термический режим

Modern And Credible Tendencies Of Waters Thermal Mode Of Black Sea North-Western Part And Estuarine Areas Of The Rivers Which Fall In Him

The stream of O2 is determined by the thermal mode of superficial layer of shelfy area of sea and estuarine areas of the rivers which fall in him. The tendencies of interannual changes of these modes are in-process investigational on the example of North-western part of sea and estuarine areas of the rivers Danube, Dnepr and South Bug. The reliable tendencies of changeability of the noted descriptions are analysed during realization of one of possible scenarios of changes of climate in the Northern Atlantic region.

The irregularity of the daily rotation of the earth, as a factor of variability of the temperature regime of the northern hemisphere

Interannual changes of mean monthly temperature of water, brought to the Northern hemisphere Lands of South-Passatian currents of the Atlantic and Pacific oceans, are characterized by the increasing trends, while in december-march, in contrast to the other months. are significantly correlated between themselves, as well as with changes in the angular velocity of the daily rotation of our planet. It allows to assume, that the irregularity of the Earth's rotation can be one of the factors of modern variability of the temperature regime of the Northern hemisphere.
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