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South Atlantic High on the right. 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.
The southern parts of the Atlantic, Indian, and Pacific oceans have three anticyclones over the Horse latitudes. Further South, a fairly continuous series of low pressure areas cover the ocean near Antarctica during the whole year and does the Antarctica High over the continent.
A high-pressure area, high, or anticyclone, is an area near the surface of a planet where the atmospheric pressure is greater than the pressure in the surrounding regions. Highs are middle-scale meteorological features that result from interplays between the relatively larger-scale dynamics of an entire planet's atmospheric circulation .
Savannah is in for a pre-summer swelter and a potential repeat of Monday’s thunderstorms. An Atlantic high-pressure system lingering over coastal Georgia and the South Carolina Lowcountry will ...
The track is likely to be heavily influenced by the position of a dome of high pressure along the southern Atlantic coast of the United States and the speed of an approaching non-tropical storm ...
The Azores High also known as North Atlantic (Subtropical) High/Anticyclone or the Bermuda-Azores High, is a large subtropical semi-permanent centre of high atmospheric pressure typically found south of the Azores in the Atlantic Ocean, at the Horse latitudes. It forms one pole of the North Atlantic oscillation, the other being the Icelandic Low.
The National Hurricane Center said Friday it is tracking 3 disturbances in the Atlantic, ... an area of high pressure expected to develop ... The most searched for chocolate dessert in the South.
The South Atlantic Convergence Zone (SACZ): The SACZ controls rainfall in the southern subtropics and extends southeastward from the large continental convective zone of tropical South America. It is generated by moisture convergence between the South Atlantic high pressure zone and the continental thermal low pressure zone.