climate
nounIn geography, a part of the surface of the earth, bounded by two circles parallel to the equator, and of such a breadth that the longest day in the parallel nearest the pole is half an hour longer than that nearest to the equator. The beginning of a climate is a parallel circle in which the longest day is half and hour shorter than that at the end. The climates begin at the equator, where the day is 12 hours long; and at the end of the first climate the longest day is 12 hours long, and this increase of half an hour constitutes a climate, to the polar circles; from which climates are measured by the increase of amonth.