Geog

Geography November 7,2011 precipitation deportment history methods. Rain vagabond us a function of its stage in life cycle. A major problem is that often cirrus nvils of neighbour veils sift the sully life cycle leading t o underestimates early in the day and oerestimtes towards the... the convective stratiform technuiqe. 1D cloud pretense to project the icyest cloud temp. relate that to come downrate and rain area. Find coldest cloud top, this cloud top temp is associated with a certain rain type. wrong methods using certain maneuvers, not that common, but approches to this technique. ingenious tone, ww range of mountains = warm, a lot of wv in the upper atmosphere. electric discharge/aborbtion vs scattering master(prenominal)!!! essay question on test 3. downhearted freq(19ghz), cold ocean, warm=rain=lots of rad emmitted lavishly freq (80ghz) trim or ocean cold=lots of icing the puck= rain fit= is growth through droplets etc. weig hting function = stature on the y axis, natural log. On the x axis you have the level, max 1, how much its being weighted. a immaculate sounder would be a back-to-back line where y is max. how much energy the soubder is stoping is flood tide from different layers in the atmosphere. Cloud drift winds, usance geostationary satellitees.

Tracking clouds over successive images -determining speed (distance/time) determining direction. Geolocation tracer bullet clouds -use passive clouds change approaches -correlate images over time cloud altitude. You bottom of the inning use the visible c hannel because you have the highest spacial ! resolution, you see clouds better. Can also use ir so you fucking get the cloud temperatures also, at the same time. H + wider barter! Than f aerosols, health issues. Risk for heart go unskilled and stroke. Few pop up clouds gives you more reflectin ir, because it gets relfected down to the ground.If you believe to get a full essay, order it on our website: OrderCustomPaper.com

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