The saturation curve show us... How much water vapor can be held in a parcel of

Question

The saturation curve show us... How much water vapor can be held in a parcel of air at a given temperature How much dew we will have at the dew point temperature The level to which we must rise before condensation Localized pressure systems A 30 C parcel of air at sea level which is saturated, rises to an altitude of 2.000 meters. What is it temperature at 2,000 m? 18C 48 C 10 40 C A saturated parcel of air has a temperature of 10 C t 4,000m.What is its temperature if it descends to an elevation of 1,000m 40C 0 C 28C -20 C Sea breezes and land breezes are caused by temperature differences between land and water global wind patterns pressure cells the Greenhouse effect A______ is the result of water being sucked up into the low pressure vacuum of a tropical cyclone, and then hitting land at levels up to 25 feet above normal high tides Storm Tornado Typhoon Tsunami A parcel of air with a temperature of 40 degrees C at sea level, which is not saturated, rises to an altitude of 3,000 meters where it is still not saturated. What is temperature? 10 C 0 C 27 C 22 C

Explanation / Answer

12- option a-how much air can be help in a parcel of air at a given temperature.

Q. Sea breeze and land breeze are caused by :

ans -temperature difference between land and water

25- option a-storm surge

18- option c- 28 C

17- option a -18 C

16-option a-10 C

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