Peculiarities of slick formation on the sea surface

被引：5

作者：

Shmirko, K. A. ^{[1
,2
]}

Konstantinov, O. G. ^{[3
]}

Pavlov, A. N. ^{[1
,2
]}

Dubinkina, E. S. ^{[2
,4
]}

机构：

[1] Russian Acad Sci, Far East Branch, Inst Automat & Control Proc, Vladivostok 690041, Russia

[2] Far Eastern Fed Univ, Vladivostok 690000, Russia

[3] Russian Acad Sci, Ilichev Pacific Oceanol Inst, Far East Branch, Vladivostok 690041, Russia

[4] Russian Acad Sci, Ural Branch, Inst Ind Ecol, Ekaterinburg 620219, Russia

来源：

IZVESTIYA ATMOSPHERIC AND OCEANIC PHYSICS | 2017年 / 53卷 / 01期

基金：

俄罗斯科学基金会;

关键词：

Stokes parameters; radiance factor; reflectance coefficient; wavy sea surface; slicks; WATER BASINS; STATE; FILM;

D O I：

10.1134/S000143381701011X

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

This paper deals with surface slicks, their nature, and causes of formation in context of the development of remote detection methods and investigation of dynamic processes in the ocean and at the air-ocean interface. A simplified formalism is introduced for slick-sea surface contrast formation which takes into account the upward sea radiation and qualitatively explains in situ measurement results. The results of a detection of slicks on the coastal water surface are also described, which, together with the simplified formalism suggested, provide optimal experimental conditions for slick-sea surface contrast measurements; i.e., the contrast of the P component of reflected radiation is measured at viewing angles close to the horizon.

引用

页码：95 / 101

页数：7

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