection>
score	7.399522

Nicht das Richtige dabei?

Schreiben Sie uns!

Overview of the multi-layer circulation in the South China Sea

Nicht das Richtige dabei?

Zugang & Verfügbarkeit

Vorhandene Bände

Nicht das Richtige dabei?