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Heat-flow measurements in the Atlantic Ocean, Indian Ocean, Mediterranean Sea, and Red Sea
Journal of Geophysical Research, 1966Eight heat-flow stations in the Atlantic Ocean southeast of Bermuda and on the outer ridge of the Puerto Rico trench have a mean of 1.01 μcal/cm2 sec. A single station on the mid-Atlantic ridge gave a value of 0.90μcal/cm2 sec. The results of four stations north of the Seychelles in the Indian Ocean range from 0.87 to 1.35 μcal/cm2 sec.
F. S. Birch, A. J. Halunen
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Sea-Level and Ocean Heat-Content Change
2013Abstract The ocean has the largest heat capacity in the climate system and as a result the ocean plays a critical role in the climate. Changes in ocean heat content dominate the Earth’s energy storage; and the ocean’s thermal expansion has been a major contributor to sea-level rise in the twentieth century and likely to be the largest contributor in ...
Church, J.A. +4 more
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Environmental science and pollution research international, 2021
Andrei Bagaev +6 more
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Andrei Bagaev +6 more
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Oceans and air–sea interaction
2011Since the publication of the First Edition of this book, many new studies have focused on the role of air–sea interaction in tropical atmospheric intraseasonal variability (ISV). The aim of this section is to summarize the results of these new studies and to extract their main conclusions.
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Holococcolithophorids from the Indian Ocean, Red Sea, Mediterranean Sea and North Atlantic Ocean
Marine Micropaleontology, 1991Abstract Holococcolithophorids formed half of the total number of species of the 1985 summer coccolithophorid flora in surface waters of the Indian Ocean, Red Sea, Mediterranean Sea and North Atlantic. They showed highest frequencies under oligotrophic conditions. Fifty-four taxa of holococcolithophorids were identified.
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Submarine gravity measurements in the Atlantic Ocean, Indian Ocean, Red Sea and Mediterranean Sea
Proceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1957The results are given of fifty-eight gravity measurements made at sea in H. M. Submarine Acheron between April and October 1955. Of these, six lie in the North Atlantic, eight in the South Atlantic and thirty-seven in the Indian Ocean.
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Erratum: Sea-Level and Ocean-Currents
Science, 1886In Science , vii. p. 75, in the letter entitled 'Sea-level and ocean-currents,' seventh line, 'Bourdalone' should read 'Bourdaloue;' thirty-third line, 'diversity' should read 'density;' p. 76, second column, thirteenth line, '25 feel' should read '2.5 feet.'
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