Sea and Land: An Illustrated History of the Wonderful and Curious Things of Nature Existing Before and Since the Deluge (Classic Reprint)

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Horton, Jennifer (2011). "Effects of offshore drilling: energy vs. environment". HowStuffWorks. Archived from the original on 29 April 2013 . Retrieved 6 May 2013. Ongoing oceanographic research includes marine lifeforms, conservation, the marine environment, the chemistry of the ocean, the studying and modelling of climate dynamics, the air-sea boundary, weather patterns, ocean resources, renewable energy, waves and currents, and the design and development of new tools and technologies for investigating the deep. [122] Whereas in the 1960s and 1970s, research could focus on taxonomy and basic biology, in the 2010s, attention has shifted to larger topics such as climate change. [123] Researchers make use of satellite-based remote sensing for surface waters, with research ships, moored observatories and autonomous underwater vehicles to study and monitor all parts of the sea. [124] Law [ edit ] Cooling power plants". World Nuclear Association. 1 September 2013. Archived from the original on 21 September 2013 . Retrieved 14 September 2013.

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Muller, R. D.; Sdrolias, M.; Gaina, C.; Steinberger, B.; Heine, C. (2008). "Long-Term Sea-Level Fluctuations Driven by Ocean Basin Dynamics". Science. 319 (5868): 1357–1362. Bibcode: 2008Sci...319.1357M. doi: 10.1126/science.1151540. PMID 18323446. S2CID 23334128. Jacques Piccard: Oceanographer and pioneer of deep-sea exploration". The Independent. 5 November 2008. Archived from the original on 25 September 2015 . Retrieved 15 September 2013.Swenson, Herbert. "Why is the ocean salty?". US Geological Survey. Archived from the original on 18 April 2001 . Retrieved 17 April 2013. Catelle, W. R. (1907). "Methods of Fishing". The Pearl: Its Story, Its Charm, and Its Value. J. B. Lippincott. p.171. Archived from the original on 22 October 2014 . Retrieved 4 May 2013. b., R. N. R.; Russell, F. S.; Yonge, C. M. (1929). "The Seas: Our Knowledge of Life in the Sea and How It is Gained". The Geographical Journal. 73 (6): 571–572. doi: 10.2307/1785367. JSTOR 1785367. Archived from the original on 2 June 2018 . Retrieved 1 July 2021.

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Joint Chief of Staff (31 August 2005). "Bulk cargo" (PDF). Department of Defense Dictionary of Military and Associated Terms. Washington DC: Department of Defense. p.73. Archived from the original (PDF) on 4 June 2011 . Retrieved 24 April 2013. Research at Sea". National Oceanography Centre. 2013. Archived from the original on 6 October 2014 . Retrieved 20 September 2013.

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Desalination is the technique of removing salts from seawater to leave fresh water suitable for drinking or irrigation. The two main processing methods, vacuum distillation and reverse osmosis, use large quantities of energy. Desalination is normally only undertaken where fresh water from other sources is in short supply or energy is plentiful, as in the excess heat generated by power stations. The brine produced as a by-product contains some toxic materials and is returned to the sea. [195] Indigenous sea peoples [ edit ] a b c "The United Nations Convention on the Law of the Sea (A historical perspective)". United Nations Division for Ocean Affairs and the Law of the Sea. Archived from the original on 6 May 2017 . Retrieved 8 May 2013.

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There is a third class of phenomena of even smaller size and shorter lifetime. In this class, vertical motions may be as significant as horizontal movement, and the Coriolis force often plays a less important role. Known as the mesoscale, this class is characterized by spatial dimensions of ten to a few hundred kilometres and lifetimes of a day or less. Because of the shorter time scale and because the other forces may be much larger, the effect of the Coriolis force in mesoscale phenomena is sometimes neglected. Conforti, B.; Bravo, Luigi Ferrari (2005). The Italian Yearbook of International Law, Volume 14. Martinus Nijhoff Publishers. p.237. ISBN 978-90-04-15027-0. Archived from the original on 26 September 2020 . Retrieved 27 August 2020.Lin, I.; Liu, W. Timothy; Wu, Chun-Chieh; Wong, George T. F.; Hu, Chuanmin; Chen, Zhiqiang; Wen-Der, Liang; Yang, Yih; Liu, Kon-Kee (2003). "New evidence for enhanced ocean primary production triggered by tropical cyclone". Geophysical Research Letters. 30 (13): 1718. Bibcode: 2003GeoRL..30.1718L. doi: 10.1029/2003GL017141. S2CID 10267488. Archived from the original on 16 October 2021 . Retrieved 27 August 2020. Lovett, Richard A. (2 March 2010). "Huge Garbage Patch Found in Atlantic too". National Geographic. Archived from the original on 5 March 2010 . Retrieved 10 July 2013. Marine and Coastal: Bathymetry". Geoscience Australia. Archived from the original on 20 October 2014 . Retrieved 25 September 2013. Vukas, B. (2004). The Law of the Sea: Selected Writings. Martinus Nijhoff Publishers. p.271. ISBN 978-90-04-13863-6. Archived from the original on 25 March 2021 . Retrieved 22 January 2019. Marine habitats can be divided horizontally into coastal and open ocean habitats. Coastal habitats extend from the shoreline to the edge of the continental shelf. Most marine life is found in coastal habitats, even though the shelf area occupies only 7 percent of the total ocean area. Open ocean habitats are found in the deep ocean beyond the edge of the continental shelf. Alternatively, marine habitats can be divided vertically into pelagic (open water), demersal (just above the seabed) and benthic (sea bottom) habitats. A third division is by latitude: from polar seas with ice shelves, sea ice and icebergs, to temperate and tropical waters. [3] :150–151

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Mangal (Mangrove)". Mildred E. Mathias Botanical Garden. Archived from the original on 23 September 2015 . Retrieved 11 July 2013. The salinity of water bodies varies widely, being lower near the surface and the mouths of large rivers and higher in the depths of the ocean; however, the relative proportions of dissolved salts vary little across the oceans. The most abundant solid dissolved in seawater is sodium chloride. The water also contains salts of magnesium, calcium, potassium, and mercury, amongst many other elements, some in minute concentrations. Murakami, M. (2002). "Water in Earth's Lower Mantle". Science. 295 (5561): 1885–1887. Bibcode: 2002Sci...295.1885M. doi: 10.1126/science.1065998. PMID 11884752. S2CID 21421320. Litter dropped on the street doesn’t stay there. Rainwater and wind carries plastic waste into streams and rivers, and through drains. Drains lead to the ocean!

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These meteorites are dated to the same epoch in which water was believed to have formed on Earth—some 11 million years after the formation of the Solar System. In short, it now appears that meteorites were depositing water on Earth in its earliest days. Whittow, John B. (1984). The Penguin Dictionary of Physical Geography. Penguin Books. pp.29, 80, 246. ISBN 978-0-14-051094-2. a b Kindersley, Dorling (2011). Illustrated Encyclopedia of the Ocean. Dorling Kindersley. ISBN 978-1-4053-3308-5. The disciplines of windsurfing". World of Windsurfing. 15 April 2013. Archived from the original on 25 September 2013 . Retrieved 4 July 2013. Several nomadic indigenous groups in Maritime Southeast Asia live in boats and derive nearly all they need from the sea. The Moken people live on the coasts of Thailand and Burma and islands in the Andaman Sea. [196] Some Sea Gypsies are accomplished free-divers, able to descend to depths of 30 metres (98ft), though many are adopting a more settled, land-based way of life. [197] [198]