2. Using the temperature controls from the instruction, what explains the different temperature patterns of Louisville, Kentucky and Fairbanks, Alaska based on the weather experienced throughout the year shown on their climographs?3.A parcel of air is being forced up the windward side of a 7,000-foot-high mountain. The parcel has a temperature of 91.0F at 0 feet in elevation. If the LCL is located at 5,000 feet, what is the temperature of this parcel of air at 1,000 feet?You must show your work, using the equation in the instructions, in order to receive full credit.4. What is the temperature of the parcel of air, detailed in question 3, at the LCL (5,000 feet)?
You must show your work, using the equation in the instructions, in order to receive full credit.5. What is the temperature of the parcel of air, detailed in question 3, at the top of the mountain (7,000 feet)?
You must show your work, using the equation in the instructions, in order to receive full credit.6. After the parcel of air has descended down the leeward side of the mountain to sea level, what is the temperature of the parcel?
You must show your work, using the equation in the instructions, in order to receive full credit.7. Using the saturation mixing ratio table from the instruction, what is the capacity (saturated mixing ratio) of the parcel of air at 2,000 feet on the windward side of the mountain (estimate the value as needed)?8. Assuming the mixing ratio of the parcel of air at 2,000 feet is 10.0 g/kg, what it is the relative humidity of the parcel in percent?
You must show your work in order to receive full credit.9. Assuming the mixing ratio of the parcel of air on the leeward side of the mountain is 8.9 g/kg, and that no additional water vapor is added to parcel of air, does the relative humidity increase or decrease as it descends the mountain? Explain.
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