8. (a) Assuming that no water vapor is added as the parcel descendsdown the lee side of the mountain to sea level, is the water vaporcontent (the mixing ratio) of the parcel higher or lower thanbefore it began to rise over the mountain? (b) Why? (c) What is the lifting condensation level of this parcel now?

answer is given below

Explanation:

there are 3 characteristics  that stability of the atmospheric layer that parcel of air is embedded are

The temperature lapse rate through the layer Temperature of the parcel at its initial levelInitial dew point of the parcel

When a portion of the air descends toward the mountain's leeward side, the humidity in the air is low, forcing the air up the mountain, causing the air to cool and reach the ice point, resulting in a maximum of air and then ascending to a higher mountain, such as clouds (rain / snow) Humidity comes out of it. Then when the mass of the same wind comes down the mountain, the air dries more

This is all you, but i can give you some topics that you could try. if it rained when you want to do something outdoors, it 'limits' that human activity. maybe you want to do an experiment that goes throughout the whole year and you have to have above freezing the entire year. this 'limits' your activity. i thought of those just off of the top of my head. something that gets to me that might be getting to you is you are thinking too hard about what to do. think simply, and if it is too simple, then bump it up just a little bit.

El nino is a weather phenomenon caused when warm water from the western pacific ocean flows eastward. part1baan average of 7.7 hurricanes and 3.6 major hurricanes compares to 5 hurricanes and 1.5 major hurricanes from 1995-2005