Capitolo 4
sun that burns some equator, the evaporation of water necessarily has to go
above with rapidity immensely greater than in the coldest zones and all the
water that you/he/she is taken on it owes, comes down clearly again.
It is not completely however, from the latitude of the region in that the
evaporation has place that the pluvius quantity from which it falls the
atmosphere is determined; for the condition on that the fall back,
in the rain, of the water that you/he/she has been taken on mainly from evaporation
it depends, it is the cooling of the atmospheric stratum that contains him/it;
and this effect is produced in ways very various, and very different
causes operate to change him/it. The stratum is sometimes refreshed being
diffused on series of mountains, sometimes meeting and becoming
mixed with current fresher than air; and sometimes, again, being
driven in winds toward a taller, and, accordingly, fresher latitude. If,
on the other hand air it stirs from mountains cold verse you heat and statement to the sun
plain, or from taller latitudes to lower, or if, among the various one
current in which falls, it is mixed with air warmer than
it, its ability to contain vapor in solution is increased and,
accordingly, instead of releasing his/her taking on the waters that it has
it becomes already in possession, thirsty for. It stirs on a
country, under these circumstances as a heat and drying wind. Under a
opposite of circumstances you/he/she would have formed going adrift fogs, or,
perhaps, also pluvius plentiful showers.
It will be evident from these considerations that the frequency of the,
showers and the quantity of the rain that it will fall, in the various one
regions respectively what the surface of the earth introduces, owes
depends on the influence combined of a lot of causes as the heat of
the climate, the proximity and the direction of mountains and seas,
the character of the prevailing winds and the reflecting qualities of
the ground. These and the other similar causes, are found, face, in fact,