Ecological Systems and Devices Annotation << Back About anomalies of currents and temperatures in east part of cyclonic circulation of the average of the Сaspian sea Ambrosimov A.K. The results of hydrophysical supervision received over the Peschanomyssky raising are presented in article, when studying genesis of an upwelling in a northeast coastal zone of the Average of the Caspian Sea. It is shown that at collision of cyclonic circulation with the Peschanomyssky raising there is a perturbation of currents. As a result of interaction the part of benthonic waters beats off in the western direction, other part of benthonic waters passes through a raising and moves to the north. Over a raising there is an intensive hashing of a stream water circulations are formed, water temperature falls – the upwelling is formed. In east branch of cyclonic circulation abnormal splashes in water temperature on the benthonic horizons are registered. There are some hypotheses of emergence of these anomalies, primary from which are the assumption of drainage of warm waters from crust breaks at the bottom of the Caspian Sea. Keywords: Central Caspian Sea, Peschanomyssky raising, benthonic currents, upwelling, temperature anomalies. Contacts: E-mail: ambrosimov@ocean.ru Pp. 36-41.