Inter-comparison studies between high-resolution HYCOM simulation and observational data: The South Atlantic and the Agulhas leakage system

被引:7
作者
Castellanos, P. [1 ]
Campos, E. J. D. [1 ]
Giddy, I. [1 ,2 ]
Santis, W. [1 ]
机构
[1] Univ Sao Paulo, Inst Oceanog, BR-05508 Sao Paulo, Brazil
[2] Univ Cape Town, Dept Oceanog, ZA-7700 Rondebosch, South Africa
基金
巴西圣保罗研究基金会;
关键词
South Atlantic ocean; Agulhas system; OGCM evaluation; GENERAL-CIRCULATION MODEL; TROPICAL ATLANTIC; OVERTURNING CIRCULATION; EQUATORIAL ATLANTIC; VARIABILITY; RETROFLECTION; TRANSPORT; DYNAMICS; VELOCITY; IMPACT;
D O I
10.1016/j.jmarsys.2016.02.010
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Statistical analyses and model-data inter-comparisons are performed to evaluate the model's ability to reproduce the dynamics in the upper layers (<2000 m) of the South Atlantic ocean. Outputs of an eddy-resolving Ocean General Circulation Model (OGCM) are analyzed and compared with observed data. The model, a 1/12-degree, 22-layer implementation of the Hybrid Coordinate Ocean Model (HYCOM) to the South Atlantic, was forced with monthly-mean products from the NCEP Reanalysis for the period 1960 to 2010. The numerical experiment was capable to reproduce the large scale and the mesoscale dynamic in the South Atlantic and in the Agulhas region. The vertical structure is in agreement with in situ data, the model has lower skill when compared with PIRATA lower temperatures, and is able to capture the seasonal and annual variability in the tropical Atlantic. Furthermore, sensitive change until 2007 is clear in the vertical structure, at 4 degrees N-38 degrees W; 0-35 degrees W and 10 degrees S-10 degrees W, suggesting an important change in the stratification. The primary results concern a significant change in the decadal anomalies of the temperatures and salinity, which exhibit a warmer and saltier water in the southeastern Atlantic. Furthermore, linear trends found in the transport time-series in the North Brazil Current, and the South Equatorial Current were seen to correspond with increasing trends of the warmer water from the Agulhas Current into South Atlantic. The integrated transport during the,period 1960-2010, shows an increase in westward changes in the large-scale circulation south of Africa are show in the negative trends indicate a widening of the "Agulhas gap" and increase in westward volume transport since 1980. It is therefore suggested that variability in the Agulhas System on the last two decades is affecting the dynamic in the South Atlantic, namely the temperature and the volume transport, reach the tropical region of the Atlantic. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:76 / 88
页数:13
相关论文
共 53 条
[1]   Impact of intensified Indian Ocean winds on mesoscale variability in the Agulhas system [J].
Backeberg, Bjoern C. ;
Penven, Pierrick ;
Rouault, Mathieu .
NATURE CLIMATE CHANGE, 2012, 2 (08) :608-612
[2]   On the role of the Agulhas system in ocean circulation and climate [J].
Beal, Lisa M. ;
De Ruijter, Wilhelmus P. M. ;
Biastoch, Arne ;
Zahn, Rainer .
NATURE, 2011, 472 (7344) :429-436
[3]   The velocity and vorticity structure of the Agulhas Current at 32°S [J].
Beal, LM ;
Bryden, HL .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 1999, 104 (C3) :5151-5176
[4]   Agulhas leakage dynamics affects decadal variability in Atlantic overturning circulation [J].
Biastoch, A. ;
Boening, C. W. ;
Lutjeharms, J. R. E. .
NATURE, 2008, 456 (7221) :489-492
[5]   Increase in Agulhas leakage due to poleward shift of Southern Hemisphere westerlies [J].
Biastoch, A. ;
Boening, C. W. ;
Schwarzkopf, F. U. ;
Lutjeharms, J. R. E. .
NATURE, 2009, 462 (7272) :495-U188
[6]  
BLANKE B, 1993, J PHYS OCEANOGR, V23, P1363, DOI 10.1175/1520-0485(1993)023<1363:VOTTAO>2.0.CO
[7]  
2
[8]   An oceanic general circulation model framed in hybrid isopycnic-Cartesian coordinates [J].
Bleck, Rainer .
OCEAN MODELLING, 2002, 4 (01) :55-88
[9]  
Bourles B, 2008, B AM METEOROL SOC, V89, P1111, DOI 10.1175/2008BAMS2462.1
[10]   Circulation in the central equatorial Atlantic: Mean and intraseasonal to seasonal variability [J].
Brandt, P ;
Schott, FA ;
Provost, C ;
Kartavtseff, A ;
Hormann, V ;
Bourles, B ;
Fischer, J .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (07)