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Type A climates are controlled mainly by the seasonal fluctuations of the trade winds, the intertropical convergence zone (ITCZ), and the Asian monsoon.
Type A climates (the warmest) are differentiated on the basis of the seasonality of precipitation: Af (no dry season), Am (short dry season), or Aw (winter dry season).
Köppen's A climates are found in a nearly unbroken belt around the Earth at low latitudes, mostly within 15° N and S. Their location within a region in which available net solar radiation is large and relatively constant from month to month ensures both high temperatures (generally in excess of 18 °C [64 °F]) and a virtual absence of thermal seasons.
Köppen specifies three A climates: Wet equatorial climate (Af) Tropical monsoon and trade-wind littoral climate (Am) Tropical wet-dry climate (Aw) Arid and semiarid climates cover about a quarter of Earth's land surface, mostly between 50° N and 50° S, but they are mainly found in the 15 30° latitude belt in both hemispheres.
Interestingly, all breeds from group 1, except KARM, are reared in SA or A climates, mainly from Asian regions.
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