孟加拉湾及其毗邻海域中尺度涡旋活动的冬、夏季差异

黄挺, 周锋, 田娣, 张家赢

海洋学研究 ›› 2020, Vol. 38 ›› Issue (3) : 21-30.

PDF(5650 KB)
PDF(5650 KB)
海洋学研究 ›› 2020, Vol. 38 ›› Issue (3) : 21-30. DOI: 10.3969/j.issn.1001-909X.2020.03.003
研究论文

孟加拉湾及其毗邻海域中尺度涡旋活动的冬、夏季差异

  • 黄挺1,2, 周锋*1,2,3, 田娣1,2, 张家赢1,2
作者信息 +

Seasonal variations of mesoscale eddy in the Bay of Bengal and its adjacent regions

  • HUANG Ting1,2, ZHOU Feng*1,2,3, TIAN Di1,2, ZHANG Jiaying1,2
Author information +
文章历史 +

摘要

基于1993—2017年从卫星高度计资料中识别出来的中尺度涡轨迹数据集,对冬、夏季孟加拉湾涡旋的源地和性质进行了研究。研究表明孟加拉湾西部、安达曼海和孟加拉湾通往赤道的出口处的中尺度涡旋活动呈现显著的季节性差异。安达曼海在冬、夏季从北往南中尺度涡旋分别以“反气旋涡-气旋涡-反气旋涡”和“气旋涡-反气旋涡-气旋涡”的格局分布。不同源区涡旋的季节性生长过程有明显差异。孟加拉湾西部的涡旋在夏季生长迅速但消散缓慢,斯里兰卡冷涡生长缓慢但消散迅速。不同源区涡旋半径和振幅大小有不同的特征。孟加拉湾西部,无论冬、夏季,反气旋涡的振幅、半径都比气旋涡大;夏季季风漂流区,气旋涡半径比反气旋涡小但是振幅比反气旋涡大;安达曼海内无论冬、夏季都是最北侧聚集区涡旋的半径和振幅最大。孟加拉湾内生命史为30~40 d的涡旋数量最多,生命史在100 d以上的涡旋主要分布在孟加拉湾西部。

Abstract

Distribution of eddy originations and characteristics of eddies in summer and winter in the Bay of Bengal (BOB) from 1993 to 2017 were analyzed based on Mesoscale Eddy Trajectory Atlas Product provided by AVISO. Seasonal variabilities of mesoscale eddies were found mainly in the western BOB, the Andaman Sea and the southern BOB. Eddies in the Andaman Sea distribute from north to south with order of “anticyclones-cyclones-anticyclones” and “cyclones-anticyclones-cyclones” in winter and summer respectively. Growth of eddies has seasonal variabilities and varies from different regions. Eddies in the western BOB intensify rapidly but vanish slowly in summer. Sri Lanka cold eddies intensify slowly but vanish rapidly. Amplitude and radius of eddies are different in different regions. Amplitude and radius of anticyclones are larger than those of cyclones whenever in summer or winter in the western BOB. Radius of anticyclones is larger than that of cyclones near the Southwest Monsoon Current. While, amplitude of anticyclones is smaller than that of cyclones. Amplitude and radius of eddies northernmost are the largest whenever in summer or winter in the Andaman Sea. Eddies with lifetime about 30-40 days are the largest number in the Bay of Bengal. Eddies with long lifetime mainly distribute in the western BOB.

关键词

孟加拉湾 / 中尺度涡 / 季节变化

Key words

Bay of Bengal / mesoscale eddy / seasonal variability

引用本文

导出引用
黄挺, 周锋, 田娣, 张家赢. 孟加拉湾及其毗邻海域中尺度涡旋活动的冬、夏季差异[J]. 海洋学研究. 2020, 38(3): 21-30 https://doi.org/10.3969/j.issn.1001-909X.2020.03.003
HUANG Ting, ZHOU Feng, TIAN Di, ZHANG Jiaying. Seasonal variations of mesoscale eddy in the Bay of Bengal and its adjacent regions[J]. Journal of Marine Sciences. 2020, 38(3): 21-30 https://doi.org/10.3969/j.issn.1001-909X.2020.03.003
中图分类号: P731.2   

参考文献

[1] BABU M T, KUMAR P S, RAO D P. A subsurface cyclonic eddy in the Bay of Bengal[J]. Journal of Marine Research, 1991, 49(3): 403-410.
[2] GOPALAN A K S, KRISHNA V V G, ALI M M, et al. Detection of Bay of Bengal eddies from TOPEX and in situ observations[J]. Journal of Marine Research, 2000, 58(5): 721-734.
[3] KUMAR P S, NUNCIO M, RAMAIAH N, et al. Eddy-mediated biological productivity in the Bay of Bengal during fall and spring inter-monsoons[J]. Deep Sea Research Part I: Oceanographic Research Papers, 2007, 54(9): 1619-1640.
[4] 邱云,李立,周喜武.斯里兰卡冷涡及其成因分析[J].热带海洋学报,2008, 27(4):45-51.
QIU Yun, LI Li, ZHOU Xiwu. Sri Lanka cold eddy and its generation mechanism analysis[J]. Journal of Tropical Oceanography, 2008, 27(4): 45-51.
[5] CHEN Gengxin, WANG Dongxiao, HOU Yijun. The features and interannual variability mechanism of mesoscale eddies in the Bay of Bengal[J]. Continental Shelf Research, 2012, 47(10): 178-185.
[6] CUI Wei, YANG Jungang, MA Yi. A statistical analysis of mesoscale eddies in the Bay of Bengal from 22-year altimetry data[J]. Acta Oceanologica Sinica, 2016, 35(11): 16-27.
[7] DANDAPAT S, CHAKRABORTY A. Mesoscale eddies in the western Bay of Bengal as observed from satellite altimetry in 1993—2014: statistical characteristics, variability and three-dimensional properties[J]. IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing, 2016, 9(11): 5044-5054.
[8] 常景龙,邱云,林新宇,等.孟加拉湾中尺度涡的总体特征与季节变化[J].应用海洋学学报,2019,38(2):149-158.
CHANG Jinglong, QIU Yun, LIN XinYu, et al. General features and seasonal variation of mesoscale eddies in the Bay of Bengal[J]. Journal of Applied Oceanography, 2019, 38(2): 149-158.
[9] BRYDEN H L, BRADY E C. Eddy momentum and heat fluxes and their effects on the circulation of the equatorial Pacific Ocean[J]. Journal of Marine Research, 1989, 47(1): 55-79.
[10] CHELTON D B, SCHLAX M G, SAMELSON R M. Global observations of nonlinear mesoscale eddies[J]. Progress in Oceanography, 2011, 91(2): 167-216.
[11] BABU M T, SARMA Y V B, MURTY V S N, et al. On the circulation in the Bay of Bengal during northern spring inter-monsoon (March-April 1987)[J]. Deep Sea Research Part II: Topical Studies in Oceanography, 2003, 50(5): 855-865.
[12] MURTY V S N, SARMA Y V B, RAO D P, et al. Water characteristics, mixing and circulation in the Bay of Bengal during southwest monsoon[J]. Journal of Marine Research, 1992, 50(2): 207-228.
[13] SURYANARAYANA A, MURTY V S N, RAO D P. Hydrography and circulation of the Bay of Bengal during early winter, 1983[J]. Deep Sea Research Part I: Oceanographic Research Papers, 1993, 40(1): 205-217.
[14] EIGENHEER A, QUADFASEL D. Seasonal variability of the Bay of Bengal circulation inferred from TOPEX/Poseidon altimetry[J]. Journal of Geophysical Research, 2000, 105(C2): 3243-3252.
[15] SOMAYAJULU Y K, MURTY V S N, SARMA Y V B. Seasonal and inter-annual variability of surface circulation in the Bay of Bengal from TOPEX/Poseidon altimetry[J]. Deep Sea Research Part II: Topical Studies in Oceanography, 2003, 50(5): 867-880.
[16] 邱云,李立.孟加拉湾上层环流研究综述[J].海洋科学进展,2006, 24(4):593-603.
QIU Yun, LI Li. Review of study on upper ocean circulation in the Bay of Bengal[J]. Advances in Marine Science, 2006, 24(4): 593-603.
[17] 邱云.孟加拉湾上层环流及其变异研究[D].厦门:厦门大学,2007.
QIU Yun. The circulation of the BOB and its variations[D]. Xiamen: Xiamen University, 2007.
[18] LEGECKIS R. Satellite observations of a western boundary current in the Bay of Bengal[J]. Journal of Geophysical Research, 1987, 92(C12): 12974-12978.
[19] SHETYE S R, GOUVEIA A D, SHENOI S S C, et al. The western boundary current of the seasonal subtropical gyre in the Bay of Bengal[J]. Journal of Geophysical Research, 1993, 98(C1): 945-954.
[20] SANILKUMAR K V, KURUVILLA T V, JOGENDRANATH D, et al. Observations of the Western Boundary Current of the Bay of Bengal from a hydrographic survey during March 1993[J]. Deep-Sea Research Part I, 1997, 44(1): 135-145.
[21] SCHOTT F A, MCCREARY J P. The monsoon circulation of the Indian Ocean[J]. Progress in Oceanography, 2001, 51(1): 1-123.
[22] CNES. Mesoscale eddy trajectory atlas product handbook: SALP-MU-P-EA-23126-CLS: issue 3.0[Z/OL].[2020-03-25].https://www.aviso.altimetry.fr/fileadmin/documents/data/tools/hdbk_eddytrajectory_META2018.pdf.
[23] KURIEN P, IKEDA M, VALSALA V K. Mesoscale variability along the east coast of India in spring as revealed from satellite data and OGCM simulations[J]. Journal of Oceanography, 2010, 66(2): 273-289.
[24] 尚晓东,徐驰,陈桂英,等.海洋中尺度涡的机械能及其源汇研究[J].热带海洋学报,2013,32(2):24-36.
SHANG Xiaodong, XU Chi, CHEN Guiying, et al. Review on mechanical energy of ocean eddies and associated energy sources and sinks[J]. Journal of Tropical Oceanography, 2013, 32(2): 24-36.
[25] VINAYACHANDRAN P N, MURTY V S, BABU V R, et al. Observations of barrier layer formation in the Bay of Bengal during summer monsoon[J]. Journal of Geophysical Research, 2002, 107(C12): 129.
[26] THADATHIL P, GOPALAKRISHNA V V, MURALEEDHARAN P M,et al. Surface layer temperature inversion in the Bay of Bengal[J]. Deep Sea Research Part I, 2002, 49(10): 1818.
[27] 李奎平,王海员,杨洋,等.孟加拉湾北部逆温现象的观测特征及机制分析[J].海洋学报,2016,38(7):22-31.
LI Kuiping, WANG Haiyuan, YANG Yang, et al. Observed characteristics and mechanisms of temperature inversion in the northern Bay of Bengal[J].Haiyang Xuebao, 2016, 38(7): 22-31.
[28] BÖNING C W, BUDICH R G. Eddy dynamics in a primitive equation model: sensitivity to horizontal resolution and friction[J]. Journal of Physical Oceanography, 1992, 22(4): 361-381.
[29] XUE H, BANE J M. A numerical investigation of the Gulf Stream and its meanders in response to cold air outbreaks[J]. Journal of Physical Oceanography, 1997, 27(12): 2606-2629.
[30] ZHUANG Wei, XIE Shangping, WANG Dongxiao, et al. Intra-seasonal variability in sea surface height over the South China Sea[J]. Journal of Geophysical Research, 2010, 115: C04010.
[31] MCCREARY J P, KUNDU P K, MOLINARI R L. A numerical investigation of dynamics, thermodynamics and mixed-layer processes in the Indian Ocean[J]. Progress in Oceanography, 1993, 31(3): 181-244.
[32] MCCREARY J P, HAN W, SHANKAR D, et al. Dynamics of the East India Coastal Current: 2. Numerical solutions[J]. Journal of Geophysical Research, 1996, 101(C6): 13993-14010.
[33] ZAMUDIO L, HURLBURT H E, METZGER E J, et al. Tropical wave-induced oceanic eddies at Cabo Corrientes and the María Islands, Mexico[J]. Journal of Geophysical Research, 2007, 112: C05048.
[34] UBELMANN C, FU L L. Cyclonic eddies formed at the Pacific tropical instability wave fronts[J]. Journal of Geophysical Research: Oceans, 2011, 116: C12021.
[35] POTEMRA J T, LUTHER M E, O'BRIEN J J. The seasonal circulation of the upper ocean in the Bay of Bengal[J]. Journal of Geophysical Research, 1991, 96(C7): 12667-12683.
[36] XIE Lingling, ZHENG Quan'an, ZHANG Shuwen, et al. The Rossby normal modes in the South China Sea deep basin evidenced by satellite altimetry[J]. International Journal of Remote Sensing, 2018, 39(2): 399-417.
[37] CLARKE A J, LIU X. Observations and dynamics of semiannual and annual sea levels near the Eastern Equatorial Indian Ocean boundary[J]. Journal of Physical Oceanography, 1993, 23(2): 386-399.

基金

“全球变化与海气相互作用专项”(二期)(GASI-04-WLHY-03,GASI-01-EIND-STwin);国家自然科学基金项目(41876026);自然资源部第二海洋研究所中央级公益性科研院所基本科研业务费专项资金项目(JT1704);浙江省自然科学杰出青年基金(LR16D060001)

PDF(5650 KB)

Accesses

Citation

Detail

段落导航
相关文章

/