Scswbc

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WebbDOI: 10.1016/J.DSR.2007.09.008 Corpus ID: 128743447; Coastal jet separation and associated flow variability in the southwest South China Sea @inproceedings{Gan2008CoastalJS, title={Coastal jet separation and associated flow variability in the southwest South China Sea}, author={Jianping Gan and Tangdong Qu}, … WebbThe SCSwbc has two stable seasonal modes corresponding to the monsoon. In winter, the SCSwbc moves westward along Guangdong continental slope, turns southward oﬀ Hainan Island, and then ﬂ ows southward along the Vietnam coast, arriving near the Natuna Islands. The SCSwbc separates into two branches here. One branch continues to ﬂ ow

Surface Pattern of the South China Sea Western Boundary Current …

WebbSCSWBC is 4.7 Sv (5.6 Sv), which is smaller (larger) than 5.2 Sv in normal years. This study provides robust observational evidence from long-term in situ volume transport monitoring that El Ni~no can have a signiﬁ-cant impact on the SCSWBC through an atmosphere-bridged teleconnection. 1. Introduction Webb28 sep. 2016 · The SCSWBC serves as the main contributor to the redistribution of water properties, momentum, and energy in the SCS [Fang et al., 2012]. Numerous studies have … how to use match and offset function in excel

Features and variability of the South China Sea western …

WebbPatterns of the surface South China Sea western boundary current (SCSwbc) in December 2003, 2004 and 2005 were explored using remote sensing sea surface temperature (SST) and sea level anomaly (SLA) and validated by data from drifting buoys and model output. Paths of the surface SCSwbc were diverse in the northern SCS because of eddies in … Webb1 jan. 2024 · As for the region off Vietnam, a coastal jet usually called the SCS western boundary current (SCSWBC) occurs mainly in winter and summer (e.g., Hu et al., 2000; … WebbThe western boundary current (WBC) in the South China Sea (SCS) flows northward in summer, closely following the Vietnam coast, and splits near 11.2° N into one eastward offshore branch named summertime eastward jet (SEJ). SEJ is significant between 110–112° E, and gradually becomes wider, shallower, weaker and warmer toward … how to use mastery 7 emote

SURFACE PATTERN OF THE SOUTH CHINA SEA WESTERN BOUNDARY CURRENT …

4: The South China Sea Western Boundary Current - World Scientific

WebbThe surface SCSwbc originated in the northern South China Sea (SCS) and flowed southwestward. After the current reached the mid-Vietnamese coast, it intensified, narrowed, and flowed southward along the eastern Vietnamese coast with a speed exceeding 0.8ms −1. The surface SCSwbc was supplied by two branches in each … Webb12 okt. 2012 · The advances in understanding the South China Sea (SCS) western boundary current (SCSwbc) have been reviewed since the works of Dale (1956) and Wyrtki (1961) … organisms that do photosynthesisWebbThe SCSwbc exhibits strong seasonal variation in its direction and patterns. In winter, the current is strong and flows southwestward along the South China shelf and slope from the east of Dongsha Islands to the northern central Vietnamese coast, then turns to the south along the central and southern Vietnamese coast, and finally partially exits the SCS … organisms that eat plant material are called

"Webb5 dec. 2024 · In 0–150 m in the SCS, the CORA salinity is higher in most time of the year. However, in the second half of the year, the salinity is slightly weaker in 100–150 m … " - Scswbc

Scswbc

A general circulation model study of the dynamics of the upper …

Webb21 okt. 2015 · Using merged sea level anomaly and absolute geostrophic velocity products from satellite altimetry and Argos drifter data, we analyzed the reversal process of the South China Sea (SCS) western boundary current (SCSwbc) from a summer to winter pattern in 2011 and important oceanic phenomena during this process. Results show … To estimate the SCSWBC transport, a zonal transect located at 13.8° N and spanning from 109.5° E to 112° E, corresponding to the location of Qui Nhon, was selected for analysis (Fig. 7). By calculating the correlation coefficient of the top 200-m mean velocity magnitude between the SCSWBC axis (109.75° E, 13.8° N; … Visa mer Based on the Sverdrup relation, the wind-driven circulation was proven to be critical for the formation of the upper oceanic circulation in the SCS … Visa mer The ideal experiments conducted by Chen and Xue (2014) suggested that flows through the open straits are of equal importance compared to the monsoon for the formation of the SCSWBC. As the strongest inflow into … Visa mer

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Webb29 juli 2024 · Large‐scale circulations are quite typical processes in the northern South China Sea (SCS) deep basin, yet their impacts on the variation of internal solitary waves (ISWs) remains poorly understood. We, here, focus on impacts of the upstream SCS western boundary current (SCSwbc) and three typical circulation patterns associated … WebbThis chapter summarizes the progress of the South China Sea western boundary current (SCSWBC) based on two reviews published in 2012 and 2013. The content includes the definition of the SCSWBC, the seasonal reversal processes, and the intraseasonal and interannual variations. Some typical features, such as thermohaline and velocity …

Webb1 Structure and variability of the SCSWBC . The studies on the SCSWBC are limited. In 1961, Wyrtki [1] pointed out for the first time that there is a western intensi-fication in the SCS. Using satellite altimeter data, Li et al. [7] noted in 1999 that the SCSWBC is mainly part of the SCS circulation, and that the strongest flow is always located in Webb30 juli 2002 · The SCSWBC in the SCS is the analog to the Kuroshio Current of the North Pacific or the Gulf Stream of the North Atlantic, which are mainly modulated by the …

WebbThe surface SCSwbc originated in the northern South China Sea (SCS) and flowed southwestward. After the current reached the mid-Vietnamese coast, it intensified, … Webb15 mars 2024 · For “U” years, under a strong winter monsoon forcing, the SCSwbc strengthen, the directly wind work and barotropic conversion from the mean kinetic …

Webbmain features of the SCSWBC both in summer and winter from 1992 to 2011 are portrayed. The interannual variability of the SCSWBC and its influencing factors are examined in …

Webb21 juli 2024 · The speedup of internal solitary wave (ISW) induced by upstream South China Sea western boundary current (SCSwbc) is comparable to that induced by Coriolis force, … how to use match bank data in netsuiteWebbThe SCSWBC system consists of the SCS Warm Current (SCSWC) and the Vietnam Coastal Current (VCC). In winter the SCSWBC splits into two branches separated at 14 –18 N. The northern branch is the SCSWC flowing northward and the southern branch is the VCC flowing southward. In summer, however, the SCSWBC flows unidirectionally northward … how to use match appWebb30 jan. 2014 · Westward intensification in marginal seas. Gengxin Chen, H. Xue. Published 30 January 2014. Environmental Science. Ocean Dynamics. An idealized model was used to examine why the strong western boundary current (WBC) is observed in the South China Sea (SCS) but not in the Gulf of Mexico (GOM) and Japan/East Sea (JES). how to use matcha tea setWebbThe SCSWBC is the most important part of the SCS current system. It is associated with the SCS throughflow in the west SCS [ Qu et al ., 2009 ], and interacts with the shelf flows … how to use matcha powder for weight lossWebb1 mars 2009 · The winter western boundary current of the South China Sea: physical structure and volume transport in December 1998. Li Li, Xiaogang Guo, Risheng Wu. Environmental Science. Acta Oceanologica Sinica. 2024. The unique survey in December 1998 mapped the entire western boundary area of the South China Sea (SCS), which … how to use matcha whisk how to use match and indexWebbUpper-layer circulation in the South China Sea has been investigated using a three-dimensional primitive equation eddy-resolving model. The model domain covers the region from 99° to 122°E and from 3° to 23°N. how to use match fields in mail merge