Presentation on theme: "Chapter 7 Water and Atmospheric Moisture Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen."— Presentation transcript:
Chapter 7 Water and Atmospheric Moisture Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen
Water and Atmospheric Moisture TOPICS: Adiabatic Processes Atmospheric Stability Clouds Fog
Adiabatic Processes Adiabatic processes Begins with a parcel of air Bouyancy caused initially by differences in (near) surface temperature Less dense, warmer air rises, more dense, colder air sinks, after which… Ascending or descending air will undergo changes in temperature with no exchange of heat. This is an adiabatic process.
Buoyancy Figure 7.15
Adiabatic Processes Adiabatic processes Normal lapse rate: the average decrease in temperature with increasing altitude Environmental lapse rate: the actual lapse rate at a particular place and time Ascending or descending air will undergo changes in temperature with no exchange of heat. This is an adiabatic process. Heat WAS exchanged = diabatic process.
Adiabatic Processes Figure 7.17
Adiabatic Processes Dry adiabatic rate (DAR) Also called the Dry Adiabatic Lapse Rate (DALR) 10 C°/ 1000 m 5.5 F°/ 1000 ft Lifting Condensation Level (LCL) is reached, then… Moist adiabatic rate (MAR) Also called the Wet Adiabatic Lapse Rate (WALR) 6 C°/ 1000 m 3.3 F°/ 1000 ft
Atmospheric Stability Figure 7.20
Atmospheric Stability Stable and unstable atmospheric conditions Involves a parcel of air and its surrounding environment in the atmosphere Stable atmosphere: A parcel of air is discouraged from rising Kind of weather normally associated? Unstable atmosphere: A parcel of air is encouraged to rise Kind of weather normally associated?
Examples of Stability Figure 7.20 Unstable Atmosphere Parcel of air is encouraged to rise
Examples of Stability Figure 7.20 Stable Atmosphere Parcel of air is discouraged from rising
Atmospheric Stability To determine atmospheric stability: Compare the ELR with the DAR (or DALR) and MAR (or WALR) If ELR < MAR < DAR = STABLE If ELR > DAR > MAR = UNSTABLE If MAR < ELR < DAR = CONDITIONALLY UNSTABLE
Atmospheric Stability For example: We measure and find the ELR to be 12 Cº/ 1000 m We know the DAR is 10 Cº/ 1000 m. We know the MAR is 6 Cº/ 1000 m. If ELR (12) > DAR (10) > MAR (6) then? If ELR > DAR > MAR = UNSTABLE
Atmospheric Stability If ELR is large (shallow slope), it will be to the left of both the DAR and MAR lines This describes unstable atmospheric conditions! If ELR is small (steep slope), it will be to the right of both the DAR and MAR lines. This describes stable atmospheric conditions!
Atmospheric Temperatures and Stability Figure 7.19 ELR
Moisture Droplets Figure 7.20
Raindrop and Snowflake Formation Figure 7.22 Collision-coalescence process Bergeron process
Cloud Types and Identification Figure
Cirrus Figure 7.23
Cirrostratus Figure 7.23
Cirrocumulus Figure 7.23
Stratus Figure 7.23
Nimbostratus Figure 7.23
Stratocumulus Figure 7.23
Cumulus Figure 7.23
Cumulonimbus Figure 7.23
Cumulonimbus Development Figure 7.24
Fog Fog – a cloud layer at or very close to the surface formed when surface air temperatures and dewpt temperature are nearly identical Advection fog – warm, moist air layers moves over a cold surface Evaporation fog – dole air moves over warmer water body Radiation fog – loss of longwave radiation over moist surface
Advection Fog Figure 7.25 When warm, moist air moves over cooler body of water, what happens?
Evaporation Fog Figure 7.26 Cold air lies over warmer body of water, and evaporation from water surface causes saturation and fog. Also, sea smoke = hazard.
Figure 7.28 Radiation Fog Loss of longwave radiation at night over moist surface causes saturation.