Answer:
South Atlantic High is a semipermanent pressure high centered at about 25°S, 15°W, in the Atlantic Ocean. It is also called the St. Helena High, Saint Helena island being the only land in the area. It can stretch thousands of miles across the South Atlantic.[1][2] This does not mean that the position and the intensity of this anticyclone are permanent, but just that we find an anticyclone on the maps describing the average monthly pressure. This area of high pressure is part of the great subtropical belt of anticyclones called the subtropical ridge. The centre of the high pressure region tends to follow the seasonal variation in position of the sun, moving south in the southern summer and north in the southern winter. This affects the climate of the adjacent continental areas, bringing seasonal changes to the climate and weather as the position of the high oscillates.
<u>Answer:</u>
One way that the world's sea influences climate and atmosphere is by assuming a significant opportunity in keeping our planet warm. Most of the radiation from the sun is consumed by the sea, especially in tropical waters around the equator, where the sea demonstrations like a monstrous, heat-holding sun based board. Land regions likewise ingest some daylight, and the climate holds heat that would somehow or another rapidly emanate into space after dusk.
Sea flows act a lot of like a transport line, moving warm water and precipitation from the equator toward the posts and cold water from the shafts back to the tropics.
