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Journal articles on the topic 'Indian Ocean'

Author: Grafiati

Published: 4 June 2021

Last updated: 31 July 2024

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1

Van der Land, J., Barbara Kwiatkowska, Jan H. Stel, Pervez Ahmed Butt, and S. H. Niaz Rizvi. "Indian Ocean." International Journal of Marine and Coastal Law 8, no. 1 (1993): 164–67. http://dx.doi.org/10.1163/157180893x00279.

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2

Jin, Xiaolin, Young-Oh Kwon, Caroline C. Ummenhofer, Hyodae Seo, Franziska U. Schwarzkopf, Arne Biastoch, Claus W. Böning, and Jonathon S. Wright. "Influences of Pacific Climate Variability on Decadal Subsurface Ocean Heat Content Variations in the Indian Ocean." Journal of Climate 31, no. 10 (April 30, 2018): 4157–74. http://dx.doi.org/10.1175/jcli-d-17-0654.1.

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Abstract Decadal variabilities in Indian Ocean subsurface ocean heat content (OHC; 50–300 m) since the 1950s are examined using ocean reanalyses. This study elaborates on how Pacific variability modulates the Indian Ocean on decadal time scales through both oceanic and atmospheric pathways. High correlations between OHC and thermocline depth variations across the entire Indian Ocean Basin suggest that OHC variability is primarily driven by thermocline fluctuations. The spatial pattern of the leading mode of decadal Indian Ocean OHC variability closely matches the regression pattern of OHC on the interdecadal Pacific oscillation (IPO), emphasizing the role of the Pacific Ocean in determining Indian Ocean OHC decadal variability. Further analyses identify different mechanisms by which the Pacific influences the eastern and western Indian Ocean. IPO-related anomalies from the Pacific propagate mainly through oceanic pathways in the Maritime Continent to impact the eastern Indian Ocean. By contrast, in the western Indian Ocean, the IPO induces wind-driven Ekman pumping in the central Indian Ocean via the atmospheric bridge, which in turn modifies conditions in the southwestern Indian Ocean via westward-propagating Rossby waves. To confirm this, a linear Rossby wave model is forced with wind stresses and eastern boundary conditions based on reanalyses. This linear model skillfully reproduces observed sea surface height anomalies and highlights both the oceanic connection in the eastern Indian Ocean and the role of wind-driven Ekman pumping in the west. These findings are also reproduced by OGCM hindcast experiments forced by interannual atmospheric boundary conditions applied only over the Pacific and Indian Oceans, respectively.

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3

Kajtar, Jules B., Agus Santoso, Matthew H. England, and Wenju Cai. "Indo-Pacific Climate Interactions in the Absence of an Indonesian Throughflow." Journal of Climate 28, no. 13 (July 1, 2015): 5017–29. http://dx.doi.org/10.1175/jcli-d-14-00114.1.

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Abstract The Pacific and Indian Oceans are connected by an oceanic passage called the Indonesian Throughflow (ITF). In this setting, modes of climate variability over the two oceanic basins interact. El Niño–Southern Oscillation (ENSO) events generate sea surface temperature anomalies (SSTAs) over the Indian Ocean that, in turn, influence ENSO evolution. This raises the question as to whether Indo-Pacific feedback interactions would still occur in a climate system without an Indonesian Throughflow. This issue is investigated here for the first time using a coupled climate model with a blocked Indonesian gateway and a series of partially decoupled experiments in which air–sea interactions over each ocean basin are in turn suppressed. Closing the Indonesian Throughflow significantly alters the mean climate state over the Pacific and Indian Oceans. The Pacific Ocean retains an ENSO-like variability, but it is shifted eastward. In contrast, the Indian Ocean dipole and the Indian Ocean basinwide mode both collapse into a single dominant and drastically transformed mode. While the relationship between ENSO and the altered Indian Ocean mode is weaker than that when the ITF is open, the decoupled experiments reveal a damping effect exerted between the two modes. Despite the weaker Indian Ocean SSTAs and the increased distance between these and the core of ENSO SSTAs, the interbasin interactions remain. This suggests that the atmospheric bridge is a robust element of the Indo-Pacific climate system, linking the Indian and Pacific Oceans even in the absence of an Indonesian Throughflow.

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4

Ming, Wan. "Zheng He’s Seven Voyages into the Namoli Ocean–the Indian Ocean." China and Asia 1, no. 1 (February 11, 2019): 92–125. http://dx.doi.org/10.1163/2589465x-00101004.

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In the history of the development of human civilization, the Silk Road has been an important route of traffic and exchange between the East and the West. From Zhang Qian’s 張騫 opening up of the Silk Road across the Western Regions (Xiyue 西域) to Zheng He’s 鄭和 sailing to the Western Oceans (xia xiyang 下西洋) more than 1500 years later, China had a continuous desire to explore beyond its borders. At the time of Zheng He, the term “Western Oceans” (xiyang 西洋) had a specific meaning. As shown by the account of Ma Huan 馬歡, who personally joined Zheng He on the voyages, the people of Ming China considered the “Western Oceans” to be the Namoli Ocean (Namoli yang 那没黎洋), later called the Indian Ocean. Thus, it could be concluded that the Western Oceans where Zheng He’s fleet went meant the Indian Ocean. Even today most scholars still divide the Eastern and Western Oceans at Brunei, with no clear understanding of where the Western Oceans to which Zheng He sailed were actually located. It is therefore important to make clear that the Western Oceans in his time referred to the Indian Ocean, before moving on to investigate the purpose of the voyages and related historical issues. Even more important is to point out that Zheng He’s expeditions in the early fifteenth century reflected that Chinese people took to the seas on a scale larger than ever before and joined the maritime and overland silk routes together. The place where this occurred was the Indian Ocean.

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5

Han, Weiqing, Jérôme Vialard, Michael J. McPhaden, Tong Lee, Yukio Masumoto, Ming Feng, and Will P. M. de Ruijter. "Indian Ocean Decadal Variability: A Review." Bulletin of the American Meteorological Society 95, no. 11 (November 1, 2014): 1679–703. http://dx.doi.org/10.1175/bams-d-13-00028.1.

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The international scientific community has highlighted decadal and multidecadal climate variability as a priority area for climate research. The Indian Ocean rim region is home to one-third of the world's population, mostly living in developing countries that are vulnerable to climate variability and to the increasing pressure of anthropogenic climate change. Yet, while prominent decadal and multidecadal variations occur in the Indian Ocean, they have been less studied than those in the Pacific and Atlantic Oceans. This paper reviews existing literature on these Indian Ocean variations, including observational evidence, physical mechanisms, and climatic impacts. This paper also identifies major issues and challenges for future Indian Ocean research on decadal and multidecadal variability.

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6

Brown, J., C. A. Clayson, L. Kantha, and T. Rojsiraphisal. "North Indian Ocean variability during the Indian Ocean dipole." Ocean Science Discussions 5, no. 2 (June 9, 2008): 213–53. http://dx.doi.org/10.5194/osd-5-213-2008.

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Abstract. The circulation in the North Indian Ocean (NIO henceforth) is highly seasonally variable. Periodically reversing monsoon winds (southwesterly during summer and northeasterly during winter) give rise to seasonally reversing current systems off the coast of Somalia and India. In addition to this annual monsoon cycle, the NIO circulation varies semiannually because of equatorial currents reversing four times each year. These descriptions are typical, but how does the NIO circulation behave during anomalous years, during an Indian Ocean dipole (IOD) for instance? Unfortunately, in situ observational data are rather sparse and reliance has to be placed on numerical models to understand this variability. In this paper, we estimate the surface current variability from a 12-year hindcast of the NIO for 1993–2004 using a 1/2° resolution circulation model that assimilates both altimetric sea surface height anomalies and sea surface temperature. Presented in this paper is an examination of surface currents in the NIO basin during the IOD. During the non-IOD period of 2000–2004, the typical equatorial circulation of the NIO reverses four times each year and transports water across the basin preventing a large sea surface temperature difference between the western and eastern NIO. Conversely, IOD years are noted for strong easterly and westerly wind outbursts along the equator. The impact of these outbursts on the NIO circulation is to reverse the direction of the currents – when compared to non-IOD years – during the summer for negative IOD events (1996 and 1998) and during the fall for positive IOD events (1994 and 1997). This reversal of current direction leads to large temperature differences between the western and eastern NIO.

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7

Kapur, Ashok, and Robert H. Bruce. "The Modern Indian Navy and the Indian Ocean: Studies in Indian Ocean." Pacific Affairs 63, no. 3 (1990): 398. http://dx.doi.org/10.2307/2759541.

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8

Phillips, Helen E., Amit Tandon, Ryo Furue, Raleigh Hood, Caroline C. Ummenhofer, Jessica A. Benthuysen, Viviane Menezes, et al. "Progress in understanding of Indian Ocean circulation, variability, air–sea exchange, and impacts on biogeochemistry." Ocean Science 17, no. 6 (November 26, 2021): 1677–751. http://dx.doi.org/10.5194/os-17-1677-2021.

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Abstract. Over the past decade, our understanding of the Indian Ocean has advanced through concerted efforts toward measuring the ocean circulation and air–sea exchanges, detecting changes in water masses, and linking physical processes to ecologically important variables. New circulation pathways and mechanisms have been discovered that control atmospheric and oceanic mean state and variability. This review brings together new understanding of the ocean–atmosphere system in the Indian Ocean since the last comprehensive review, describing the Indian Ocean circulation patterns, air–sea interactions, and climate variability. Coordinated international focus on the Indian Ocean has motivated the application of new technologies to deliver higher-resolution observations and models of Indian Ocean processes. As a result we are discovering the importance of small-scale processes in setting the large-scale gradients and circulation, interactions between physical and biogeochemical processes, interactions between boundary currents and the interior, and interactions between the surface and the deep ocean. A newly discovered regional climate mode in the southeast Indian Ocean, the Ningaloo Niño, has instigated more regional air–sea coupling and marine heatwave research in the global oceans. In the last decade, we have seen rapid warming of the Indian Ocean overlaid with extremes in the form of marine heatwaves. These events have motivated studies that have delivered new insight into the variability in ocean heat content and exchanges in the Indian Ocean and have highlighted the critical role of the Indian Ocean as a clearing house for anthropogenic heat. This synthesis paper reviews the advances in these areas in the last decade.

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9

Watanabe, Hiromi Kayama, Chong Chen, Daniel P. Marie, Ken Takai, Katsunori Fujikura, and Benny K. K. Chan. "Phylogeography of hydrothermal vent stalked barnacles: a new species fills a gap in the Indian Ocean ‘dispersal corridor’ hypothesis." Royal Society Open Science 5, no. 4 (April 2018): 172408. http://dx.doi.org/10.1098/rsos.172408.

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Phylogeography of animals provides clues to processes governing their evolution and diversification. The Indian Ocean has been hypothesized as a ‘dispersal corridor’ connecting hydrothermal vent fauna of Atlantic and Pacific oceans. Stalked barnacles of the family Eolepadidae are common associates of deep-sea vents in Southern, Pacific and Indian oceans, and the family is an ideal group for testing this hypothesis. Here, we describe Neolepas marisindica sp. nov. from the Indian Ocean, distinguished from N. zevinae and N. rapanuii by having a tridentoid mandible in which the second tooth lacks small elongated teeth. Morphological variations suggest that environmental differences result in phenotypic plasticity in the capitulum and scales on the peduncle in eolepadids. We suggest that diagnostic characters in Eolepadidae should be based mainly on more reliable arthropodal characters and DNA barcoding, while the plate arrangement should be used carefully with their intraspecific variation in mind. We show morphologically that Neolepas specimens collected from the South West Indian Ridge, the South East Indian Ridge and the Central Indian Ridge belong to the new species. Molecular phylogeny and fossil evidence indicated that Neolepas migrated from the southern Pacific to the Indian Ocean through the Southern Ocean, providing key evidence against the ‘dispersal corridor’ hypothesis. Exploration of the South East Indian Ridge is urgently required to understand vent biogeography in the Indian Ocean.

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10

Meehl, Gerald A., Julie M. Arblaster, and Johannes Loschnigg. "Coupled Ocean–Atmosphere Dynamical Processes in the Tropical Indian and Pacific Oceans and the TBO." Journal of Climate 16, no. 13 (July 1, 2003): 2138–58. http://dx.doi.org/10.1175/2767.1.

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Abstract The transitions (from relatively strong to relatively weak monsoon) in the tropospheric biennial oscillation (TBO) occur in northern spring for the south Asian or Indian monsoon and northern fall for the Australian monsoon involving coupled land–atmosphere–ocean processes over a large area of the Indo-Pacific region. Transitions from March–May (MAM) to June–September (JJAS) tend to set the system for the next year, with a transition to the opposite sign the following year. Previous analyses of observed data and GCM sensitivity experiments have demonstrated that the TBO (with roughly a 2–3-yr period) encompasses most ENSO years (with their well-known biennial tendency). In addition, there are other years, including many Indian Ocean dipole (or zonal mode) events, that contribute to biennial transitions. Results presented here from observations for composites of TBO evolution confirm earlier results that the Indian and Pacific SST forcings are more dominant in the TBO than circulation and meridional temperature gradient anomalies over Asia. A fundamental element of the TBO is the large-scale east–west atmospheric circulation (the Walker circulation) that links anomalous convection and precipitation, winds, and ocean dynamics across the Indian and Pacific sectors. This circulation connects convection over the Asian–Australian monsoon regions both to the central and eastern Pacific (the eastern Walker cell), and to the central and western Indian Ocean (the western Walker cell). Analyses of upper-ocean data confirm previous results and show that ENSO El Niño and La Niña events as well as Indian Ocean SST dipole (or zonal mode) events are often large-amplitude excursions of the TBO in the tropical Pacific and Indian Oceans, respectively, associated with anomalous eastern and western Walker cell circulations, coupled ocean dynamics, and upper-ocean temperature and heat content anomalies. Other years with similar but lower-amplitude signals in the tropical Pacific and Indian Oceans also contribute to the TBO. Observed upper-ocean data for the Indian Ocean show that slowly eastward-propagating equatorial ocean heat content anomalies, westward-propagating ocean Rossby waves south of the equator, and anomalous cross-equatorial ocean heat transports contribute to the heat content anomalies in the Indian Ocean and thus to the ocean memory and consequent SST anomalies, which are an essential part of the TBO.

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11

Sreeja, K. "Blue Ocean Strategies and Indian Companies." Asian Review of Social Sciences 9, no. 1 (May 5, 2020): 23–26. http://dx.doi.org/10.51983/arss-2020.9.1.1611.

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The Blue Ocean Strategy is relatively a new concept propounded by Kim and Mauborgne in 2005 in their famous book “Blue Ocean Strategy: How to Create Uncontested Market Space and Make the Competition Irrelevant”. Blue oceans are the unexplored market space where no competition exists at present. This is a concept paper based on content exploration and no scientific enquiry is carried out as part of this study. The present paper explains the concept of Blue Ocean Strategy by illustrating the examples of some companies using this strategy

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12

McDougall, Derek. "Indian ocean regionalism." Journal of the Indian Ocean Region 12, no. 1 (August 4, 2015): 115–16. http://dx.doi.org/10.1080/19480881.2015.1065568.

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13

Robert Ray, Senator. "Indian Ocean Security." Maritime Studies 1990, no. 53 (July 1990): 10–13. http://dx.doi.org/10.1080/07266472.1990.10878243.

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14

Gray, Stephen. "Indian Ocean Islands." Wasafiri 7, no. 14 (September 1991): 23–27. http://dx.doi.org/10.1080/02690059108574249.

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15

McDougall, Derek. "Indian ocean regionalism." Round Table 86, no. 341 (January 1997): 53–66. http://dx.doi.org/10.1080/00358539708454344.

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16

"Indian ocean." Choice Reviews Online 26, no. 04 (December 1, 1988): 26–1903. http://dx.doi.org/10.5860/choice.26-1903.

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17

Rodrigo, Dhanushka. "Indian Ocean Geopolitics." SSRN Electronic Journal, 2021. http://dx.doi.org/10.2139/ssrn.3783748.

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18

"Indian Ocean Islands." International African Bibliography 45, no. 1-2 (July 1, 2015): 99–100. http://dx.doi.org/10.1515/iab-2015-0008.

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19

"Indian Ocean Islands." International African Bibliography 44, no. 1-2 (June 1, 2014): 93–94. http://dx.doi.org/10.1515/iab.2014.008.

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20

"Indian Ocean Islands." International African Bibliography 44, no. 3-4 (December 19, 2014): 223–25. http://dx.doi.org/10.1515/iab.2014.018.

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21

"INDIAN OCEAN ISLANDS." International African Bibliography 41, no. 4 (February 2012): 263. http://dx.doi.org/10.1515/iab-2011-0028.

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22

"Indian Ocean Islands." iabi 42, no. 3-4 (December 2012): 229–31. http://dx.doi.org/10.1515/iab-2012-0018.

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23

"Indian Ocean Islands." iabi 43, no. 1-2 (June 2013): 122–23. http://dx.doi.org/10.1515/iab-2013-0008.

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24

"Indian Ocean Islands." iabi 42, no. 1-2 (December 2012): 100–101. http://dx.doi.org/10.1515/iab-2012-0008.

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25

"Indian Ocean Islands." iabi 43, no. 3-4 (December 2013): 115–16. http://dx.doi.org/10.1515/iab.2013.018.

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26

"FISH: Indian Ocean." Africa Research Bulletin: Economic, Financial and Technical Series 45, no. 6 (August 2008): 17896A—17897B. http://dx.doi.org/10.1111/j.1467-6346.2008.01803.x.

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27

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 20, no. 1 (1990). http://dx.doi.org/10.1515/iabi.1990.20.1.51.

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28

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 20, no. 2 (1990). http://dx.doi.org/10.1515/iabi.1990.20.2.122.

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29

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 20, no. 3 (1990). http://dx.doi.org/10.1515/iabi.1990.20.3.194.

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30

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 20, no. 4 (1990). http://dx.doi.org/10.1515/iabi.1990.20.4.267.

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31

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 21, no. 1 (1991). http://dx.doi.org/10.1515/iabi.1991.21.1.44.

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32

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 21, no. 2 (1991). http://dx.doi.org/10.1515/iabi.1991.21.2.94.

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33

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 21, no. 3 (1991). http://dx.doi.org/10.1515/iabi.1991.21.3.168.

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34

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 22, no. 1 (1992). http://dx.doi.org/10.1515/iabi.1992.22.1.36a.

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35

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 22, no. 2 (1992). http://dx.doi.org/10.1515/iabi.1992.22.2.98.

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36

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 22, no. 3 (1992). http://dx.doi.org/10.1515/iabi.1992.22.3.178.

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37

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 22, no. 4 (1992). http://dx.doi.org/10.1515/iabi.1992.22.4.274.

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38

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 23, no. 1 (1993). http://dx.doi.org/10.1515/iabi.1993.23.1.45.

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39

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 23, no. 2 (1993). http://dx.doi.org/10.1515/iabi.1993.23.2.108.

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40

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 23, no. 3 (1993). http://dx.doi.org/10.1515/iabi.1993.23.3.174.

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41

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 24, no. 1 (1994). http://dx.doi.org/10.1515/iabi.1994.24.1.40.

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42

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 24, no. 2 (1994). http://dx.doi.org/10.1515/iabi.1994.24.2.118a.

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43

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 24, no. 3 (1994). http://dx.doi.org/10.1515/iabi.1994.24.3.189.

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44

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 24, no. 4 (1994). http://dx.doi.org/10.1515/iabi.1994.24.4.281.

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45

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 25, no. 1 (1995). http://dx.doi.org/10.1515/iabi.1995.25.1.39a.

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46

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 25, no. 2 (1995). http://dx.doi.org/10.1515/iabi.1995.25.2.110.

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47

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 25, no. 3 (1995). http://dx.doi.org/10.1515/iabi.1995.25.3.193.

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48

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 25, no. 4 (1995). http://dx.doi.org/10.1515/iabi.1995.25.4.283a.

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49

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 26, no. 1 (1996). http://dx.doi.org/10.1515/iabi.1996.26.1.43.

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50

"INDIAN OCEAN ISLANDS." International African Bibliography (IAB) 26, no. 3 (1996). http://dx.doi.org/10.1515/iabi.1996.26.3.222.

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