Exam 7: Water and Atmospheric Moisture

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Hydrogen bonding results from the fact that

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Relative humidity is not affected by changes in temperature or pressure.

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When water freezes, its density

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In which of the following months would the relative humidity likely be the highest (assuming a Northern Hemisphere station).

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The bulk of the evaporation on Earth occurs over the continents.

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List and describe the cloud classes and their associated cloud types, along with a discussion of the type of weather associated with each.

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If you visited Mount Shasta City (elevation 900 m [3000 ft.]) and found the outside air temperature to be 27°C (81°F), what would be the air temperature at the summit of Mount Shasta (elevation 4200 m [14,000 ft.]) at that moment-assuming that the temperature conditions with altitude change at an average, or normal, lapse rate?

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The difference between the dry adiabatic rate and the moist adiabatic rate is on account of

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The moist adiabatic rate (MAR) is less than the dry adiabatic rate (DAR) because of the release of the latent heat of condensation within the rising parcel of air.

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Clouds that have vertical development and produce thunderstorms are called

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When water freezes, its volume

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Unstable conditions are produced when the environmental lapse rate is greater than the dry adiabatic rate.

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Which of the following is used to measure relative humidity?

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When the environmental lapse rate is between the dry and moist adiabatic lapse rates conditions are described as

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Below a temperature of 4°C (39°F), water expands as it continues to cool.

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Water movement through the soil and water held in a cylindrical tube result from a common phenomenon. What is this phenomenon?

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The latent heat of melting and the latent heat of freezing involve the absorption or release of ________ calories per gram of water changing state.

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The process of deposition in the atmosphere produces

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Areas between 25° to 35° latitude usually become ________ because this area is dominated by air that is sinking and being ________.

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The average moist adiabatic rate is 6 C°/1000 m (3.3 F°/1000 ft), but values actually vary as a function of both temperature and moisture content.

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