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Cette carte conceptuelle, cree avec IHMC CmapTools, contient des informations liees a : Dust Storms, Dust Grains become Dust in Atmosphere, Positive Feedback arises because Dust in Atmosphere raises Temperature, "Great Dust Storms" are Highly Variable in Occurrence, Dust Storms have typical size of 100,000 to 500,000 km2, Strong Winds experience Positive Feedback, Global Scale Dust Storms are termed "Great Dust Storms", Dust Storms occur in All Seasons, Dust in Atmosphere absorbs Daytime Heat, Dust Storms typically, last A Few Days, Dust in Atmosphere raises Temperature and Increased Heating leads to Stronger Winds, Dust in Atmosphere subject to Nighttime Cooling, Dust Grains may be as large as Fine Soil (~100 microns), Dust Grains may be as small as One Micron, Global Scale Dust Storms remain Poorly Understood Phenomenon, Positive Feedback arises because Hot Air Rises, Highly Variable in Occurrence almost always occur during Southern Summer, Dust Devils were observed by Pathfinder Lander, Dust Storms include Dust Devils, Dust Devils are ~2 km in width, Strong Winds can raise Dust Grains