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The Atlantic ITCZ is very sensitive to even small changes in the interhemispheric SST gradient due to the fact that tropical SSTs are very uniform in magnitude throughout the equatorial region between 10 °S-5 °N. Therefore, even a small change in the SST field can cause a significant impact on the position and displacement of the ITCZ.
The equatorial region near the Intertropical Convergence Zone (ITCZ), or monsoon trough, is the wettest part of the world's continents. Annually, the rain belt within the tropics marches northward by August, then moves back southwards into the Southern Hemisphere by February and March.
This region is known as the Intertropical Convergence Zone. This zone is the result of trade winds from the northern and southern part of the hemisphere eventually joining together. [1] Still another definition states that the thermal equator is the latitude at which insolation is identical throughout the year.
The ring current system consists of a band, at a distance of 3 to 8 R E, [1] which lies in the equatorial plane and circulates clockwise around the Earth (when viewed from the north). The particles of this region produce a magnetic field in opposition to the Earth's magnetic field and so an Earthly observer would observe a decrease in the ...
The equatorial zone has 4 seasons 2 dry and 2 wet. [2] The equatorial zone It is characterized by abundant rainfall (more than 1,000 mm of rainfall per year) and especially by the absence of a dry season: we speak here of "dry seasons" for the periods when it rains less (December–January, then July–August, with local variations).
The latitude of the Earth's equator is, by definition, 0° (zero degrees) of arc.The equator is one of the five notable circles of latitude on Earth; the other four are the two polar circles (the Arctic Circle and the Antarctic Circle) and the two tropical circles (the Tropic of Cancer and the Tropic of Capricorn).