东印度洋深层环流和水团变异研究进展*

doi:10.11978/2025034

热带海洋学报 ›› 2026, Vol. 45 ›› Issue (1): 17-26.doi: 10.11978/2025034CSTR: 32234.14.2025034

东印度洋深层环流和水团变异研究进展^*

梁湛林¹^,²(), 王卫强¹^,²()

¹热带海洋环境与岛礁生态全国重点实验室(中国科学院南海海洋研究所), 广东广州 511458
²广东省海洋遥感与大数据重点实验室(中国科学院南海海洋研究所), 广东广州 510301

收稿日期:2025-01-28 修回日期:2025-03-03 出版日期:2026-01-10 发布日期:2026-01-30
通讯作者: 王卫强
作者简介:
梁湛林(1992—), 男, 助理研究员, 从事东印度洋深层环流研究。email: liangzl@scsio.ac.cn
*本研究的数据及样品采集得到国家自然科学基金共享航次计划项目(项目批准号: 42249910、42149910)的资助, 该航次(航次编号NORC2023-10+NORC2023-303和NORC2022-10+NORC2022-303)由中国科学院南海海洋研究所“实验6”号科考船实施, 在此一并致谢。感谢美国国家海洋和大气管理局提供的WOA23 (World Ocean Atlas 2023)数据支撑, 感谢绘制地形图所使用的GMT软件(Wessel et al, 2019)
基金资助:
中国科学院海外科教合作中心部署项目(133244KYSB20200024); 国家重点研发计划项目(2022YFE0203500); 广东省科技计划项目(2022B1212050003); 中国科学院国际伙伴计划项目(059GJHZ2023104MI); 中国科学院南海海洋研究所自主部署项目(SCSIO202201); 中国科学院南海海洋研究所自主部署项目(SCSIO2023HC07); 国家自然科学基金共享航次计划项目(42249910); 国家自然科学基金共享航次计划项目(42149910)

Research progress on the characteristics of deep-sea circulation and water masses in the deep Eastern Indian Ocean^*

LIANG Zhanlin¹^,²(), WANG Weiqiang¹^,²()

¹State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 511458, China
²Guangdong Key Lab of Ocean Remote Sensing and Big Data (LORS), South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China

Received:2025-01-28 Revised:2025-03-03 Online:2026-01-10 Published:2026-01-30
Contact: WANG Weiqiang
Supported by:
Project Deployment for the Overseas Science and Education Cooperation Center of the Chinese Academy of Sciences(133244KYSB20200024); National Key Research and Development Program of China(2022YFE0203500); Science and Technology Planning Project of Guangdong Province, China(2022B1212050003); International Partnership Program of Chinese Academy of Sciences(059GJHZ2023104MI); Development Fund of South China Sea Institute of Oceanology of the Chinese Academy of Sciences(SCSIO202201); Development Fund of South China Sea Institute of Oceanology of the Chinese Academy of Sciences(SCSIO2023HC07); Shiptime Sharing Project of National Natural Science Foundation of China (NSFC)(42249910); Shiptime Sharing Project of National Natural Science Foundation of China (NSFC)(42149910)

摘要/Abstract

摘要：

东印度洋深海是全球深海系统的重要组成部分, 在全球碳循环、热量分配和营养物质运输中具有重要作用。东印度洋深海被90°E海岭分成中印度洋海盆和西澳大利亚海盆, 两个海盆间的水团特性和环流具有显著差异。为了进一步深入理解东印度洋的深海环流及水团特征, 本文通过回顾现有的研究成果, 总结和阐述了: 1)东印度洋深海地形的特殊性; 2)深海水团的来源和路径; 3)深层经向翻转环流; 4)中印度洋海盆和西澳大利亚海盆之间深层水的差异和联系。最后, 本文提出了未来东印度洋深海研究中需要重点关注的科学问题, 旨在为该领域的进一步研究提供参考。

关键词: 东印度洋, 深海, 环流, 水团

Abstract:

The deep water of the Eastern Indian Ocean is a crucial component of the global deep-sea system, playing a significant role in the global carbon cycle and the distribution of heat and nutrients. It is divided by the Ninety East Ridge into the Central Indian Basin (CIB) and the West Australian Basin (WAB). These two basins exhibit distinct differences in their water mass characteristics and circulation patterns. To further understand the deep-sea circulation and water mass features in the Eastern Indian Ocean, this paper reviews existing research findings and summarizes the following aspects: 1) the unique topography of the deep Eastern Indian Ocean; 2) the sources and pathways of deep-sea water masses; 3) the deep meridional overturning circulation; and 4) the differences and connections between the deep-sea water masses in the CIB and the WAB. Finally, this paper highlights key scientific issues that need to be addressed in future research on the deep sea of the Eastern Indian Ocean, providing a reference for related studies.

Key words: Eastern Indian Ocean, deep sea, circulation, water masses

中图分类号:

P731.27

梁湛林, 王卫强. 东印度洋深层环流和水团变异研究进展^*[J]. 热带海洋学报, 2026, 45(1): 17-26.

LIANG Zhanlin, WANG Weiqiang. Research progress on the characteristics of deep-sea circulation and water masses in the deep Eastern Indian Ocean^*[J]. Journal of Tropical Oceanography, 2026, 45(1): 17-26.

图/表 5

图1

图2

图3

图4

图5

参考文献 74

[1]	黄旭媚, 王卫强, 刘海龙, 2016. 基于多套数据的印度洋深层经向翻转环流的动力特征[J]. 热带海洋学报, 35(4): 11-20. doi: 10.11978/2015126
	HUANG XUMEI, WANG WEIQIANG, LIU HAILONG, 2016. The dynamic characteristics of deep meridional overturning circulation in the Indian Ocean based on six reanalysis datasets[J]. Journal of Tropical Oceanography, 35(4): 11-20 (in Chinese with English abstract). doi: 10.11978/2015126
[2]	朱佳豪, 裴彦良, 支鹏遥, 等, 2024. 东印度洋东经90°海岭的地球物理特征和成因探讨[J]. 海洋科学进展, 42(3): 515-531.
	ZHU JIAHAO, PEI YANLIANG, ZHI PENGYAO, et al, 2024. Geophysical characteristics and genesis of the Ninetyeast Ridge in the eastern Indian Ocean[J]. Advances in Marine Science, 42(3): 515-531 (in Chinese with English abstract).
[3]	ADERHOLD K, ABERCROMBIE R E, 2016. Seismotectonics of a diffuse plate boundary: Observations off the Sumatra-Andaman trench[J]. Journal of Geophysical Research: Solid Earth, 121(5): 3462-3478. doi: 10.1002/jgrb.v121.5
[4]	BINDOFF N L, ROSENBERG M A, WARNER M J, 2000. On the circulation and water masses over the Antarctic continental slope and rise between 80 and 150°E[J]. Deep Sea Research Part II: Topical Studies in Oceanography, 47(12-13): 2299-2326. doi: 10.1016/S0967-0645(00)00038-2
[5]	BOWIN C, 1973. Origin of the Ninety East Ridge from studies near the equator[J]. Journal of Geophysical Research (1896-1977), 78(26): 6029-6043. doi: 10.1029/JB078i026p06029
[6]	CARPENTER G, EWING J, 1973. Crustal deformation in the Wharton Basin[J]. Journal of Geophysical Research (1896-1977), 78(5): 846-850. doi: 10.1029/JB078i005p00846
[7]	CHENG LIJING, TRENBERTH K E, FASULLO J, et al, 2017. Improved estimates of ocean heat content from 1960 to 2015[J]. Science Advances, 3(3): e1601545.
[8]	CLOWES A J, DEACON G E R, 1935. The deep-water circulation of the Indian ocean[J]. Nature, 136(3450): 936-938. doi: 10.1038/136936a0
[9]	DONOHUE K A, HUFFORD G E, MCCARTNEY M S, 1999. Sources and transport of the deep western boundary current east of the Kerguelen Plateau[J]. Geophysical Research Letters, 26(7): 851-854. doi: 10.1029/1999GL900099
[10]	DRIJFHOUT S S, GARABATO A C N, 2008. The zonal dimension of the Indian ocean meridional overturning circulation[J]. Journal of Physical Oceanography, 38(2): 359-379. doi: 10.1175/2007JPO3640.1
[11]	FISCHER R L, JANTSCH M Z, COMER R L, 1982. General bathymetric chart of the oceans (GEBCO), map 5. 09[Z]. Ottawa: Canadian Hydrographic Service.
[12]	FREY F A, PRINGLE M, MELENEY P, et al, 2011. Diverse mantle sources for Ninetyeast Ridge magmatism: Geochemical constraints from basaltic glasses[J]. Earth and Planetary Science Letters, 303(3-4): 215-224. doi: 10.1016/j.epsl.2010.12.051
[13]	FREY F A, WEIS D, 1995. Temporal evolution of the Kerguelen plume: Geochemical evidence from 38 to 82 ma lavas forming the Ninetyeast ridge[J]. Contributions to Mineralogy and Petrology, 121(1): 12-28. doi: 10.1007/s004100050087
[14]	FUKAMACHI Y, RINTOUL S R, CHURCH J A, et al, 2010. Strong export of Antarctic Bottom Water east of the Kerguelen plateau[J]. Nature Geoscience, 3(5): 327-331. doi: 10.1038/ngeo842
[15]	GANACHAUD A, WUNSCH C, MAROTZKE J, et al, 2000. Meridional overturning and large-scale circulation of the Indian Ocean[J]. Journal of Geophysical Research: Oceans, 105(C11): 26117-26134.
[16]	GUNN K L, RINTOUL S R, ENGLAND M H, et al, 2023. Recent reduced abyssal overturning and ventilation in the Australian Antarctic Basin[J]. Nature Climate Change, 13(6): 537-544. doi: 10.1038/s41558-023-01667-8
[17]	HERNÁNDEZ-GUERRA A, TALLEY L D, 2016. Meridional overturning transports at 30°S in the Indian and Pacific Oceans in 2002-2003 and 2009[J]. Progress in Oceanography, 146: 89-120. doi: 10.1016/j.pocean.2016.06.005
[18]	HUFFORD G E, MCCARTNEY M S, DONOHUE K A, 1997. Northern boundary currents and adjacent recirculations off southwestern Australia[J]. Geophysical Research Letters, 24(22): 2797-2800. doi: 10.1029/97GL02278
[19]	JOHNSON G C, 2008. Quantifying Antarctic bottom water and north Atlantic deep water volumes[J]. Journal of Geophysical Research: Oceans, 113(C5): 2007JC004477.
[20]	JOHNSON G C, SLOYAN B M, KESSLER W S, et al, 2002. Direct measurements of upper ocean currents and water properties across the tropical Pacific during the 1990s[J]. Progress in Oceanography, 52(1): 31-61. doi: 10.1016/S0079-6611(02)00021-6
[21]	KOUKETSU S, DOI T, KAWANO T, et al, 2011. Deep ocean heat content changes estimated from observation and reanalysis product and their influence on sea level change[J]. Journal of Geophysical Research: Oceans, 116(C3): C03012.
[22]	KRISHNA K S, ABRAHAM H, SAGER W W, et al, 2012. Tectonics of the Ninetyeast Ridge derived from spreading records in adjacent oceanic basins and age constraints of the ridge[J]. Journal of Geophysical Research: Solid Earth, 117(B4): 2011JB008805.
[23]	LAGERLOEF G S E, MITCHUM G T, LUKAS R B, et al, 1999. Tropical Pacific near-surface currents estimated from altimeter, wind, and drifter data[J]. Journal of Geophysical Research: Oceans, 104(C10): 23313-23326.
[24]	LEE TONG, MAROTZKE J, 1998. Seasonal cycles of meridional overturning and heat transport of the Indian ocean[J]. Journal of Physical Oceanography, 28(5): 923-943. doi: 10.1175/1520-0485(1998)028<0923:SCOMOA>2.0.CO;2
[25]	LEMENKOVA P, 2021. Exploring structured scripting cartographic technique of GMT for ocean seafloor modeling: A case of the East Indian Ocean[J]. Maritime Technology and Research, 3(2): 162-184. doi: 10.33175/mtr.2021.248158
[26]	LEVCHENKO O V, SBORSHCHIKOV I M, MARINOVA Y G, 2014. Tectonics of the Ninety-East Ridge[J]. Oceanology, 54(2): 231-244. doi: 10.1134/S0001437014020143
[27]	LEVIN L A, LE BRIS N, 2015. The deep ocean under climate change[J]. Science, 350(6262): 766-768. doi: 10.1126/science.aad0126
[28]	LUDDEN J N, THOMPSON G, BRYAN W B, et al, 1980. The origin of lavas from the Ninetyeast Ridge, eastern Indian Ocean: an evaluation of fractional crystallization models[J]. Journal of Geophysical Research: Solid Earth, 85(B8): 4405-4420.
[29]	LUMPKIN R, SPEER K, 2007. Global ocean meridional overturning[J]. Journal of Physical Oceanography, 37(10): 2550-2562. doi: 10.1175/JPO3130.1
[30]	MACDONALD A M, 1998. The global ocean circulation: a hydrographic estimate and regional analysis[J]. Progress in Oceanography, 41(3): 281-382. doi: 10.1016/S0079-6611(98)00020-2
[31]	MANTYLA A W, REID J L, 1995. On the origins of deep and bottom waters of the Indian Ocean[J]. Journal of Geophysical Research: Oceans, 100(C2): 2417-2439.
[32]	MCCARTNEY M S, DONOHUE K A, 2007. A deep cyclonic gyre in the Australian-Antarctic Basin[J]. Progress in Oceanography, 75(4): 675-750. doi: 10.1016/j.pocean.2007.02.008
[33]	MCDONAGH E L, BRYDEN H L, KING B A, et al, 2008. The circulation of the Indian Ocean at 32°S[J]. Progress in Oceanography, 79(1): 20-36. doi: 10.1016/j.pocean.2008.07.001
[34]	MICHAEL L, KRISHNA K S, 2011. Dating of the 85°E Ridge (northeastern Indian Ocean) using marine magnetic anomalies[J]. Current Science, 100(9): 1314-1322.
[35]	ORSI A H, JOHNSON G C, BULLISTER J L, 1999. Circulation, mixing, and production of Antarctic bottom water[J]. Progress in Oceanography, 43(1): 55-109. doi: 10.1016/S0079-6611(99)00004-X
[36]	ORSI A H, WHITWORTH T, NOWLIN W D, 1995. On the meridional extent and fronts of the Antarctic Circumpolar Current[J]. Deep Sea Research Part I: Oceanographic Research Papers, 42(5): 641-673. doi: 10.1016/0967-0637(95)00021-W
[37]	PALMER J, SEMPÉRÉ J C, CHRISTIE D M, et al, 1993. Morphology and tectonics of the Australian-Antarctic discordance between 123° E and 128° E[J]. Marine Geophysical Researches, 15(2): 121-152. doi: 10.1007/BF01204132
[38]	PARK Y H, CHARRIAUD E, FIEUX M, 1998. Thermohaline structure of the Antarctic surface water/winter water in the Indian sector of the Southern Ocean[J]. Journal of Marine Systems, 17(1-4): 5-23. doi: 10.1016/S0924-7963(98)00026-8
[39]	PURKEY S G, JOHNSON G C, 2012. Global contraction of Antarctic bottom water between the 1980s and 2000s[J]. Journal of Climate, 25(17): 5830-5844. doi: 10.1175/JCLI-D-11-00612.1
[40]	REID J L, 2003. On the total geostrophic circulation of the Indian Ocean: flow patterns, tracers, and transports[J]. Progress in Oceanography, 56(1): 137-186. doi: 10.1016/S0079-6611(02)00141-6
[41]	ROBBINS P E, TOOLE J M, 1997. The dissolved silica budget as a constraint on the meridional overturning circulation of the Indian Ocean[J]. Deep Sea Research Part I: Oceanographic Research Papers, 44(5): 879-906. doi: 10.1016/S0967-0637(96)00126-4
[42]	RODMAN M R, GORDON A L, 1982. Southern Ocean bottom water of the Australian-New Zealand sector[J]. Journal of Geophysical Research: Oceans, 87(C8): 5771-5778.
[43]	SCHMITZ JR W J, 1995. On the interbasin-scale thermohaline circulation[J]. Reviews of Geophysics, 33(2): 151-173. doi: 10.1029/95RG00879
[44]	SCHMITZ W J, 1996. On the world ocean circulation. Volume Ⅱ, the Pacific and Indian Oceans / a global update[R]. Woods Hole: Woods Hole Oceanographic Institution.
[45]	SCHOTT F A, MCCREARY J P, 2001. The monsoon circulation of the Indian ocean[J]. Progress in Oceanography, 51(1): 1-123. doi: 10.1016/S0079-6611(01)00083-0
[46]	SILVA I G N, WEIS D, SCOATES J S, et al, 2013. The Ninetyeast Ridge and its relation to the Kerguelen, Amsterdam and St. Paul Hotspots in the Indian Ocean[J]. Journal of Petrology, 54(6): 1177-1210. doi: 10.1093/petrology/egt009
[47]	SILVANO A, PURKEY S, GORDON A L, et al, 2023. Observing Antarctic bottom water in the Southern Ocean[J]. Frontiers in Marine Science, 10: 1221701. doi: 10.3389/fmars.2023.1221701
[48]	SLOYAN B M, 2006. Antarctic bottom and lower circumpolar deep water circulation in the eastern Indian Ocean[J]. Journal of Geophysical Research: Oceans, 111(C2): 2005JC003011.
[49]	SLOYAN B M, RINTOUL S R, 2001. The Southern Ocean limb of the global deep overturning circulation[J]. Journal of Physical Oceanography, 31(1): 143-173. doi: 10.1175/1520-0485(2001)031<0143:TSOLOT>2.0.CO;2
[50]	SMITH W H F, SANDWELL D T, 1997. Global sea floor topography from satellite altimetry and ship depth soundings[J]. Science, 277(5334): 1956-1962. doi: 10.1126/science.277.5334.1956
[51]	SOLODOCH A, STEWART A L, HOGG A M, et al, 2022. How does Antarctic bottom water cross the Southern Ocean?[J]. Geophysical Research Letters, 49(7): e2021GL097211.
[52]	SPEICH S, BLANKE B, MADEC G, 2001. Warm and cold water routes of an O. G. C. M. thermohaline conveyor belt[J]. Geophysical Research Letters, 28(2): 311-314. doi: 10.1029/2000GL011748
[53]	SRINIVASAN A, GARRAFFO Z, ISKANDARANI M, 2009. Abyssal circulation in the Indian Ocean from a 1/12° degrees resolution global hindcast[J]. Deep-Sea Research Part I: Oceanographic Research Papers, 56(11): 1907-1926. doi: 10.1016/j.dsr.2009.07.001
[54]	STEVENS D E, MCNEILL L C, HENSTOCK T J, et al, 2020. A complete structural model and kinematic history for distributed deformation in the Wharton Basin[J]. Earth and Planetary Science Letters, 538: 116218. doi: 10.1016/j.epsl.2020.116218
[55]	STEWART H A, JAMIESON A J, 2019. The five deeps: The location and depth of the deepest place in each of the world’s oceans[J]. Earth-Science Reviews, 197: 102896. doi: 10.1016/j.earscirev.2019.102896
[56]	STOMMEL H, 1958. The abyssal circulation[J]. Deep Sea Research (1953), 5(1): 80-82. doi: 10.1016/S0146-6291(58)80014-4
[57]	STRAMMA L, SCHMIDTKO S, LEVIN L A, et al, 2010. Ocean oxygen minima expansions and their biological impacts[J]. Deep Sea Research Part I: Oceanographic Research Papers, 57(4): 587-595. doi: 10.1016/j.dsr.2010.01.005
[58]	SUDRE J, MORROW R A, 2008. Global surface currents: a high-resolution product for investigating ocean dynamics[J]. Ocean Dynamics, 58(2): 101-118. doi: 10.1007/s10236-008-0134-9
[59]	TALLEY L D, PICKARD G L, EMERY W J, et al, 2011. Descriptive Physical Oceanography (Sixth Edition)[M]. Boston: Academic Press.
[60]	TALLEY L D, BARINGER M O, 1997. Preliminary results from WOCE hydrographic sections at 80°E and 32°S in the central Indian Ocean[J]. Geophysical Research Letters, 24(22): 2789-2792. doi: 10.1029/97GL02657
[61]	TAMSITT V, TALLEY L D, MAZLOFF M R, 2019. A deep eastern boundary current carrying Indian deep water south of Australia[J]. Journal of Geophysical Research: Oceans, 124(3): 2218-2238. doi: 10.1029/2018JC014569
[62]	TOGGWEILER J R, SAMUELS B, 1995. Effect of drake passage on the global thermohaline circulation[J]. Deep Sea Research Part I: Oceanographic Research Papers, 42(4): 477-500. doi: 10.1016/0967-0637(95)00012-U
[63]	TOOLE J M, WARREN B A, 1993. A hydrographic section across the subtropical South Indian Ocean[J]. Deep Sea Research Part I: Oceanographic Research Papers, 40(10): 1973-2019. doi: 10.1016/0967-0637(93)90042-2
[64]	WANG JINGHONG, SHU YEQIANG, WANG DONGXIAO, et al, 2024. Observed 10-20-day deep-current variability at 5°N, 90.5°E in the eastern Indian ocean[J]. Journal of Physical Oceanography, 54(2): 521-536. doi: 10.1175/JPO-D-23-0082.1
[65]	WANG WEIQIANG, KÖHL A, STAMMER D, 2012. The deep meridional overturning circulation in the Indian Ocean inferred from the GECCO synthesis[J]. Dynamics of Atmospheres and Oceans, 58: 44-61. doi: 10.1016/j.dynatmoce.2012.08.001
[66]	WANG WEIQIANG, ZHU XIUHUA, WANG CHUNZAI, et al, 2014. Deep meridional overturning circulation in the Indian Ocean and its relation to Indian Ocean Dipole[J]. Journal of Climate, 27(12): 4508-4520. doi: 10.1175/JCLI-D-13-00472.1
[67]	WARREN B A, 1977. Deep Western boundary current in the eastern Indian ocean[J]. Science, 196(4285): 53-54. pmid: 17733523
[68]	WARREN B A, 1982. The deep water of the Central Indian Basin[J]. Journal of Marine Research, 40: 823-860.
[69]	WARREN B A, JOHNSON G C, 2002. The overflows across the Ninetyeast Ridge[J]. Deep Sea Research Part II: Topical Studies in Oceanography, 49(7-8): 1423-1439. doi: 10.1016/S0967-0645(01)00156-4
[70]	WESSEL P, LUIS J F, UIEDA L, et al, 2019. The generic mapping tools version 6[J]. Geochemistry, Geophysics, Geosystems, 20(11): 5556-5564. doi: 10.1029/2019GC008515
[71]	WILLIAMS G D, AOKI S, JACOBS S S, et al, 2010. Antarctic bottom water from the Adélie and George V land coast, east Antarctica (140-149°E)[J]. Journal of Geophysical Research: Oceans, 115(C4): 2009JC005812.
[72]	YE RUIJIE, ZHOU FENG, MA XIAO, et al, 2023. Energetic bottom current at the equatorial gap of the Ninety East Ridge in the Indian Ocean based on mooring data[J]. Journal of Geophysical Research: Oceans, 128(3): e2022JC018974.
[73]	YOU YUZHU, 2000. Implications of the deep circulation and ventilation of the Indian Ocean on the renewal mechanism of North Atlantic Deep Water[J]. Journal of Geophysical Research: Oceans, 105(C10): 23895-23926.
[74]	ZIKA J D, LALIBERTÉ F, MUDRYK L R, et al, 2015. Changes in ocean vertical heat transport with global warming[J]. Geophysical Research Letters, 42(12): 4940-4948. doi: 10.1002/grl.v42.12

东印度洋深层环流和水团变异研究进展^*

Research progress on the characteristics of deep-sea circulation and water masses in the deep Eastern Indian Ocean^*

RichHTML

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

图/表 5

参考文献 74

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	吴兰军, 黎刚, 杨梦林. 西亚干旱区全新世水文气候研究进展[J]. 热带海洋学报, 2026, 45(1): 3-16.
[2]	钟卿文, 陈更新, 陈举, 何云开. 印度洋赤道深层流的季节内变化特征及其驱动机制^*[J]. 热带海洋学报, 2026, 45(1): 140-153.
[3]	庞小艳, 李晓琳, 王俊锋, 田新朋, 徐石海, 刘永宏. 印度洋深海来源真菌Penicillium sp. SCSIO 06871次级代谢产物研究[J]. 热带海洋学报, 2024, 43(6): 190-195.
[4]	李黛, 王旭东, 贾子策, 冯东. 深海极端环境黑碳的地球化学特征及其环境意义^*[J]. 热带海洋学报, 2024, 43(4): 20-32.
[5]	曾步燕, 梁志凤, 罗琴琴, 曾玲, 杨长庚, 王锂韫, 孙玉林. 深海真菌101#的分子鉴定、次生代谢产物及其生物活性研究^*[J]. 热带海洋学报, 2023, 42(5): 104-114.
[6]	宋永相, 李晓悦, 鞠建华. 深海放线菌Streptomyces koyangensis SCSIO 5802中次级代谢产物neoabyssomicin H的分离鉴定^*[J]. 热带海洋学报, 2023, 42(3): 169-173.
[7]	李若飞, 柯志新, 李开枝, 刘甲星, 谭烨辉. 基于ZooScan图像分析“海马”冷泉区浮游动物垂直分布特征[J]. 热带海洋学报, 2023, 42(2): 87-96.
[8]	张金尚, 邹定辉, 马玉, 李锐祥, 刘愉强, 孟强, 刘同木, 史华明. 南海北部水团及中尺度现象对营养盐时空分布的影响^*[J]. 热带海洋学报, 2023, 42(1): 168-181.
[9]	唐娇雨, 王卫强, 徐康, 张镇秋. 赤道东印度洋次表层高盐水的年际变化^*[J]. 热带海洋学报, 2023, 42(1): 10-21.
[10]	丛梦静, 胡怡伟, 赵凯, 张晓勇, 刘永宏, 王俊锋. 深海冷泉来源真菌Talaromyces helicus SCSIO41311中聚酮类化学成分研究[J]. 热带海洋学报, 2022, 41(5): 117-120.
[11]	王俊锋, 周雯颖, 田新朋, 刘永宏. 深海热液真菌Fusarium sp. SCSIO 06196中抗病毒聚酮类化学成分研究[J]. 热带海洋学报, 2022, 41(5): 189-193.
[12]	尹健强, 李开枝, 谭烨辉. 南海南部海域浮游介形类新种——南沙深海浮萤*[J]. 热带海洋学报, 2022, 41(2): 193-197.
[13]	王雪松, 陈忠, 许安涛, 田雨杭, 曹立, 张斌. 南海东北部深海盆末次冰盛期以来陆源碎屑粒度特征及影响因素^*[J]. 热带海洋学报, 2022, 41(1): 158-170.
[14]	何子康, 王喜冬, 陈志强, 范开桂. 利用海洋温度剖面与海表盐度反演盐度剖面方法研究[J]. 热带海洋学报, 2021, 40(6): 41-51.
[15]	杜岩, 陈举, 经志友, 王祥鹏, 陈更新, 徐驰, 储小青, 陈植武, 徐杰, 施震, 唐世林, 何云开, 梁韵, 施平. 南海开放共享航次关键科学问题的思考——从多尺度海洋动力学角度出发[J]. 热带海洋学报, 2020, 39(6): 1-17.

东印度洋深层环流和水团变异研究进展*

Research progress on the characteristics of deep-sea circulation and water masses in the deep Eastern Indian Ocean*

RichHTML

PDF (PC)

赞

可视化

摘要/Abstract

引用本文

使用本文

图/表 5

参考文献 74

相关文章 15

Metrics

本文评价

推荐阅读 0

东印度洋深层环流和水团变异研究进展^*

Research progress on the characteristics of deep-sea circulation and water masses in the deep Eastern Indian Ocean^*