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1.
On the basis of hydrographic data obtained from 28 November to 27 December, 1998, the three-dimensional structure of circulation
in the South China Sea (SCS) is computed using a three-dimensional diagnostic model. The combination of sea surface height
anomaly from altimeter data and numerical results provides a consistent circulation pattern for the SCS, and main circulation
features can be summarized as follows: in the northern SCS there are a cold and cyclonic circulation C1 with two cores C1-1
and C1-2 northwest of Luzon and an anticyclonic eddy (W1) near Dongsha Islands. In the central SCS there is a stronger cyclonic
circulation C2 with two cores C2-1 and C2-2 east of Vietnam and a weaker anticyclonic eddy W2 northwest of Palawan Island.
A stronger coastal southward jet presents west of the eddy C2 and turns to the southeast in the region southwest of eddy C2-2,
and it then turns to flow eastward in the region south of eddy C2-2. In the southern SCS there are a weak cyclonic eddy C3
northwest of Borneo and an anti-cyclonic circulation W3 in the subsurface layer. The net westward volume transport through
section CD at 119.125°E from 18.975° to 21.725°N is about 10.3 × 106 m3s−1 in the layer above 400 m level. The most important dynamic mechanism generating the circulation in the SCS is a joint effect
of the baroclinicity and relief (JEBAR), and the second dynamical mechanism is an interaction between the wind stress and
relief (IBWSR). The strong upwelling occurs off northwest Luzon. 相似文献
2.
夏季南海上层环流动力机制的数值研究 总被引：10，自引：0，他引：10
通过利用一个分区性的正压-斜压衔接模式来探讨夏季南海的上层环流特征及其动力机制,结果表明:夏季期间,由于风生环流的不稳定性促使在东沙群岛附近的气旋涡的强度及位置发生变化,并间接导致黑潮侵入南海北部的程度变化以及气旋涡南侧的反气旋式环流、西沙群岛西南侧的气旋涡的强度和范围出现波动现象;在南海南部的北向西边界流由于离岸的西南季风所驱动在中南半岛中部沿岸脱离岸线往东北方向的流动,导致沿岸的水体大量流失而在沿岸形成一支南向补偿流并在西沙群岛西南侧诱生一气旋涡,而上述的离岸西边界流则作顺时针方向流动,从而在南海南部形成反气旋式大环流;在南沙海槽附近出现的局地气旋涡和万安滩附近的气旋涡分别受β效应、底形效应的作用而形成. 相似文献
3.
冬季南海上层环流动力机制的数值研究 总被引：13，自引：2，他引：13
通过利用一个分区性的正压-斜压衔接模式来探讨冬季南海的上层环流特征及其动力机制,结果表明:(1)在南海北部,流态主要受黑潮的影响,除了东沙群岛西南的大陆架海域以及吕宋岛北部西岸附近各为一反气旋涡外,整个南海北部为一气旋式大环流所控制.(2)在南海南部主要是风生环流,源自粤西沿岸的水体在东北季风的作用下顺南海西边界岸线向南流动,形成一支相当强的西边界流;同时,由于受北康暗沙以南的陆架坡底形效应和β效应的作用,使得在南海南部出现以一个反气旋涡在南沙海槽处产生、发展并向西传播乃至衰减的约50d的周期性过程 相似文献
4.
南海冬、夏季环流的三维数值模拟 总被引：6，自引：0，他引：6
本文利用一个斜压三维陆架海模式——HAMSOM模式对12月份和8月份的南海环流进行数值模拟,结果为:对上层流场,在12月份,在西沙群岛－中沙群岛海区间呈现一个气旋式环流,在越南中部东岸存在一支南向西边界流,在金兰湾的远海为一局地反气旋涡,在南海南部,主要表现为万安滩的气旋式大弯曲(气旋涡)及在北康暗沙北侧的反气旋涡;在8月份,在东沙群岛－中沙群岛－吕宋岛西侧海域间存在一大尺度的气旋涡,在南海西部主要表现为以西沙群岛南部的气旋涡与金兰湾－礼乐滩间的反气旋式大环流相对峙的局面,同时在万安滩东侧有－气旋涡.由于斜压效应、底形效应的作用,使冬、夏季的南海南部中层流场几乎与上层流场相反. 相似文献
5.
孟加拉湾上层环流研究综述 总被引：2，自引：0，他引：2
综述了孟加拉湾上层环流研究的主要成果并指出,研究海区环流与季风转换不完全同步。在西南季风期间,南、北海区各有一气旋式环流;在秋季季风过渡期间,出现海湾尺度的气旋式环流;在东北季风期间,气旋式环流减弱北移,南部则为一反气旋式环流控制;春季与秋季的情形相反,整个湾出现一海湾尺度的反气旋式环流。研究海区环流的变异主要受季风、赤道远地作用和浮力通量等复杂外源作用的影响。东印度沿岸流的季节变化与季风转换也不同步,局地风、内部Ekman抽吸、远地沿岸风及赤道远地作用的影响对沿岸流周年变化有重要作用。孟加拉湾上层环流年际变化显著,此年际变化主要受赤道风场的影响。 相似文献
6.
On the basis of hydrographic data obtained from 12 June to 6 July, 1998, the three-dimensional structure of circulation in
the South China Sea (SCS) is computed using a three-dimensional diagnostic model. The combination of sea surface height anomaly
from altimeter data and numerical results provides a consistent circulation pattern for the SCS, and the main circulation
features can be summarized as follows: In the northern SCS there are a cyclonic eddy C1 near Dongsha Islands and an anti-cyclonic
eddy W1 west of Luzon Island. In the central SCS a strong anti-cyclonic eddy W3 and a cyclonic eddy C3 compose a quasi-dipole
southeast of Vietnam. A coastal northward jet is present at the western boundary near the Vietnam coast above 300 m level.
This northward coastal jet flows northward and turns eastward at about 14°N, and then flows southeastward into the area between
eddies W3 and C3. In the southern SCS the current is weaker. The most important dynamic mechanism underlying the circulation
in the SCS is the joint effect of the baroclinicity and relief (JEBAR), and the second dynamical mechanism is the interaction
between the wind stress and relief (IBWSR). Comparison of the characters of circulation in the SCS during summer 2000 with
that during summer 1998 reveals no obvious variability of the main characteristics. 相似文献
7.
1998年冬季南海环流的三维结构 总被引：10，自引：3，他引：7
利用1998年11月28日至12月27日南海的调查资料,采用三维海流诊断模式,计算了冬季南海三维海流,所得结果如下:(1)冬季南海环流系统方面:1)南海北部,在吕宋西北海域分别存在一个气旋式、反气旋式涡.2)南海中部,在越南近岸存在较强的、南向的西边界射流.其以东海域出现较强的气旋式环流.南海中部东侧海域存在一个较弱的反气旋式环流.3)南海南部,一般流速较弱.在112°E以西受反气旋式环流所控制,加里曼丹岛西北海域存在气旋性环流.由于受调查海域所限,这两个环流只部分出现.(2)上述环流系统与200 m层水平温度、密度分布对应较好.(3)南海冬季环流垂向速度分布方面:1)表层,南海北部,在吕宋西北为范围较大的上升流海区.而在东沙群岛附近海域出现了下降流.海南岛以南及东南海域也存在下降流.南海中部,越南以东海域出现范围较大的下降流,其以东为上升流海域,而在巴拉望岛西北海域又出现下降流.南海南部,基本上被上升流海域所控制.2)次表层与表层不同,例如在次表层,海南岛东南部海域出现上升流.中层和深层垂向速度分布与次表层相似.(4)关于南海垂向速度分量分布的动力原因:在表层,风应力旋度场起着主要作用;在次表层,β效应与斜压场相互作用是重要的动力因子,而风应力旋度场和β效应与正压场相互作用也有一定影响;在南海中部等区域的中层以及在南海的深层,主要受B效应与斜压场相互作用和B效应与正压场相互作用的共同作用. 相似文献
8.
The seasonal climatic circulation of the sea reconstructed on the basis of assimilation of new arrays of many-year average
hydrological data in a model is analyzed. Five layers are discovered in the structure of climatic currents in the sea in depth:
the surface Ekman layer (∼ 10 m), a layer with small vertical gradients of the kinetic energy (∼ 10–60 m), a layer with relatively
high vertical gradients of the kinetic energy (∼ 60–150 m), a layer with gradual decrease in the kinetic energy and intensification
(from 250–350 m) of the east cyclonic gyre and Batumi anticyclonic eddy (∼ 150–1000 m), and an abyssal layer characterized
by an almost barotropic velocity (∼ 1000–2000 m). The specific features of the seasonal evolution of currents at these depths
are investigated. It is shown that the key role in the formation of deep-water circulation of the sea is played by the south
east flow, east cyclonic gyre, and Batumi anticyclonic eddy.
__________
Translated from Morskoi Gidrofizicheskii Zhurnal, No. 6, pp. 28–45, November–December, 2005. 相似文献
9.
A coupled single-layer/two-layer model is employed to study the South China Sea (SCS) upper circulation and its response before and after the onset of summer monsoon. It is found that, in summer, due to the β effect and the first baroclinic mode of the wind-driven current, a northward western boundary jet current is formed along the Indo-China Peninsula coast, and it leaves the coast at about 13° N and diffuses towards northeast; next to the Indo-China Peninsula, a large anticyclonic 相似文献
10.
11.
利用25年(1993—2017)的卫星高度计资料, 采用复经验正交函数(complex empirical orthogonal function, CEOF)方法, 分析南海北部海区海面高度季节内变异的时空分布及传播特征。标准差分析表明, 南海北部海面高度的季节内变异(intra-seasonal variability of sea level anomalies, SLA-ISV)在沿陆坡外侧区较强, 且SLA-ISV表现出明显的季节性变化, 冬半年强于夏半年。CEOF前两个主要模态能较好地揭示研究海区SLA-ISV的时空分布及其传播特征, 并表明SLA-ISV的强度受到季节性变化和年际变化的调制。全年CEOF的第一模态揭示SLA-ISV从台湾岛西南至西沙群岛以东区域的冬半年西南向传播特征; 而全年CEOF的第二模态则表现了SLA-ISV分别在台湾岛西南和东沙群岛西南的西南向传播特征。南海北部中尺度涡季节变化统计分析表明, CEOF的分解结果与南海北部的涡旋活动一致。 相似文献
12.
The continental slope in the northern South China Sea(SCS) is rich in mesoscale eddies which play an important role in transport and retention of nutrients and biota. In this study, we investigate the statistical properties of eddy distributions and propagation in a period of 24 years between 1993 and 2016 by using the altimeter data. A total of 147 eddies are found in the continental slope region(CSR), including 70 cyclonic eddies(CEs) and 77 anticyclonic eddies(ACEs). For those eddies that appear in the CSR, the surrounding areas of Dongsha Islands(DS) and southwest of Taiwan(SWT) are considered as the primary sources, where eddies generated contribute more than 60% of the total. According to the spatial distribution of eddy relative vorticity, eddies are weakening as propagating westward. Although both CEs and ACEs roughly propagate along the slope isobaths, there are discrepancies between CEs and ACEs. The ACEs move slightly faster in the zonal direction, while the CEs tend to cross the isobaths with large bottom depth change. The ACEs generally move further into the basin areas after leaving the CSR while CEs remain around the CSR. The eddy propagation on the continental slope is likely to be associated with mean flow at a certain degree because the eddy trajectories have notable seasonal signals that are consistent with the seasonal cycle of geostrophic current. The results indicate that the eddy translation speed is statistically consistent with geostrophic velocity in both magnitude and direction. 相似文献
13.
Patterns of upper layer circulation variability in the South China Sea from satellite altimetry using the self-organizing map 总被引：2，自引：2，他引：0
Patterns of the South China Sea (SCS) circulation variability are extracted from merged satellite altimetry data from October 1992 through August 2004 by using the self-organizing map (SOM). The annual cycle, seasonal and inter-annual variations of the SCS surface circulation are identified through the evolution of the characteristic circulation patterns. The annual cycle of the SCS gener- al circulation patterns is described as a change between two opposite basin-scale SW-NE oriented gyres embedded with eddies: low sea surface height anomaly (SSHA) (cyclonic) in winter and high SSHA (anticyclonic) in summer half year. The transition starts from July--August (January--February) with a high (low) SSHA tongue east of Vietnam around 12°～14° N, which de- velopa into a big anticyclonic (cyclonic) gyre while moving eastward to the deep basin. During the transitions, a dipole structure, cyclonic (anticyclonic) in the north and anticyclonic (cyclonic) in the south, may be formed southeast off Vietnam with a strong zonal jet around 10°～12° N. The seasonal variation is modulated by the interannual variations. Besides the strong 1997/1998 e- vent in response to the peak Pacific El Nino in 1997, the overall SCS sea level is found to have a significant rise during 1999～ 2001, however, in summer 2004 the overall SCS sea level is lower and the basin-wide anticyclonic gyre becomes weaker than the other years. 相似文献
14.
P矢量方法在南海夏季环流诊断计算中的应用 总被引：8，自引：4，他引：8
基于1998年6～7月南海调查航次的CTD资料,对南海环流采用最近发展的P矢量方法进行诊断计算.计算结果:黑潮向西入侵南海,然后做反气旋弯曲向东北方向流动,最终有通过巴士海峡流出南海的趋势.在南海北部存在一个气旋性环流,这个环流的强度和范围随深度增加而减小.该环流的冷中心位置随深度增加稍向南移.南海中部、越南以东海域存在一个明显的气旋涡和反气旋涡,尤其在200m及其以上水层均相当稳定,反气旋涡位于越南以东,其中心位置在11°53'N,111°50'E,气旋涡的中心位置在13°17'N,112°55'E,两者的尺度皆约为250km.吕宋岛西侧存在一个反气旋涡.在计算海区南部、巴拉望岛西南海域,100m以上层存在一个反气旋式涡.从各层流场分布均可以显示海流在西部强化的现象. 相似文献
15.
Calculation of circulation in the South China Sea during summer of 2000 by the modified inverse method 总被引：3，自引：0，他引：3
YUAN Yaochu LIU Yonggang LIAO Guanghong LOU Ruyun SU Jilan WANG Kangshan 《海洋学报(英文版)》2005,24(1):14-30
On the basis of hydrographic data obtained in August 2000 cruise, the circulation in the South China Sea (SCS) is computed by the modified inverse method in combination with SSH data from TOPEX/ERS-2 analysis. For study of the dynamical mechanism, which causes the pattern of summer circulation in the SCS, the diagnostic model (Yuan et al. 1982. Acta Oceanologica Sinica,4(1):1-11; Yuan and Su. 1992. Numerical Computation of Physical Oceanography.474-542) is used to simulate numerically the summer circulation in the SCS. The following results 相似文献
16.
基于南沙群岛海域综合科学考察11个航次的实测资料,研究了南沙群岛海域的混合层深度季节变化特征。研究结果表明,南沙群岛海域混合层深度存在明显的季节变化,并且与季风和海表热通量的变化密切相关。春季,风速较小且风向不稳定,海面得到的净热通量全年最大,上层水体层结稳定,混合层深度较小;夏季,南海西南季风盛行,上层为反气旋式环流,海面得到的净热通量减少,混合层呈加深的趋势;秋季,海面净热通量继续减少,混合层深度达到最大值;冬季,东北季风驱动下形成的上层气旋式环流引起深层冷水的上升,限制了混合层的加深。 相似文献
17.
东沙群岛西南海区的溶解氧、活性磷酸盐和活性硅酸盐100m层四季的平面等值线出现封闭或半封闭的分布,表明了该海域气旋型涡旋的终年存在,溶解氧饱和度的断面分布也证实了东沙群岛西南海域终年存在下层海水抬升,并表明冷涡轴随深度增加而向东南方向倾斜。温度、盐度、溶解氧.活性磷酸盐在表层都有一均匀层,次表层有一跃层,而深层值则季节变化不大。 相似文献
18.
19.
A three-dimensional numerical model is used to simulate sea level and velocity variations in the South China Sea for 1992–1995. The model is driven by daily wind and daily sea surface temperature fields derived from the NCEP/NCAR 40-year reanalysis project. The four-year model outputs are analyzed using time-domain Empirical Orthogonal Functions (EOF). Spatial and temporal variations of the first two modes from the simulation compare favorably with those derived from satellite altimetry. Mode 1, which is associated with a southern gyre, shows symmetric seasonal reversal. Mode 2, which contributes to a northern gyre, is responsible for the asymmetric seasonal and interannual variations. In winter, the southern and northern cyclonic gyres combine into a strong basin-wide cyclonic gyre. In summer, a cyclonic northern gyre and an anticyclonic southern gyre form a dipole with a jet leaving the coast of Vietnam. Interannual variations are particularly noticeable during El Niño. The winter gyre is generally weakened and confined to the southern basin, and the summer dipole structure does not form. Vertical motions weaken accordingly with the basin-wide circulation. Variations of the wind stress curl in the first two EOF modes coincide with those of the model-derived sea level and horizontal velocities. The mode 1 wind stress curl, significant in the southern basin, coincides with the reversal of the southern gyre. The mode 2 curl, large in the central basin, is responsible for the asymmetry in the winter and summer gyres. Lack of the mode 2 contribution during El Niño events weakens the circulation. The agreement indicates that changes in the wind stress curl contribute to the seasonal and interannual variations in the South China Sea. 相似文献
20.
Argo floats revealing bimodality of large-scale mid-depth circulation in the North Atlantic 总被引：1，自引：1，他引：0
Analysis of Argo float trajectories at 1 000 m and temperature at 950 m in the North Atlantic between November 2003 and January 2005 demonstrates the existence of two different circulation modes with fast transition between them. Each mode has a pair of cyclonic - anticyclonic gyres. The difference is the location of the cyclonic gyre. The cyclonic gyre stretches from southeast to northwest in the first mode and from the southwest to the northeast in the second mode. The observed modes strongly affect the heat and salt transport in the North Atlantic. In particular, the second mode slows down the westward transport of the warm and saline water from the Mediterranean Sea. 相似文献