Intraseasonal variability of the South Vietnam upwelling, South China Sea: influence of atmospheric forcing and ocean intrinsic variability
-
Published:2023-04-17
Issue:2
Volume:19
Page:453-467
-
ISSN:1812-0792
-
Container-title:Ocean Science
-
language:en
-
Short-container-title:Ocean Sci.
Author:
Herrmann Marine,To Duy Thai,Estournel Claude
Abstract
Abstract. The South Vietnam upwelling (SVU) develops off the Vietnamese coast (South
China Sea, SCS) during the southwest summer monsoon over four main areas: the
northern coastal upwelling (NCU), the southern coastal upwelling (SCU), the
offshore upwelling (OFU) and the shelf off the Mekong River mouth (MKU). An
ensemble of 10 simulations with perturbed initial conditions were run with
the fine-resolution SYMPHONIE model (1 km inshore) to investigate the daily
to intraseasonal variability of the SVU and the influence of the ocean
intrinsic variability (OIV) during the strong SVU of summer 2018. The intraseasonal variability is similar for the SCU, MKU and OFU, driven to the
first order by the wind variability. The MKU and SCU are induced by stable ocean
dynamics (the northeastward then eastward boundary current) and have very
little chaotic variability. The OIV has a stronger influence on OFU. In
July, OFU mainly develops along the northern flank of the eastward jet. The
influence of the OIV is strongest and related to the chaotic variability of the
meridional position of the jet. In August, this position is stable and OFU
develops mainly in the area of positive wind curl and cyclonic eddies north
of the jet. The influence of the OIV, weaker than in July, is related to the
organization of this mesoscale circulation. The NCU shows a behavior different
from that observed in the other areas. In the heart of summer, a large-scale
circulation formed by the eastward jet and eddy dipole is well established
with an alongshore current preventing the NCU development. In early and late
summer, this circulation is weaker, allowing a mesoscale circulation of
strongly chaotic nature to develop in the NCU area. During those periods,
the OIV influence on the NCU is very strong and related to the organization of
this mesoscale circulation: the NCU is favored (annihilated) by
offshore-oriented (alongshore) structures.
Funder
Vietnam Academy of Science and Technology
Publisher
Copernicus GmbH
Subject
Cell Biology,Developmental Biology,Embryology,Anatomy
Reference37 articles.
1. Bombar, D., Dippner, J. W., Doan, H. N., Ngoc, L. N., Liskow, I.,
Loick-Wilde, N., and Voss, M.: Sources of new nitrogen in the Vietnamese
upwelling region of the South China Sea, J. Geophys. Res.-Ocean., 115, 6018,
https://doi.org/10.1029/2008JC005154, 2010. 2. Chen, C. and Wang, G.: Interannual variability of the eastward current in
the western South China Sea associated with the summer Asian monsoon, J.
Geophys. Res.-Ocean., 119, 5745–5754, https://doi.org/10.1002/2014JC010309,
2014. 3. Chen, C., Lai, Z., Beardsley, R. C., Xu, Q., Lin, H., and Viet, N. T.:
Current separation and upwelling over the southeast shelf of Vietnam in the
South China Sea, J. Geophys. Res.-Ocean., 117, 1–16,
https://doi.org/10.1029/2011JC007150, 2012. 4. Da, N. D., Herrmann, M., Morrow, R., Niño, F., Huan, N. M., and Trinh,
N. Q.: Contributions of Wind, Ocean Intrinsic Variability, and ENSO to the
Interannual Variability of the South Vietnam Upwelling: A Modeling Study, J.
Geophys. Res.-Ocean., 124, 6545–6574, https://doi.org/10.1029/2018JC014647,
2019. 5. Dippner, J. W., Nguyen, K. V., Hein, H., Ohde, T., and Loick, N.:
Monsoon-induced upwelling off the Vietnamese coast, Ocean Dynam., 57, 46–62,
https://doi.org/10.1007/S10236-006-0091-0, 2007.
Cited by
4 articles.
订阅此论文施引文献
订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
|
|