Scan0007 - 3of3 Lu Ifme M “M...

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Unformatted text preview: 3of3 Lu... Ifme. M... “M “A"!nnnnlnIflnu-Ifivlntmnbimfrflrlannn‘l 'I ‘l 1 IT Ahh‘rf hflp:flwwwggynga.edu/people/ficuliylslnpldns/dir/GEOGI11Illecmr... Al also influence precipitation patterns xvation: ”351 . * 6b W {30 hiql'flr m dunflwwrmdg )Tadfimm @mg 4 3m, * mdéoitm fiehmflj \HUUP/W WM LEMTQW offal giddf WU daily, 76 Mfg, Cloud Cover & Albedo: ** clouds trap—in terrestrial radiation keeping the surface warmer, BUT also reflect solar radiation coming in * cloudy day vs clear day; cloudy night vs clear night (Know the differences in temps due to these situatioris.) a: CLW data is dead/W 0000M lhan 0c GLEN dag *mflaudfl Marie :6 1,23anng [1,3er than mm turgid *** Worldwide T° Patterns * variations controlled by the above factors * one of the key factors is that the proportion of land to water varies over the earth's surface ** Southern Hemisphere: 81% water, 19% land “F6 VflMOctlmé ‘9 range QUIZ smolLt/p ** Northern Hendsphere: 61% water, 39% land (93 3/323 122.) =e= mmfitr T b var-com m5 * grew;- mwija/r firm, Venetian “UL! [aim than W * coldest T°'s: over land at high latitudes in winter In I9 93 EX: Siberia & Antarctica CVOSiTOV, g i QHJ’O'K’WO, ,quc C- {3304:} * warmest T°'s: in the tropical deserts in summer E : Sahara X Unmet m M22 CS‘SOC C Lm\L OJ‘CT FOG/6 Bl P3 DA "118 '8123120119121PM \LDOWf-M- krms Wind Chill Indm Muted“ Haiti” 13M ...
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