Атлантичний океан

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.

Surface temperatures of many waters in the Atlantic Ocean during the period of the modern warming rising steadily, driven by a reduction of its apvelings and increase the flow of heat delivered from the South Atlantic jet northern South Equatorial Current. In the period of 2002 - 2011 years. Atlantic warming has stopped. In subsequent years, the twenty-first century, probably reducing its surface temperature, which could lead to a cooling of the climate in Europe and North America.

General regularities of location in the Atlantic ocean areas, where in the period 2000 - 2012, dominated steady tendencies of changes of mean monthly values of surface temperature, time of year does not depend. At the same time, their configurations and sizes in the change of seasons significantly changed. This indicates the importance of influence on the process, not only the factor of water of the Atlantic, the Arctic and the Antarctic, but also a factor of changes in the intensity of what is happening in its areas of upwelling. The location of the waters of the Atlantic ocean, where in this period there was a significant cooling, coin-cides with the position of his areas in which the interannual changes of surface temperatures significantly affect the state of the Arctic and North Atlantic oscillations. Above them are the main tropospheric jet stream. This suggests the possibility of a significant impact of the process-not only the greenhouse effect in the earth's atmos-phere, but also on the weather conditions change in many extratropical Northern hemisphere regions, as well as variations of the CCA over many of its regions, which took place in the same period.