GEG 2304 Lecture Notes - Lecture 6: Longwave, Shortwave Radio, Heat Flux

• School: University of Ottawa
• Department: Geography
• Course: GEG 2304
• Professor: Conrad

Document Summary

The chapter 3 will not be on the quiz. Latent are evaporating water into the same air. The ocean is always warmer in the winter than the land is and in the summer time it is the opposite. This is because in the winter the snow has such a high albedo there is little radiation that is absorbed not allowing the land to warm. This is a result of the local energy balance modified by the wind. The ocean currents: do the same thing as the atmosphere. Bring warmer water northwards and bringing colder water southwards. This just takes longer then the atmosphere moves around air. More radiation in the tropical region the(cid:374) i(cid:374) the polar regio(cid:374)s. the earth"s surfa(cid:272)e loses radiatio(cid:374) to lo(cid:374)g (cid:449)a(cid:448)es. The lo(cid:374)g (cid:449)a(cid:448)es do(cid:374)"t (cid:272)ha(cid:374)ge (cid:373)u(cid:272)h fro(cid:373) lo(cid:374)g to lat. Lo(cid:374)g (cid:449)a(cid:448)e radiation is a function of temperature. Large incoming solar radiation until about 40 degree lat.