Title On the possible climatic consequences of the large oil spills in oceans /
Authors Prokopčiuk, Nina ; Tarasiuk, Nikolaj ; Franck, Ulrich ; Schraufnagel, Dean Ernest ; Valiulis, Algirdas ; Konstantinova, Marina ; Zielinski, Tymon ; Valiulis, Arūnas
DOI 10.3390/atmos15101216
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Is Part of Atmosphere.. Basel : MDPI. 2024, vol. 15, iss. 10, art. no. 1216, p. [1-20].. eISSN 2073-4433
Keywords [eng] climate warming ; oil spills ; North Atlantic Oscillation ; surface film ; ocean pollution ; production water
Abstract [eng] In the North Atlantic and the Northern Ocean, from the second half of 2010 to 2014, satellite imagery data showed increased surface water temperatures (in the Icelandic Depression area in September–October 2010, it was 1.3 °C higher than in 2009). The peak of the annual sum of mean monthly ocean surface temperatures near the Icelandic Depression in 2010 (109.3 °C), as well as the negative values of the monthly averaged North Atlantic Oscillation (NAO) indices, estimated in the second half of 2010 and until March 2011, can be explained by the appearance of an additional film of oil origin on the water surface, formed after an oil spill accident at the Deepwater Horizon drilling rig in the Gulf of Mexico. Insufficient evaporative cooling of surface waters near the Icelandic Depression related to the formation of an additive film due to the influence of pollution of the North Sea by oil can explain the earlier peak in the annual sum of mean monthly ocean surface temperatures near the Icelandic Depression in 2003 (107.2 °C). Although global warming is usually ascribed to increased greenhouse gases in the atmosphere, ocean surface water pollution could increase the heat content of the ocean and explain the steady temperature stratification and desalination of these waters due to the melting of Greenland’s glaciers. Thus, when analyzing the concept of global warming, it is necessary to take into account the aspects of pollution of the ocean surface waters to assess the changes in their capacity to accumulate solar radiation, as well as the changes in the heat content of the ocean mixing zone (~200 m).
Published Basel : MDPI
Type Journal article
Language English
Publication date 2024
CC license CC license description