GEOG 272 Lecture Notes - Lecture 17: Supercooling, Sittwe, Transpiration
21 Nov 2017
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Lecture 17: climographs, so he(cid:396)e"s (cid:272)li(cid:373)og(cid:396)aph fo(cid:396) si(cid:374)gapo(cid:396)e. the (cid:272)li(cid:373)og(cid:396)aph depi(cid:272)ts te(cid:373)pe(cid:396)atu(cid:396)e , as the (cid:396)ed li(cid:374)e, a(cid:374)d precipitation, lower purple bars, for each month of the year, now here we see singapore. Rly high temperatures every month throughout the year. Air masses are satu(cid:396)ated, (cid:272)o(cid:374)tai(cid:374)i(cid:374)g huge a(cid:373)ou(cid:374)ts of (cid:448)apo(cid:396). So let"s see (cid:449)hat so(cid:396)t of a climate it is. Driest (cid:373)o(cid:374)th is (cid:1005)(cid:1011), so (cid:449)a(cid:455) off the (cid:373)ap. Polar of arctic cicrcle which is at 66. 5 degrees. And u can see here the temperature, as u expect rly cold te(cid:373)ps (cid:272)uz of the high latitude, lo(cid:449) i(cid:374)solatio(cid:374). (cid:1004) photope(cid:396)iod du(cid:396)i(cid:374)g pa(cid:396)t of the (cid:455)ea(cid:396). He(cid:396)e"s (cid:1004) degrees, avg temp would be -12, not a lot of precipitation for entire year. 12, 130mm. and probably more precipitation in summer. Summer precipitation, mean annual this formula defines the threshold between b climates and humid climates. If precipitation for our location is greater than this threshold value theres no aridity.
