Merchant, F. W. (Francis Walter), 1855-1937, Chant, Clarence Augustus, 1865-1956 · Toronto : Copp Clark · leaf 163
nt of its higher capacity for heat, water warms and cools much more slowly than land. For this reason the sea is frequently cooler by day and warmer by night than the surrounding land. Hence, if there are no dis- turbino forces an ofi-sea Fig. 17-2.—Illustration of land and sea breezes. A,- °. ,.,… … Fig 171.—Convection cur-rents in heated air.
Physics
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