EARTH 4 Lecture Notes - Lecture 11: Intertropical Convergence Zone, Horse Latitudes, Westerlies
Document Summary
Counterclockwise in northern hemisphere sta(cid:396)ti(cid:374)g at si(cid:374)gle (cid:862)(cid:272)ell(cid:863) (cid:373)odel topic 5 atmosphere. Buffalo disk = slower than quito disk northern hemisphere = deflected to right southern hemisphere = deflected to left o(cid:272)ea(cid:374) (cid:272)u(cid:396)(cid:396)e(cid:374)ts a(cid:396)e (cid:374)a(cid:373)ed fo(cid:396) whe(cid:396)e they"(cid:396)e goi(cid:374)g at(cid:373)osphe(cid:396)i(cid:272) wi(cid:374)ds a(cid:396)e (cid:374)a(cid:373)ed fo(cid:396) the di(cid:396)e(cid:272)tio(cid:374) they"(cid:396)e (cid:272)o(cid:373)i(cid:374)g f(cid:396)o(cid:373) Doldrums = lack of wind itcz intertropical convergence zone, zone between the tropics where winds come together or converge, it can occur north or south of the equator, where heat meets halfway depending on season. Horse latitudes between westerlies and trade winds throw horses off ship because no wind and no ability to move. Pollutants are transported by winds to other parts of the world. Carbon dioxide accumulates in atmosphere, higher contribution each year, contributing to rising global temperatures, nasa satellite view of carbon dioxide in atmosphere. --differential heating monsoons: first picture = dry winds, second picture = warm wet air winds.
