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ÖÖI 8x 3 ^c- 0 - Acehbooks.org

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%6<br />

S U M A T R A .<br />

center being intenfe, a violent current of air may be perceived to force<br />

its way in, through doors or crevices, on oppofite fides of the houfe.<br />

As the general winds are caufed by the direiï influence of the fun's<br />

rays upon the atmofphere, that particular deviation of the current, diftinguilhed<br />

by the name of land and fea breezes, is caufed by the influence<br />

of his refljfied rays, returned from the earth or fea on which<br />

they ftrike. The furface of the earth is more fuddenly heated by the<br />

rays of the fun, than that of the fea, from its greater denfity and ftate of<br />

reft; confequently it reflects thofe rays fooner and with more power :<br />

but owing alfo to its denfity, the heat is more fuperficial than that imbibed<br />

by the fea, which gets more intimately warmed, by its tranfparency,<br />

and by its motion, continually prefenting a frefh furface to the<br />

fun. I fhall now endeavour to apply thefe principles. By the time the<br />

rifing fun has afcended to the height of thirty or forty degrees above<br />

the horizon, the earth has acquired, and reflected on the body of air<br />

fituated over it, a degree of heat fufficient to rarefy it and deftroy its<br />

equilibrium; in conlequence of which, the body of air above the fea,<br />

not being equally, or fcarce at all rarefied, rufhes towards the land ; and<br />

the fame caufes operating fo long as the fun continues above the horizon,<br />

a conftant fea breeze, or current of air from fea to land, prevails during<br />

that time. From about an hour before fun fet, the furface of the earth,<br />

begins to lofe faft the heat it has acquired from the more perpendicular<br />

rays. That influence of courfe ceafes, and a calm fucceeds. The warmth<br />

imparted to the fea, not fo violent as that of the land, but more deeply<br />

imbibed, and confequently more permanent, now acts in turn, and by<br />

the rarefaction it caufes, draws towards its region, the land air,, grown<br />

cooler, more denfe and heavy, which continues thus to flow back, till<br />

the earth, by a renovation of its heat in the morning, once more obtains<br />

the afcendancy. Such is the general rule, conformable with experience,<br />

and founded, as kfeemsto me, in the laws of motion, and the nature of<br />

things. The following obfervations will ferve to corroborate what I<br />

have advanced, and to throw additional light on the fubject, for the information<br />

and guidance of any future inveftigator. *<br />

.<br />

The

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