precipitation
life history methods.
Rain rate us a function of its stage in life cycle. A major problem is that often cirrus nvils of neighboring veils sift the cloud life cycle leading t o underestimates early in the day and oerestimtes towards the...
the convective stratiform technuiqe. 1D cloud model to project the icyest cloud temp. relate that to rainrate 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.
Bright tone, ww range of mountains = warm, a lot of wv in the upper atmosphere.
Emission/aborbtion vs scattering
master(prenominal)!!! essay question on test 3.
low freq(19ghz), cold ocean, warm=rain=lots of rad emmitted
high freq (80ghz) trim or ocean cold=lots of ice= rain
fit= is growth through droplets etc.
weighting 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 straight line where y is max. how much energy the soubder is seeing is coming 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 can use the visible channel because you have the highest spacial resolution, you see clouds better. Can also use ir so you can get the cloud temperatures also, at the same time.
H
+ wider swap! Than f
aerosols, health issues. Risk for heart go bad and stroke.
Few pop up clouds gives you more reflectin ir, because it gets relfected down to the ground.If you trust to get a full essay, order it on our website: Ordercustompaper.com
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