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CONDENSATION. Chapter 17 Test 4 material End. CLOUDS ARE THE VISIBLE PRODUCTS OF CONDENSATION AND DEPOSITION WITHIN THE ATMOSPHERE. WE NEED A NUCLEI AS A SURFACE FOR CONDENSATION TO TAKE PLACE. CONDENSATION NUCLEI. FOREST FIRES VOLCANOES WIND EROSION SEA WAVES POLLEN CHIMNEY SMOKE.
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CONDENSATION Chapter 17 Test 4 material End
CLOUDS ARE THE VISIBLE PRODUCTS OF CONDENSATION AND DEPOSITION WITHIN THE ATMOSPHERE. • WE NEED A NUCLEI AS A SURFACE FOR CONDENSATION TO TAKE PLACE
CONDENSATION NUCLEI • FOREST FIRES • VOLCANOES • WIND EROSION • SEA WAVES • POLLEN • CHIMNEY SMOKE
CLOUDS • ARE VISIBLE EVIDENCE OF MOISTURE WITHIN THE ATMOSPHERE • CLASSIFIED BY THEIR APPEARANCE AND THEIR ALTITUDE ABOVE THE SURFACE
BY APPEARANCE • CIRRUS OR CIRRO = FEATHERY • STRATUS OR STRATO = LAYERED • CUMULUS OR CUMULO = PUFFY • NIMBO OR NIMBUS = RAIN • FRACTO OR FRACTUS = BROKEN
HIGH CLOUDS • FOUND AT ALTITUDES ABOVE 20,000 FEET • TEMPERATURES ARE SO LOW THAT CLOUDS ARE COMPOSED SOLELY OF ICE CRYSTALS • PREFIX CIRRO DENOTES HIGH CLOUD
TYPES OF HIGH CLOUDS • CIRRUS - ALSO CALLED MARE’S TAILS BECAUSE THEY LOOK LIKE STRANDS OF HORSE HAIR
HIGH CLOUD • CIRROSTRATUS - ARE NEARLY TRANSPARENT SO THAT SUN OR MOON SHINES THROUGH • OFTEN SEE HALO AROUND THEM WHICH CAN BE PREDICTOR OF RAIN BECAUSE THESE ARE CLOUDS SEEN PRECEDING A WARM FRONT
HIGH CLOUD • CIRROCUMULUS - CONSIST OF SMALL WHITE PUFFS ARRANGED IN A WAVELIKE PATTERN • CALLED A MACKERAL SKY BECAUSE IT LOOKS SIMILAR TO FISH SCALES
MIDDLE CLOUDS • HAVE A BASE BETWEEN 6,500 TO 20,000 FEET ABOVE THE SURFACE • COMPOSED OF ICE CRYSTALS OR SUPERCOOLED WATER DROPLETS OR BOTH • PREFIX ALTO IS USED TO DENOTE MIDDLE CLOUD
MIDDLE CLOUDS • ALTO STRATUS - UNIFORMLY GRAY OR WHITE AND USUALLY SO THICK THAT SUN IS DIMLY VISIBLE (SAID TO LOOK LIKE FROSTED GLASS) • CAN DISTINGUISH THESE FROM CIRRO STRATUS (SHADOW ON GROUND) BECAUSE THERE WOULD BE NO SHADOW
MIDDLE CLOUDS • ALTOCUMULUS - CONSIST OF PATCHES THAT FORM LINES OR WAVES • HAVE LARGER SIZE AND SHARPER FEATURES THAN CIRROCUMULUS
LOW CLOUDS • HAVE BASES FROM THE EARTH SURFACE (FOG) TO 6,500 FEET ABOVE SURFACE • COMPOSED OF WATER DROPLETS • NO PREFIX DESIGNATION
LOW CLOUDS • STRATOCUMULUS - CONSIST OF LARGE PUFFS ARRANGED IN LAYERS • NIMBOSTRATUS - DARK GRAY CLOUDS THAT GO FROM HORIZON TO HORIZON AND CONTAIN PRECIPITATION
LOW CLOUDS • STRATUS - OCCUR AS A UNIFORM GRAY LAYER THAT STRECHES FROM HORIZON TO HORIZON • MAY GET DRIZZLE FROM THESE CLOUDS
FOGS • ADVECTION - WARM MOIST AIR OVER A WATER SURFACE BLOWS OVER A COOLER LAND SURFACE (ALSO KNOWN AS COASTAL FOG) • RADIATION - DUE TO NIGHT-TIME RADIATIONAL COOLING. FOUND IN LOW-LYING AREAS AND BURNS OFF BY AM
FOGS • FRONTAL - DUE TO UPLIFTING OF AIR ALONG THE PASSAGE OF FRONTS. CAN BE WIDESPREAD AND LONG LASTING. • UPSLOPE - OCCURS AS AIR MOVES UP A SLOPE. SMOKEY MOUNTAINS
FOGS • STEAM - ALSO KNOWN AS EVAPORATION FOG. FOUND OVER WATERBODIES IN FALL OR EARLY WINTER AS WATER TEMPERATURE IS HIGHER THAN SURFACE AIR TEMPERATURES
CLOUDS OF VERTICAL DEVELOPMENT • CUMULUS - OCCURS AS AIR RISES VERTICALLY TO ABOUT 3000-6500 FEET. • RESEMBLE PUFFS OR COTTON BALLS • CAN GO THROUGH STAGES OF VERTICAL DEVELOPMENT AS UNSTABLE AIR RISES • CUMULONIMBUS
UNUSUAL CLOUDS • ALTOCUMULUS LENTICULARIS - ALSO KNOWN AS LENTICULAR CLOUD AND FOUND NEAR MOUNTAIN RANGES. • BANNER - DRAPED OVER THE TOP OF MOUNTAIN LIKE A FLAG • CONTRAIL
TYPES OF PRECIPITATION • VIRGA • MIST • DRIZZLE - STRATUS • RAIN - NIMBOSTRATUS OR CUMULONIMBUS • FREEZING RAIN (GLAZE)
SLEET • SNOW • HAIL
HOW DOES IT RAIN? • COLLISION-COALESCENCE • BERGERON PROCESS
SNOW • HEXAGONAL • NEEDLES • DENDRITES • PLATES • COLUMNS • SIZE DEPENDS UPON TEMPERATURE • TOO COLD OR TOO WARM? • 10 INCHES SNOW= 1 INCH RAIN
HAIL • RANGE IN SIZE FROM A PEA TO AS LARGE AS A GRAPEFRUIT • 2 POUNDS AND AS LARGE AS A SOFTBALL • SOMETIMES USE SNOWPLOWS TO CLEAR HAIL FROM HIGHWAYS (18 INCHES OF HAIL) IN GREAT PLAINS