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9/29/2010 GEOG 1001: Clouds and Lifting September 30th, 2010 Dr. Bob Ross Last time • Polarity of water molecule and strength of hydrogen bond. • Phase changes. • Relative Humidity (changes with temperature) • Atmospheric Stability (ELR VS DAR and MAR) ©2010 American Public Television & Old Post Productions Clouds and Fog • Cloud Formation Processes • Cloud Types and Identification • Fog Cloud Formation Processes • Moisture droplet • Cloud-condensation nuclei 1 9/29/2010 Raindrop and Snowflake Formation Moisture Droplets Figure 7.21 Figure 7.20 Cloud Types and Identification Cirrus Bright and fluffy clouds Low clouds Figure 7.22 Figure 7.22 2 9/29/2010 Cirrostratus Altocumulus Figure 7.22 Altostratus Figure 7.22 Nimbostratus Figure 7.22 Figure 7.22 3 9/29/2010 Stratus Cumulus Figure 7.22 Cumulonimbus Figure 7.22 Cumulonimbus Development Figure 7.22 Figure 7.23 4 9/29/2010 Advection Fog Fog • Fog is a cloud layer on the ground; several types: • Advection fog (warm air moves over cold) • Evaporation fog • Upslope fog • Valley fog • Radiation fog Figure 7.24 Evaporation Fog Valley Fog Figure 7.25 Figure 7.25 Figure 7.26 5 9/29/2010 Atmospheric Lifting Mechanisms Atmospheric Lifting Mechanisms • • • • Convergent Lifting Convectional Lifting Orographic Lifting Frontal Lifting (Cold and Warm Fronts) Figure 8.6 Orographic Precipitation Convection over Florida Figure 8.8 Figure 8.9 6 9/29/2010 Orographic Patterns Frontal Lifting • Cold Fronts – Cold air forces warm air aloft – 400 km wide (250 mi) • Warm Fronts – Warm air moves up and over cold air – 1000 km wide (600 mi) Increased precipitation intensity Increased precipitation frequency Figure 8.10 Cold Frontal Lifting Warm Front Figure 8.11 Figure 8.13 7 9/29/2010 Summary • Cloud formation • Cloud types • Atmospheric lifting – Convergent Lifting – Convectional Lifting – Orographic Lifting – Frontal Lifting (Cold and Warm Fronts) 8