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Books on the topic 'North Atlantic sea surface temperature'

Author: Grafiati

Published: 2 June 2025

Last updated: 31 July 2025

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1

Norris, S. W. Near surface sea temperatures in coastal waters of the North Sea, English Channel and Irish Sea. Centre for Environment, Fisheries and Aquaculture Science, 2001.

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2

Becker, Gerd Axel. Atlas of North Sea surface temperatures: Weekly and monthly means for the period 1969 to 1993. Bundesamt für Seeschiffahrt und Hydrographie, 2000.

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3

Steffen, Konrad. Surface temperature and sea ice of an Arctic polynya: North Water in winter : Canadian and Greenlandic High Arctic. Geographisches Institut, Eidgenössische Technische Hochschule Zürich, 1985.

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4

Kishōbu, Japan Kishōchō Kaiyō. Hokusei Taiheiyō zenkyū kaimen suion heinen bunpuzu: Climatic charts of sea surface temperature of the western north Pacific and the global ocean. Kishōchō Kaiyō Kishōbu, 1991.

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5

Levy-Ryan, Ellen. Moored current meter data from the Atlantic north equatorial counter current near 6⁰ N 28⁰ W (March-October, 1984): Vol. XXXVII. Woods Hole Oceanographic Institution, 1985.

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6

André, Rochon, and American Association of Stratigraphic Palynologists. Foundation., eds. Distribution of recent dinoflagellate cysts in surface sediments from the North Atlantic Ocean and adjacent seas in relation to sea-surface parameters. American Association of Stratigraphic Palynologists, Inc., 1999.

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7

Levy-Ryan, Ellen. Moored current meter and temperature-pressure recorder measurements from the western North Atlantic (high energy benthic boundary layer and abyssal circulation experiments 1983-1984): Volume XXXIX. Woods Hole Oceanographic Institution, 1986.

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8

Singh, Sandipa. Monthly maps of sea surface height in the North Atlantic and zonal indices for the Gulf Stream using TOPEX/Poseidon altimeter data. Woods Hole Oceanographic Institution, 1997.

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9

A, Kelly Kathryn, and United States. National Aeronautics and Space Administration., eds. Monthly maps of sea surface height in the North Atlantic and zonal indices for the Gulf Stream using TOPEX/Poseidon altimeter data. Woods Hole Oceanographic Institution, 1997.

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10

A, Kelly Kathryn, and United States. National Aeronautics and Space Administration., eds. Monthly maps of sea surface height in the North Atlantic and zonal indices for the Gulf Stream using TOPEX/Poseidon altimeter data. Woods Hole Oceanographic Institution, 1997.

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11

Riehl, Herbert 1915, and University of Chicago Dept of Meteo. Sea Surface Temperatures of the North Atlantic, 1887-1936. Creative Media Partners, LLC, 2021.

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12

Servain, Jacques. Climatic atlas of the tropical Atlantic wind stress and sea surface temperature, 1985-1989. IFREMER, 1990.

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13

Goswami, B. N., and 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 sta

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14

Benestad, Rasmus. Climate in the Barents Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.655.

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The Barents Sea is a region of the Arctic Ocean named after one of its first known explorers (1594–1597), Willem Barentsz from the Netherlands, although there are accounts of earlier explorations: the Norwegian seafarer Ottar rounded the northern tip of Europe and explored the Barents and White Seas between 870 and 890 ce, a journey followed by a number of Norsemen; Pomors hunted seals and walruses in the region; and Novgorodian merchants engaged in the fur trade. These seafarers were probably the first to accumulate knowledge about the nature of sea ice in the Barents region; however, scienti

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15

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can hav

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16

Lézine, Anne-Marie. Vegetation at the Time of the African Humid Period. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.530.

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An orbitally induced increase in summer insolation during the last glacial-interglacial transition enhanced the thermal contrast between land and sea, with land masses heating up compared to the adjacent ocean surface. In North Africa, warmer land surfaces created a low-pressure zone, driving the northward penetration of monsoonal rains originating from the Atlantic Ocean. As a consequence, regions today among the driest of the world were covered by permanent and deep freshwater lakes, some of them being exceptionally large, such as the “Mega” Lake Chad, which covered some 400 000 square kilom

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