We characterize the climate of the Atlantic Ocean: temperature, humidity, features

It is impossible to say unambiguously how he, the climate of the Atlantic Ocean, can not, since this pond is located practically in all areas of our planet. It stretches from the North to the South, touching the shores of the polar islands and continents. Its width is equal to the difference between Europe and North America, between Africa and South America. Of course, such a situation will cause various weather conditions in certain areas of a given geographic object. Because now we will consider the climate of the Atlantic Ocean briefly, describing its main zones and their features.

Belts in which the pond lies

To begin with, we note that in terms of its size, the waters of the Atlantic are considered second in the world. The ocean itself plays a major role in shaping the climate on the continents that are adjacent to it. For example, its northern part is warmer than the southern part due to the Gulf Stream. Therefore, in countries of Western Europe and North Africa, the climate is mild, without sharp temperature changes. But the adjoining lands in the south are characterized by more windy weather and a sharper change in the temperature regime. Thus, the climate of the Atlantic Ocean forms the weather on the lands that it ishes, which largely affects the seismic state of the entire planet. The very waters of the Atlantic are located in all climatic zones. We will count from the equator in both directions, since their location is identical. This equatorial belt, subequatorial, tropical, subtropical and temperate. Further in the North waters pass into the arctic zone, and in the south - into the Antarctic zone.

Air and water surface temperature

Here it is necessary to distinguish that from what hemisphere we speak - North or South, it depends on how warm or cold this or that climate zone will be. Equatorial latitude is characterized, as you guessed, by the highest temperature indicators. Here during the year the thermometer does not fall below the mark of +25 (on the average it is 30-32). Approximately the same heat and surface water. In the northern tropics , the dry trade winds blow, which carry sand from the Sahara. Because in summer here it is very dry and hot - more than 23 degrees; In winter the temperature drops to 21. The southern tropics are cooler and wetter, as the water area here is expanding. Moderate latitudes are a zone of sharp annual temperature differences (in both hemispheres). In summer, it's hot in the tropics, and in the winter the thermometer drops to +5 and below. The Arctic zone is characterized by temperature differences by a difference of 20 degrees. In winter the ocean freezes here, in summer the temperature rises to 3-5 above zero. The coldest region is the Antarctic zone. Here, the climate of the Atlantic Ocean goes into the polar, so the annual difference is more than 30 degrees.

Humidity and latitudinal zoning

Each strip of the Atlantic has its own special pressure. Thanks to him, the zones of highs and lows that form clouds and a nebula over the waters are singled out. These indicators influence on what climate in the Atlantic Ocean will form over one or another part of it. Equator - a zone of low pressure, that is a minimum. There is a maximum of precipitation - from 3000 mm per year, most of which falls on the summer. In winter fogs are often formed. The northern tropics and temperate latitudes form a zone of the Azores maximum. Precipitation here is very small - an average of 750 mm, but often trade winds and stronger winds that form a tornado and storms. Below the equator is the area of the South Atlantic peak. Here the pressure is also high, but rains happen much more often (up to 1000 mm), due to fewer winds. Antarctica and the Arctic are two minimum zones. Precipitation average is 2000 mm, the regions are stable against winds.

Features of the Atlantic Ocean Climate

In addition to the fact that the northern part of the Gulf Stream is much warmer than the southern one, the differences in temperature are also traced in some areas between the West and the East. Between 30 degrees north latitude and 30 degrees south latitude, the ocean water is warmer near the shores of America than near Africa. This is caused by the same trade winds that fall on the tropical and subtropical strips. They blow from the coast of Africa, bringing with them not only the sand of the Sahara, but also the sharp daily fluctuations in temperature that can be traced in the desert. Because of this, the water cools, waves often rise in it. Also, such winds do not allow clouds to gather to balance the humidity in the air. The closer to the West, the more calm the trade winds become. Sometimes there are storms, but in general the water is warmer, and the air temperature is much higher than in the East.

Summarizing

The climate of the Atlantic Ocean is a mix that includes ice expanses that freeze for half a year, and hot equatorial territories where it is always very warm and humid.