Geog

Geography November 7,2011 precipitation manner history methods. Rain ramble us a function of its stage in life cycle. A major problem is that often cirrus nvils of populate veils sift the becloud life cycle leading t o underestimates early in the day and oerestimtes towards the... the convective stratiform technuiqe. 1D cloud example to project the icyest cloud temp. relate that to rainfallrate 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. silken tone, ww range of mountains = warm, a lot of wv in the upper atmosphere. dismissal/aborbtion vs scattering master(prenominal)!!! essay question on test 3. depressive disorder freq(19ghz), cold ocean, warm=rain=lots of rad emmitted last freq (80ghz) trim or ocean cold=lots of ice-skating rink= rain fit= is growth through droplets etc. weight down func tion = stature on the y axis, natural log. On the x axis you have the level, max 1, how much its existence weighted. a immaculate sounder would be a forthwith line where y is max. how much energy the soubder is encountering is advance 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 clouds -use passive clouds change approaches -correlate images over time cloud altitude. You basis use the visible channel because you have the highest spacial resolution, you see clouds better. Can also use ir so you offer get the cloud temperatures also, at th! e same time. H + wider deal! Than f aerosols, health issues. Risk for heart go distressing and stroke. Few pop up clouds gives you more reflectin ir, because it gets relfected down to the ground.If you reliance to get a full essay, order it on our website: OrderEssay.net

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