Atmospheric processes contributing to reversal of the Soya Current in the La Perouse strait

A.A. Bobkov, G.V. Shevchenko, V.Yu. Tsepelev

Результат исследований: Публикации в книгах, отчётах, сборниках, трудах конференцийстатья в сборнике

Выдержка

Research is based on the analysis of cases of reversal of the Soya Current vectors registered in the cold period 1999 – 2001 be means of mooring stations located in the La Perouse Strait. Proved that such turns can be caused by two factors: 1) general weakening of a flow in the winter period due to alignment of difference in levels between Japanese and Okhotsk seas; 2) anemobaric influence on the water area of a strait through drift component depending on force and a direction of a wind, and through gradients of atmospheric pressure. Action of latter is studied. Tidal effect is not taken into consideration as it is off a period of probed temporary scale. Optimum localization of centers of sea level pressure above the area under discussion contributing origin to gale winds from the East at moments of reversal of current is defined and the gradients of atmospheric pressure are calculated. Results are compared. Discovered, that the quota of a gradient of atmospheric pressure between water areas in the periods
Язык оригиналаанглийский
Название основной публикацииProceedings of the 19th International Symposium on Okhotsk Sea & Sea Ice, Mombetsu, 22-28 February, 2004
ИздательThe Okhotsk Sea & Cold Ocean Research Association (OSCORA)
Страницы282-286
СостояниеОпубликовано - 2004
Опубликовано для внешнего пользованияДа

Отпечаток

atmospheric pressure
strait
sea level pressure
water
winter
atmospheric process
analysis
cold
effect
station
alignment
sea

Цитировать

Bobkov, A. A., Shevchenko, G. V., & Tsepelev, V. Y. (2004). Atmospheric processes contributing to reversal of the Soya Current in the La Perouse strait. В Proceedings of the 19th International Symposium on Okhotsk Sea & Sea Ice, Mombetsu, 22-28 February, 2004 (стр. 282-286). The Okhotsk Sea & Cold Ocean Research Association (OSCORA).
Bobkov, A.A. ; Shevchenko, G.V. ; Tsepelev, V.Yu. / Atmospheric processes contributing to reversal of the Soya Current in the La Perouse strait. Proceedings of the 19th International Symposium on Okhotsk Sea & Sea Ice, Mombetsu, 22-28 February, 2004. The Okhotsk Sea & Cold Ocean Research Association (OSCORA), 2004. стр. 282-286
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abstract = "Research is based on the analysis of cases of reversal of the Soya Current vectors registered in the cold period 1999 – 2001 be means of mooring stations located in the La Perouse Strait. Proved that such turns can be caused by two factors: 1) general weakening of a flow in the winter period due to alignment of difference in levels between Japanese and Okhotsk seas; 2) anemobaric influence on the water area of a strait through drift component depending on force and a direction of a wind, and through gradients of atmospheric pressure. Action of latter is studied. Tidal effect is not taken into consideration as it is off a period of probed temporary scale. Optimum localization of centers of sea level pressure above the area under discussion contributing origin to gale winds from the East at moments of reversal of current is defined and the gradients of atmospheric pressure are calculated. Results are compared. Discovered, that the quota of a gradient of atmospheric pressure between water areas in the periods",
author = "A.A. Bobkov and G.V. Shevchenko and V.Yu. Tsepelev",
year = "2004",
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pages = "282--286",
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Bobkov, AA, Shevchenko, GV & Tsepelev, VY 2004, Atmospheric processes contributing to reversal of the Soya Current in the La Perouse strait. в Proceedings of the 19th International Symposium on Okhotsk Sea & Sea Ice, Mombetsu, 22-28 February, 2004. The Okhotsk Sea & Cold Ocean Research Association (OSCORA), стр. 282-286.

Atmospheric processes contributing to reversal of the Soya Current in the La Perouse strait. / Bobkov, A.A.; Shevchenko, G.V.; Tsepelev, V.Yu.

Proceedings of the 19th International Symposium on Okhotsk Sea & Sea Ice, Mombetsu, 22-28 February, 2004. The Okhotsk Sea & Cold Ocean Research Association (OSCORA), 2004. стр. 282-286.

Результат исследований: Публикации в книгах, отчётах, сборниках, трудах конференцийстатья в сборнике

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T1 - Atmospheric processes contributing to reversal of the Soya Current in the La Perouse strait

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N2 - Research is based on the analysis of cases of reversal of the Soya Current vectors registered in the cold period 1999 – 2001 be means of mooring stations located in the La Perouse Strait. Proved that such turns can be caused by two factors: 1) general weakening of a flow in the winter period due to alignment of difference in levels between Japanese and Okhotsk seas; 2) anemobaric influence on the water area of a strait through drift component depending on force and a direction of a wind, and through gradients of atmospheric pressure. Action of latter is studied. Tidal effect is not taken into consideration as it is off a period of probed temporary scale. Optimum localization of centers of sea level pressure above the area under discussion contributing origin to gale winds from the East at moments of reversal of current is defined and the gradients of atmospheric pressure are calculated. Results are compared. Discovered, that the quota of a gradient of atmospheric pressure between water areas in the periods

AB - Research is based on the analysis of cases of reversal of the Soya Current vectors registered in the cold period 1999 – 2001 be means of mooring stations located in the La Perouse Strait. Proved that such turns can be caused by two factors: 1) general weakening of a flow in the winter period due to alignment of difference in levels between Japanese and Okhotsk seas; 2) anemobaric influence on the water area of a strait through drift component depending on force and a direction of a wind, and through gradients of atmospheric pressure. Action of latter is studied. Tidal effect is not taken into consideration as it is off a period of probed temporary scale. Optimum localization of centers of sea level pressure above the area under discussion contributing origin to gale winds from the East at moments of reversal of current is defined and the gradients of atmospheric pressure are calculated. Results are compared. Discovered, that the quota of a gradient of atmospheric pressure between water areas in the periods

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BT - Proceedings of the 19th International Symposium on Okhotsk Sea & Sea Ice, Mombetsu, 22-28 February, 2004

PB - The Okhotsk Sea & Cold Ocean Research Association (OSCORA)

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Bobkov AA, Shevchenko GV, Tsepelev VY. Atmospheric processes contributing to reversal of the Soya Current in the La Perouse strait. В Proceedings of the 19th International Symposium on Okhotsk Sea & Sea Ice, Mombetsu, 22-28 February, 2004. The Okhotsk Sea & Cold Ocean Research Association (OSCORA). 2004. стр. 282-286