Moisture in the Atmosphere. Assignment 3. Due February 10
Purpose: assess impact of ascent and descent upon parcel properties as a function of parcel theory assumptions .
- This assignment uses your laminated Skew-T diagram.
- 1. A parcel is lifted adiabatically beginning from a temperature of 10C at 900 mb. It's dewpoint is 5C.
- a. Determine the parcel's temperature, dewpoint, and mixing ratio when it is lifted to 850 mb. 700 mb. 500 mb.
- b. What is the pressure, temperature, dewpoint, mixing ratio and RH at the LCL?
- c. What is the parcel's initial wet bulb temperature? Potential temperature? wet bulb potential temperature? equivalent temperature? Equivalent potential temperature?
- d. What is the parcel's web bulb temperature, potential temperature, wet bulb potential temperature, equivalent potential temperature, equivalent temperature at 850 mb, 700 mb, 500 mb?
- e. After the parcel descends back down from 500 mb to 900 mb, what are the values of the quantities in a and d?
- 2. A parcel is lifted adiabatically to the top of the atmosphere beginning from a temperature of 10C at 900 mb. Its dewpoint is 5C. As it ascends all the water vapor that condenses falls out of the parcel. Repeat a-e.
- 3. A parcel is lifted to 500 mb adiabatically beginning from a temperature of 10C at 900 mb. Its dewpoint is 5C.
As it ascends, 20% of the water vapor that condenses fall out of the parcel. Repeat a-e.