surface temperature

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.

Paper deals with statistical relations between Caribbean sea surface temperature variations and solar ac-tivity. With the use of correlation analysis between time series of mean year temperatures changes, their anoma-lies index and Wolf numbers, hypothesis of the Caribbean Sea surface temperatures variations delay caused by solar activity changes was tested. It was found that the features of sub-Antarctic intermediate waters circulation of the Atlantic Ocean cause the presence of a significant statistical relations between Caribbean Sea average surface temperatures changes and solar activity variations, that are advancing them approximately on 200 years. Developed ultralong-range forecast of Caribbean Sea average surface temperatures changes show that until the middle of the XXI century downward trend will dominate, and further, to the end of it, – upward.

In features the location of the segments an atmosphere, which the interannual changes in CCA statistically significantly associated with the same time variations surface temperature of the Pacific Ocean Gulf of Alaska. The influence of seasonal factors. The adequacy of representations the impact on air exchange between troposphere and stratosphere and the planetary gravitational waves, that form over areas of interaction of jets with inhomogeneities of the atmospheric pressure field which are destroyed in tropopause and stratosphere.

There are the influence of geography of the Pacific Ocean on the significance of the statistical relationship of interannual variations of surface temperatures and changes in the distributions of total ozone in the Earth's atmosphere. The features of the seasonal variability of the location of its waters, providing state of the ozone layer on the most significant impact.

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.

The features of the location of the ozone layer segments, where the statistical relationship of interannual changes in the CCA during the spring and autumn months, as well as variations of the surface temperature of the North Atlantic area, is essential. In the spring months of such segments of the atmosphere located HN over individual portions of subtropical and extra-tropical jet streams, and over the polar regions. Areas of similar seg-ments are maximal. In autumn the area is much less similar segments, they are located in the zone corresponding subtropical jet stream. Revealed features consistent understanding of the impact on the processes of air between the troposphere and stratosphere that have jet streams. They show a significant statistical relationship between changes in surface temperature of ocean waters, which are located in different hemispheres.