Calculate parcel temperatures for all windward and lee-side


This short paper provides you an opportunity to apply the information introduced in Module Three.

Prompt:

For this assignment, you will trace the path of a hypothetical parcel as it moves over a mountain. You will assume the mountain base to be at sea level on both sides with a peak of 3,000 meters (m) and that the initial parcel conditions include a temperature of 10 °Celsius and a lifting condensation level (LCL) of 1,000 m. Be sure to provide a written explanation of all your calculations.

Specifically, the following critical elements must be addressed:

- Calculate parcel temperatures for all windward and lee-side levels and explain your calculations.

- What would happen to the parcel (size, Ta, relative humidity [RH]), and how would it change as it ascends the windward side and descends the lee side? What would the parcel temperature be at 1,000 m on the windward side, at the peak, 1,000 m on the lee side, and at the lee base? Why would the temperatures be different at the same levels on each side of the mountain?

Guidelines for Submission: Your assignment must be submitted as a one-page Word document, with double spacing, 12-point Times New Roman font, one-inch margins, and all sources used cited in APA format.

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Science: Calculate parcel temperatures for all windward and lee-side
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This paper has been prepare for mountain behavior while air moves from sea level to the peak level of the mountain. In this paper, there are discussion about the characteristics of air at windward side and leeward side of mountain. The air get cooler when moves form windward side and the air get more density when it moves from peak of mountain to sea level of the mountain due to warm of air. This paper is prepare in Microsoft word file.

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