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Data publikacji: 6 września 2023

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1

Kumar, M. Dileep. Biogeochemistry of the North Indian Ocean. New Delhi: Indian National Science Academy, 2006.

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Kumar, M. Dileep. Nitrogen in the North Indian Ocean. Redaktorzy Raghuram N. (Nandula) editor, Society for Conservation of Nature (New Delhi, India). Indian Nitrogen Group i International Nitrogen Initiative. South Asian Nitrogen Centre. Noida: Published by Indian Nitrogen Group, Society for Conservation of Nature in association with South Asian Nitrogen Centre, International Nitrogen Initiative, 2010.

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3

Mohapatra, M., B. K. Bandyopadhyay i L. S. Rathore, red. Tropical Cyclone Activity over the North Indian Ocean. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-40576-6.

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McCreary, Julian P., i Satish R. Shetye. Observations and Dynamics of Circulations in the North Indian Ocean. Singapore: Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-5864-9.

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Niyas, N. T. Variability and trend in the cyclonic storms over North Indian ocean. Pune: National Climate Centre, Office of the Additional Director General of Meteorology (Research), India Meteorological Dept., 2009.

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Niyas, N. T. Variability and trend in the cyclonic storms over North Indian ocean. Pune: India Meteorological Department, 2009.

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7

Fisheries development in the north west Indian Ocean: The impact of commercial fishing arrangements. London: Ithaca Press, 1985.

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8

Rao, Y. V. Rama. Further evaluation of the quasi-lagrangian model for cyclone track prediction in the North Indian Ocean. Dhaka: SAARC Meteorological Research Centre, 2005.

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9

B. R. S. B. Basnayake. Structure and movement of tropical cyclones over the North Indian ocean simulated by WRF-ARW model. Dhaka: SAARC Meteorological Research Centre, 2010.

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10

Abhijit, Sarkar, i Indian Space Research Organisation, red. Winds and waves over the north Indian Ocean derived from GEOSAT altimeter data, November 1986-October 1987. Bangalore: Indian Space Research Organisation, 1990.

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11

Tsunami --grief beyond tears: Notes on a humanitarian journey in Aceh, Indonesia, and north Malaysia. Kuala Lumpur: Dewan Bahasa dan Pustaka, 2006.

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12

India. Meteorological Dept. Office of the Additional Director General of Meteorology (Research) i India. Meteorological Dept. Marine Climatology Section., red. Marine climatological summary charts 1991-2000: For the Indian ocean between 20 ̊E & 100 ̊E and North of 15 ̊S. Pune: Office of the Additional Director General of Meteorology (Research), India Meteorological Dept., 2007.

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13

North American Society of Oceanic History. Beyond Cape Horn and the Cape of Good Hope; North Americans in the Indian Ocean and the Pacific 1785-1885: Proceedings of the North American Society for Oceanic History, Ninth annual meeting. Salem, Mass: The Peabody Museum of Salem, 1986.

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14

Canada. Oceanography, ocean drilling: Memorandum of understanding between the United States of America and Canada, signed at Washington April 15, 1985. Washington, D.C: Dept. of State, 1992.

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15

Canada. Oceanography, ocean drilling: Memorandum of understanding between the United States of America and Canada, signed at Ottawa and Washington December 23 and 30, 1988. Washington, D.C: Dept. of State, 1993.

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16

Arbeitskreis "Geographie der Meere und Küsten." Tagung. Von der Nordsee bis zum Indischen Ozean: Ergebnisse der 8. Jahrestagung des Arbeitskreises "Geographie der Meere und Küsten", 13.-15. Juni 1990, Düsseldorf = From the North Sea to the Indian Ocean : results of the 8th Annual Meeting of the Working Group "Marine and coastal geography", June 13-15, 1990, Düsseldorf. Stuttgart: F. Steiner, 1991.

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17

Allen, Michael S. The Ocean of Inquiry. Oxford University Press, 2022. http://dx.doi.org/10.1093/oso/9780197638958.001.0001.

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Advaita Vedānta is one of the best-known schools of Indian philosophy, but much of its history—a history closely interwoven with that of medieval and modern Hinduism—remains surprisingly unexplored. This book focuses on a single remarkable work and its place within that history: The Ocean of Inquiry, a vernacular compendium of Advaita Vedānta by the North Indian monk Niścaldās (ca. 1791–1863). Though not well known today, Niścaldās’s work was once referred to by Vivekananda (himself a key figure in the shaping of modern Hinduism) as the most influential book in India. The present book situates The Ocean of Inquiry as a representative of both a neglected genre (vernacular Vedānta) and a neglected period (ca. 17th–19th centuries) in the history of Indian philosophy. It argues that the rise of Advaita Vedānta to a position of prestige began well before the period of British rule in India, and that vernacular texts like The Ocean of Inquiry played an important role in popularizing Vedāntic teachings. It also offers a new appraisal of the period of late Advaita Vedānta, arguing that it should not be seen as one of barren scholasticism. For thinkers like Niścaldās, intellectual “inquiry” (vicāra) was not an academic exercise but a spiritual practice—indeed, it was the central practice on the path to liberation. The book concludes by arguing that without understanding both vernacular Vedānta and the scholasticism of the period, one cannot fully understand the emergence of modern Hinduism.
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18

Buschmann, Rainer F., i Lance Nolde, red. The World’s Oceans. ABC-CLIO, 2018. http://dx.doi.org/10.5040/9798216039464.

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This single-volume resource explores the five major oceans of the world, addressing current issues such as sea rise and climate change and explaining the significance of the oceans from historical, geographic, and cultural perspectives. The World’s Oceans: Geography, History, and Environment is a one-stop resource that describes in-depth the Arctic, Atlantic, Indian, Pacific, and Southern Oceans and identifies their importance, today and throughout history. Essays address the subject areas of oceans and seas in world culture, fishing and shipping industries through history, ocean exploration, and climate change and oceans. The book also presents dozens of entries covering a breadth of topics on human culture, the environment, history, and current issues as they relate to the oceans and ocean life. Sample entries provide detailed information on topics such as the Bermuda Triangle, Coral Reefs, the Great Pacific Garbage Patch, Ice Melt, Myths and Legends, Piracy, and Whaling. Contributions to the work come from top researchers in the fields of history and maritime studies, including Paul D’Arcy, John Gillis, Tom Hoogervorst, Michael North, and Lincoln Paine. The volume highlights the numerous ways in which Earth’s oceans have influenced culture and society, from the earliest seafaring civilizations to the future of the planet.
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19

NOAA. Tide Tables 2007: West Coast of North and South America (Tide Tables West Coast of North and South America). International Marine/Ragged Mountain Press, 2006.

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20

NOAA. Tide Tables 2007: West Coast of North and South America (Tide Tables West Coast of North and South America). International Marine/Ragged Mountain Press, 2006.

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21

NOAA. Tide Tables 2007: East Coast of North and South America, Including Greenland (Tide Tables East Coast of North and South America). International Marine/Ragged Mountain Press, 2006.

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22

NOAA. Tide Tables 2007: East Coast of North and South America, Including Greenland (Tide Tables East Coast of North and South America). International Marine/Ragged Mountain Press, 2006.

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23

Rathore, L. S., M. Mohapatra i B. K. Bandyopadhyay. Tropical Cyclone Activity over the North Indian Ocean. Springer International Publishing AG, 2016.

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24

Rathore, L. S., M. Mohapatra i B. K. Bandyopadhyay. Tropical Cyclone Activity over the North Indian Ocean. Springer London, Limited, 2016.

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25

Shetye, Satish, i Julian P. McCreary. Observations and Dynamics of Circulations in the North Indian Ocean. Springer, 2023.

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26

Morrell, Abby Jane. Narrative of a Voyage to the Ethiopic and South Atlantic Ocean, Indian Ocean, Chinese Sea, North and South Pacific Oceans in the Years 1829, 1830 1831. Cambridge University Press, 2012.

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27

Morrell, Abby Jane. Narrative of a Voyage to the Ethiopic and South Atlantic Ocean, Indian Ocean, Chinese Sea, North and South Pacific Oceans in the Years 1829, 1830 1831. Cambridge University Press, 2013.

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28

Meteorological and Model Traits Knowledge Bases for North Indian Ocean Tropical Cyclones. Storming Media, 2002.

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29

Bennett, Jim. 1. Early navigational cultures. Oxford University Press, 2017. http://dx.doi.org/10.1093/actrade/9780198733713.003.0001.

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Distinct geographies, where areas of sea were demarcated not only by land, but also by climate and current, helped to create different cultures of navigation that for centuries followed individual trajectories. ‘Early navigational cultures’ explains that the sky was one thing that was shared by ancient navigational cultures. It describes the techniques used by seamen in the Mediterranean, Pacific Ocean, Indian Ocean, and North Atlantic to register direction and position—the two fundamental variables of navigation. Before the use of a magnetic compass, navigation was also possible using other techniques such as coastal navigation (or pilotage), and a good understanding of tides, currents, swells, and behaviour of seabirds.
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30

Numerical investigation on wind induced interannual variability of the North Indian Ocean SST. Pune: [Indian Institute of Tropical Meteorology], 1999.

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31

Morrell, Benjamin. Narrative of Four Voyages: To the South Sea, North and South Pacific Ocean, Chinese Sea, Ethiopic and Southern Atlantic Ocean, Indian and Antarctic Ocean. University of Cambridge ESOL Examinations, 2014.

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32

Morrell, Benjamin. Narrative of Four Voyages: To the South Sea, North and South Pacific Ocean, Chinese Sea, Ethiopic and Southern Atlantic Ocean, Indian and Antarctic Ocean. University of Cambridge ESOL Examinations, 2014.

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33

(Editor), Gwyn Campbell, Suzanne Miers (Editor) i Joseph C. Miller (Editor), red. Women and Slavery, V. 1: Africa, the Indian Ocean World, and the Medieval North Atlantic. Ohio University Press, 2007.

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34

(Editor), Gwyn Campbell, Suzanne Miers (Editor) i Joseph C. Miller (Editor), red. Women and Slavery, V. 1: Africa, the Indian Ocean World and the Medieval North Atlantic. Ohio University Press, 2007.

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35

Further evaluation of the quasi-lagrangian model for cyclone track prediction in the North Indian ocean. Dhaka: SAARC Meteorological Research Centre, 2005.

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36

Further evaluation of the quasi-lagrangian model for cyclone track prediction in the North Indian ocean. Dhaka: SAARC Meteorological Research Centre, 2005.

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37

Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.

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The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry and wet events are regulated by the boreal summer ISO (BSISO). The BSISO over Indian monsoon region consists of northward propagating 30–60 day and westward propagating 10–20 day modes. The “clustering” of synoptic activity was separately modulated by both the 30–60 day and 10–20 day BSISO modes in approximately equal amounts. The clustering is particularly strong when the enhancement effect from both modes acts in concert. The northward propagation of BSISO is primarily originated from the easterly vertical shear (increasing easterly winds with height) of the monsoon flows, which by interacting with the BSISO convective system can generate boundary layer convergence to the north of the convective system that promotes its northward movement. The BSISO-ocean interaction through wind-evaporation feedback and cloud-radiation feedback can also contribute to the northward propagation of BSISO from the equator. The 10–20 day oscillation is primarily produced by convectively coupled Rossby waves modified by the monsoon mean flows. Using coupled general circulation models (GCMs) for ISO prediction is an important advance in subseasonal forecasts. The major modes of ISO over Indian monsoon region are potentially predictable up to 40–45 days as estimated by multiple GCM ensemble hindcast experiments. The current dynamical models’ prediction skills for the large initial amplitude cases are approximately 20–25 days, but the prediction of developing BSISO disturbance is much more difficult than the prediction of the mature BSISO disturbances. This article provides a synthesis of our current knowledge on the observed spatial and temporal structure of the ISO over India and the important physical processes through which the BSISO regulates the ISM active-break cycles and severe weather events. Our present capability and shortcomings in simulating and predicting the monsoon ISO and outstanding issues are also discussed.
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38

Marine climatological summary charts 1991-2000 for the Indian ocean between 20̊E & 100̊E and North of 15̊S. Pune: Office of the Additional Director of Meteorology (Research), India Meteorological Dept., 2007.

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39

Marine climatological summary charts 1991-2000 for the Indian ocean between 20E & 100E and North of 15S. Pune: Office of the Additional Director of Meteorology (Research), India Meteorological Department, 2007.

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40

Marine climatological summary charts 1991-2000 for the Indian ocean between 20E & 100E and North of 15S. Pune: Office of the Additional Director of Meteorology (Research), India Meteorological Department, 2007.

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41

Narrative of Four Voyages to the South Sea, North and South Pacific Ocean, Chinese Sea, Ethiopic and Southern Atlantic Ocean, Indian and Antarctic Ocean, from the Year 1822 To 1831. Creative Media Partners, LLC, 2022.

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42

Morrell, Benjamin. Narrative of Four Voyages: To the South Sea, North and South Pacific Ocean, Chinese Sea, Ethiopic and Southern Atlantic Ocean, Indian and Antarctic Ocean; from the Year 1822 To 1831. Creative Media Partners, LLC, 2018.

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43

Morrell, Benjamin. A Narrative of Four Voyages: The South Sea, North and South Pacific Ocean, Chinese Sea, Ethiopic and Southern Atlantic Ocean, Indian and Antarctic Ocean from the Year 1822 to 1831. Kessinger Publishing, 2005.

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Morrell, Benjamin. Narrative of Four Voyages to the South Sea, North and South Pacific Ocean, Chinese Sea, Ethiopic and Southern Atlantic Ocean, Indian and Antarctic Ocean, from the Year 1822 To 1831. HardPress, 2020.

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45

Morrell, Benjamin. A Narrative Of Four Voyages: The South Sea, North And South Pacific Ocean, Chinese Sea, Ethiopic And Southern Atlantic Ocean, Indian And Antarctic Ocean From The Year 1822 To 1831. Kessinger Publishing, LLC, 2005.

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46

Earle, Peter. English Sailors, 1570-1775. Liverpool University Press, 2018. http://dx.doi.org/10.5949/liverpool/9780968128831.003.0006.

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This chapter describes the competition Britain faced in its two century journey of becoming the possessor of the world’s largest trading fleet and the world’s most powerful navy. It stops at several important benchmark dates in European shipping trade history, including the growth of the East Coast coal trade; trade with the Mediterranean; oceanic fishing off the coast of Iceland and the Newfoundland Banks; voyages to the Indian Ocean; colonization in North America and West Indies; increase in demand for timber and marine stores; and the rapid expansion of slave trade from West Africa. The chapter also documents the increased employment levels as a result of trade growth, and estimates at the number of sailors employed at significant dates in maritime history, and investigates their geographical origin, wage, and approach to teamwork.
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47

Marine climatological summary charts 1991-2000: For the Indian ocean between 20 ̊E & 100 ̊E and North of 15 ̊S. Pune: Office of the Additional Director General of Meteorology (Research), India Meteorological Dept., 2007.

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48

al- Tashāwur al-fannī ḥawla al-taʻarruf ʻalá nashāṭāt taqdīr al-makhzūn al-samakī wa-taqwīmihā fī minṭaqat shamāl ghārb al-Muḥīṭ al-Hindī (al-khiljān wa-al-Baḥr al-Aḥmar): Technical consultation on identification and evaluation of fish stock assessment activities in the North-Western India Ocean (gulfs and Red Sea) : background papers : 5-7 December 1993, Gulf hotel, Bahrain. [S.l.]: FAO, 1993.

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49

Dussubieux, Laure, i Heather Walder, red. The Elemental Analysis of Glass Beads. Leuven University Press, 2022. http://dx.doi.org/10.11116/9789461664655.

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Glass beads, both beautiful and portable, have been produced and traded globally for thousands of years. Modern archaeologists study these artifacts through sophisticated methods that analyze the glass composition, a process which can be utilized to trace bead usage through time and across regions. This book publishes open-access compositional data obtained from laser ablation – inductively coupled plasma – mass spectrometry, from a single analytical laboratory, providing a uniquely comparative data set. The geographic range includes studies of beads produced in Europe and traded widely across North America and beads from South and Southeast Asia traded around the Indian Ocean and beyond. The contributors provide new insight on the timing of interregional interactions, technologies of bead production and patterns of trade and exchange, using glass beads as a window to the past. This volume will be a key reference for glass researchers, archaeologists, and any scholars interested in material culture and exchange; it provides a wide range of case studies in the investigation and interpretation of glass bead composition, production and exchange since ancient times.
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50

Goswami, B. N., i Soumi Chakravorty. Dynamics of the Indian Summer Monsoon Climate. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.613.

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Lifeline for about one-sixth of the world’s population in the subcontinent, the Indian summer monsoon (ISM) is an integral part of the annual cycle of the winds (reversal of winds with seasons), coupled with a strong annual cycle of precipitation (wet summer and dry winter). For over a century, high socioeconomic impacts of ISM rainfall (ISMR) in the region have driven scientists to attempt to predict the year-to-year variations of ISM rainfall. A remarkably stable phenomenon, making its appearance every year without fail, the ISM climate exhibits a rather small year-to-year variation (the standard deviation of the seasonal mean being 10% of the long-term mean), but it has proven to be an extremely challenging system to predict. Even the most skillful, sophisticated models are barely useful with skill significantly below the potential limit on predictability. Understanding what drives the mean ISM climate and its variability on different timescales is, therefore, critical to advancing skills in predicting the monsoon. A conceptual ISM model helps explain what maintains not only the mean ISM but also its variability on interannual and longer timescales.The annual ISM precipitation cycle can be described as a manifestation of the seasonal migration of the intertropical convergence zone (ITCZ) or the zonally oriented cloud (rain) band characterized by a sudden “onset.” The other important feature of ISM is the deep overturning meridional (regional Hadley circulation) that is associated with it, driven primarily by the latent heat release associated with the ISM (ITCZ) precipitation. The dynamics of the monsoon climate, therefore, is an extension of the dynamics of the ITCZ. The classical land–sea surface temperature gradient model of ISM may explain the seasonal reversal of the surface winds, but it fails to explain the onset and the deep vertical structure of the ISM circulation. While the surface temperature over land cools after the onset, reversing the north–south surface temperature gradient and making it inadequate to sustain the monsoon after onset, it is the tropospheric temperature gradient that becomes positive at the time of onset and remains strongly positive thereafter, maintaining the monsoon. The change in sign of the tropospheric temperature (TT) gradient is dynamically responsible for a symmetric instability, leading to the onset and subsequent northward progression of the ITCZ. The unified ISM model in terms of the TT gradient provides a platform to understand the drivers of ISM variability by identifying processes that affect TT in the north and the south and influence the gradient.The predictability of the seasonal mean ISM is limited by interactions of the annual cycle and higher frequency monsoon variability within the season. The monsoon intraseasonal oscillation (MISO) has a seminal role in influencing the seasonal mean and its interannual variability. While ISM climate on long timescales (e.g., multimillennium) largely follows the solar forcing, on shorter timescales the ISM variability is governed by the internal dynamics arising from ocean–atmosphere–land interactions, regional as well as remote, together with teleconnections with other climate modes. Also important is the role of anthropogenic forcing, such as the greenhouse gases and aerosols versus the natural multidecadal variability in the context of the recent six-decade long decreasing trend of ISM rainfall.
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