Tidal Effects on Circulation in and near the East China Sea

We incorporate tidal currents into a previously validated, three-dimensional, subtidal circulation model to assess tidal effects on the circulation in and around the East China Sea. Of particular interest is the tide-enhanced Changjiang plume dispersal and circulation in the southern East China Sea....
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Hung-Jen Lee [verfasserIn] Shenn-Yu Chao [verfasserIn] Kon-Kee Liu [verfasserIn] Shih-Jen Huang [verfasserIn] Gwo-Ching Gong [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2014

Schlagwörter:	Changjiang plume Taiwan Warm Current Tidal residual coastal flow

Übergeordnetes Werk:	In: Terrestrial, Atmospheric and Oceanic Sciences - Springer, 2016, 25(2014), 2, p 233
Übergeordnetes Werk:	volume:25 ; year:2014 ; number:2, p 233

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc Journal toc

DOI / URN:	10.3319/TAO.2013.10.08.01(Oc)

Katalog-ID:	DOAJ024803812

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520			\|a We incorporate tidal currents into a previously validated, three-dimensional, subtidal circulation model to assess tidal effects on the circulation in and around the East China Sea. Of particular interest is the tide-enhanced Changjiang plume dispersal and circulation in the southern East China Sea. The modeling results show that without tides, the Changjiang plume in summer presents itself as a stagnant, expansive pool in regions bordering the northern East China Sea and Yellow Sea, too far north and too accumulating relative to observations. The winter plume dispersal pushed by the north-northeast monsoon follows the China coastline southeastward as a coastal current that matches more closely with observations with or without tides. Incorporating the effect of tides brings the model closer to observation, especially in summer. During summer the Taiwan Warm Current shifts to lower latitudes, enhances upwelling off southeast China and induces a southward tidal residual coastal flow off southeast China. Tides also induce the observed seaward detachment of the summer plume. In winter, the prevailing north-northeast monsoon suppresses the Taiwan Warm Current to the minimum. However, if the winter monsoon is weakened for a few weeks, the Taiwan Warm Current reappears and these three mechanisms begin to operate as in summer. CTD surveys and satellite observations south of the Changjiang River estuary contribute to a better understanding of the tidal effects on regional ocean currents.
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callnumber-first	Q - Science
author	Hung-Jen Lee
spellingShingle	Hung-Jen Lee misc QE1-996.5 misc QC801-809 misc Changjiang plume misc Taiwan Warm Current misc Tidal residual coastal flow misc Geology misc Geophysics. Cosmic physics Tidal Effects on Circulation in and near the East China Sea
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topic_title	QE1-996.5 QC801-809 Tidal Effects on Circulation in and near the East China Sea Changjiang plume Taiwan Warm Current Tidal residual coastal flow
topic	misc QE1-996.5 misc QC801-809 misc Changjiang plume misc Taiwan Warm Current misc Tidal residual coastal flow misc Geology misc Geophysics. Cosmic physics
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title	Tidal Effects on Circulation in and near the East China Sea
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title_full	Tidal Effects on Circulation in and near the East China Sea
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title_sort	tidal effects on circulation in and near the east china sea
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title_auth	Tidal Effects on Circulation in and near the East China Sea
abstract	We incorporate tidal currents into a previously validated, three-dimensional, subtidal circulation model to assess tidal effects on the circulation in and around the East China Sea. Of particular interest is the tide-enhanced Changjiang plume dispersal and circulation in the southern East China Sea. The modeling results show that without tides, the Changjiang plume in summer presents itself as a stagnant, expansive pool in regions bordering the northern East China Sea and Yellow Sea, too far north and too accumulating relative to observations. The winter plume dispersal pushed by the north-northeast monsoon follows the China coastline southeastward as a coastal current that matches more closely with observations with or without tides. Incorporating the effect of tides brings the model closer to observation, especially in summer. During summer the Taiwan Warm Current shifts to lower latitudes, enhances upwelling off southeast China and induces a southward tidal residual coastal flow off southeast China. Tides also induce the observed seaward detachment of the summer plume. In winter, the prevailing north-northeast monsoon suppresses the Taiwan Warm Current to the minimum. However, if the winter monsoon is weakened for a few weeks, the Taiwan Warm Current reappears and these three mechanisms begin to operate as in summer. CTD surveys and satellite observations south of the Changjiang River estuary contribute to a better understanding of the tidal effects on regional ocean currents.
abstractGer	We incorporate tidal currents into a previously validated, three-dimensional, subtidal circulation model to assess tidal effects on the circulation in and around the East China Sea. Of particular interest is the tide-enhanced Changjiang plume dispersal and circulation in the southern East China Sea. The modeling results show that without tides, the Changjiang plume in summer presents itself as a stagnant, expansive pool in regions bordering the northern East China Sea and Yellow Sea, too far north and too accumulating relative to observations. The winter plume dispersal pushed by the north-northeast monsoon follows the China coastline southeastward as a coastal current that matches more closely with observations with or without tides. Incorporating the effect of tides brings the model closer to observation, especially in summer. During summer the Taiwan Warm Current shifts to lower latitudes, enhances upwelling off southeast China and induces a southward tidal residual coastal flow off southeast China. Tides also induce the observed seaward detachment of the summer plume. In winter, the prevailing north-northeast monsoon suppresses the Taiwan Warm Current to the minimum. However, if the winter monsoon is weakened for a few weeks, the Taiwan Warm Current reappears and these three mechanisms begin to operate as in summer. CTD surveys and satellite observations south of the Changjiang River estuary contribute to a better understanding of the tidal effects on regional ocean currents.
abstract_unstemmed	We incorporate tidal currents into a previously validated, three-dimensional, subtidal circulation model to assess tidal effects on the circulation in and around the East China Sea. Of particular interest is the tide-enhanced Changjiang plume dispersal and circulation in the southern East China Sea. The modeling results show that without tides, the Changjiang plume in summer presents itself as a stagnant, expansive pool in regions bordering the northern East China Sea and Yellow Sea, too far north and too accumulating relative to observations. The winter plume dispersal pushed by the north-northeast monsoon follows the China coastline southeastward as a coastal current that matches more closely with observations with or without tides. Incorporating the effect of tides brings the model closer to observation, especially in summer. During summer the Taiwan Warm Current shifts to lower latitudes, enhances upwelling off southeast China and induces a southward tidal residual coastal flow off southeast China. Tides also induce the observed seaward detachment of the summer plume. In winter, the prevailing north-northeast monsoon suppresses the Taiwan Warm Current to the minimum. However, if the winter monsoon is weakened for a few weeks, the Taiwan Warm Current reappears and these three mechanisms begin to operate as in summer. CTD surveys and satellite observations south of the Changjiang River estuary contribute to a better understanding of the tidal effects on regional ocean currents.
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container_issue	2, p 233
title_short	Tidal Effects on Circulation in and near the East China Sea
url	https://doi.org/10.3319/TAO.2013.10.08.01(Oc) https://doaj.org/article/a2e6a57023c546b8893a53ed246328f6 http://tao.cgu.org.tw/media/k2/attachments/v252p233.pdf https://doaj.org/toc/1017-0839 https://doaj.org/toc/2311-7680
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up_date	2024-07-04T00:26:42.719Z
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Tidal Effects on Circulation in and near the East China Sea

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