Answer:
C. dry adiabatic lapse rate
Explanation:
- When a parcel of air cools down its due to the rising from the adiabatic lapse rate processes. At a rate of 10 C/Km as the dry adiabatic lapses rate minuses the heat added by the latent heat of condensation.
- This the parcel of air has to expand and then cool and thus its density gets reduced. Thus occurs as the air pressure decreases the parcel with an increase in height.
Answer:
The difference between the given topics is described below.
Explanation:
<u>Slope decline</u>:
- The decline has been characterized as anything being rejected, downhill, diminished, or sinking from perspective. Somebody else says anything when approached for supper would be an illustration of decline.
<u>Slope retreat</u>:
- The gradual retreat of something like a scarp or perhaps the mountainous slope has been considered as an explanation for the erosion of backward as well as downwards.
Rainfall and temperature can affect the rate in which rocks weather. High temperatures and greater rainfall increase the rate of chemical weathering. Minerals in a rock buried in soil will therefore break down more rapidly than minerals in a rock that is exposed to air.
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