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ISU GEO 211 - Chapter 6- Stability and Cloud development
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GEO 211 1st Edition Lecture 15Outline of Last Lecture I. Cloud classification (based on form and height)A. Latin Words used in the classification:1. Stratus2. Cumulus3. Cirrus4. Alto5. NimbusB. Height of cloudsC. 10 common cloud types (4 groups) table 5.2- High clouds1. Cirrus (Ci) 2. Cirrocumulus (Cc) 3. Cirrostratus (Cs) - Middle clouds1. Altocumulus (Ac) 2. Altostratus (As) \- Low clouds1. Stratus (St) 2. Stratocumulus (Sc) 3. Nimbostratus (Ns)Outline of Current Lecture II. Chapter 6- Stability and Cloud developmentA. What is adiabatic process?B. Adiabatic coolingC. Adiabatic warmingD. Adiabatic processE. Adiabatic ratesF. Dry adiabatic lapse rate:G. Moist adiabatic lapse rateH. Non-Adiabatic ratesThese notes represent a detailed interpretation of the professor’s lecture. GradeBuddy is best used as a supplement to your own notes, not as a substitute.I. Rate of decrease of an air temperature (static air) with elevationCurrent LectureII. Chapter 6- Stability and Cloud developmentA. What is adiabatic process?- Rising in air parcel EXPANDS- Expansion is due to decrease of pressure with altitude- Expanded rising air COOLSB. Adiabatic cooling- Cooling that is taking place within the air parcel without losing its heat to surroundingsC. Adiabatic warming- Compressed sinking air warms- Warming takes place within the parcel without drawing heat from the surroundings D. Adiabatic process- Expanding and cooling or compressing and warming of air with no interchange ofheat with its surroundingsE. Adiabatic rates- Every 1000 feet temperature drops a certain amount (constant)- Dry adiabatic rate (DALR)- Moist adiabatic rate (MALR)F. Dry adiabatic lapse rate:- Rate of change in temperature in a rising or descending unsaturated air parcel only 15.5° F/1000 feetG. Moist adiabatic lapse rate- Rate of change in temperature in a rising or descending saturated air parcel- Varies- but always less than 5.5°F/1000 feetH. Non-Adiabatic rates- Environmental lapse rateI. Rate of decrease of an air temperature (static air) with elevation- 3.5°F/1000 feet- Dew point lapse rate- Rate of change of dew point temperature 1°F/1000


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ISU GEO 211 - Chapter 6- Stability and Cloud development

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