On the possibile contrinution of advection into the formation of CIL in the Baltic Sea :: IKBFU's united scientific journal editorial office


Forgot your password?
Login As
You can log in if you are registered at one of these services:
The real and legitimate goal of the sciences is the endowment of human life with new inventions and riches
Francis Bacon

DOI-generator Search by DOI on Crossref.org

On the possibile contrinution of advection into the formation of CIL in the Baltic Sea

Author Kozlova O.
Pages 156-162
Article Download
Keywords T, S-analysis, the Baltic Sea, cold intermediate layer.
Abstract (summary) This article offers the results of an analysis of mean annual (1952—2005) data on the  temperature and salinity in the Baltic Sea published by the Institute for Baltic Sea Research (Warnemünde, Germany). The data were averaged by months, one-degree quadrants, and 10 meter-thick layers. It was found that, throughout the year, 54 % of the minimum sea water temperatures in the intermediate layer are 0.01—0.1 °C lower than those at the surface of the same spot. It suggests the possibility of advection contributing to the formation of CIL in the Baltic Sea.

1. Владимирцев Ю. А. О промежуточных слоях в океане // Океанология.1963. Т. 3, вып. 5. С. 798—805.
2. Гидрометеорология и гидрохимия морей СССР. Л., 1992. Т. 3 : Балтийское море.
3. Козлова О. И. Характеристики холодного промежуточного слоя в централь-ной части Балтийского моря после зим различной суровости // Исследовано в России. 2010. С. 149—158. URL: http://zhurnal.gpi.ru/articles/2010/010.pdf (дата обращения: 04.05.2012).
4. Морозов Е. Г., Щука С. А., Голенко Н. Н. и др. Структура температуры в прибрежной зоне Балтийского моря // Доклады Академии наук. 2007. Т. 416, № 1.С. 115—118.
5. State and Evolution of the Baltic Sea, 1952—2005. A Detailed 50-year Survey of Meteorology and Climate, Physics, Chemistry, Biology, and Marine Environment //ed. by R. Feistel [et al.]. Wiley & Sons, 2008.

Back to the section