GEOG102 Study Guide - Final Guide: Fluid Parcel, Dew Point, Latent Heat

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Heat is energy (cid:862) e(cid:374)si(cid:271)le(cid:863) heat or (cid:862)e(cid:374)thalp(cid:455)(cid:863: sense heat as transfer of energy from an object to or from our skin, heat is gained by absorption of energy, heat is lost by emission of energy. Temperature measures the average energy of motion of molecules in an object. Altitude (air cools with height, normally 1 c/100m: dry adiabatic lapse rate: high altitude has greater daily range, high altitude has lower annual average. Cloud cover: clouds have high albedo, clouds moderate temperatures. Marine temperatures: coastal regions have smaller daily and annual temperature ranges, e. g. Inland regions have greater daily and annual temperature ranges: e. g. Both cities have similar latitudes, about 49 n and 50 n, respectively. Vancouver has more moderate pattern of average maximum and minimum temperatures. Va(cid:374)(cid:272)ou(cid:448)er"s a(cid:374)(cid:374)ual ra(cid:374)ge of (cid:1005)(cid:1010) c is far less tha(cid:374) wi(cid:374)(cid:374)ipeg"s 38 c ra(cid:374)ge. Wi(cid:374)(cid:374)ipeg"s (cid:272)o(cid:374)ti(cid:374)e(cid:374)tal te(cid:373)perature patter(cid:374) is (cid:373)ore e(cid:454)tre(cid:373)e in every aspect than that of maritime vancouver.

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