Analysis of clouds modes in Antarctica

Authors

  • О. М. Прокоф’єв Odessa State Environmental University, Ukraine

Keywords:

general overcast, overcast of the bottom circle, Antarctica

Abstract

General overcast of Antarctica, overcast of the bottom circle and the attitude of average quantity of clouds of the bottom circle to total of clouds is considered. Existential distribution of the general overcast and overcast of the bottom circle has been found out. The greatest quantity of overcast is characteristic for the Bellingshausen station which is on a way of moving cyclones in East-Pacific and Southern-American branches. Modern dynamics of overcast quantity of different circles has been shown.

Author Biography

О. М. Прокоф’єв, Odessa State Environmental University

Assistant

References

Vojtkovskij, K.F. (1999). Osnovy gljaciologii. M., Nauka, 256 s.

Gljaciologicheskij slovar'. (1976). L., Gidrometeoizdat, 247 s.

Kotljakov, V.M. (2010). Kriosfera i klimat. Jekologija i zhizn', 11, 51-59.

Klimat poljarnyh rajonov. (1973). L., Gidrometeoizdat, 444 s.

Kukla, G. (1981). Snow cover and climate. Glaciol. Data (Snow Watch 1980), 11, 27–29.

Danova, T., Prokofev, O. (2008). Description of temperature and regime of humidity of troposphere above Antarctic Continent. Materіali Mіzhnarodnoy antarktichnoy konferencіy ІAS 2008 "Ukrayna v Antarkticі - nacіonal'nі prіoriteti і global'na іntegracіja" m. Kiyv, Ukrayna, 77.

Danova T.E., Prokof'ev O.M. (2009). Dinamika temperatury vozduha troposfery pribrezhnyh stancij Antarktidy. Ukrayns'kij gіdrometeorologіchnij zhurnal, 5, 107-112.

Baza dannyh AANII [Jelektronnyj resurs]. Retrieved from: http://www.aari.ru (data zvernennja: 15.01.2013).

Goncharova, L.D., Shkol'nij, E.P. (2007). Metodi obrobki ta analіzu gіdrometeorologіchnoy іnformacіy. Navchal'nij posіbnik. Odesa, 454 s.

Published

2013-12-05

Issue

Section

Geography