The impact of Fohn winds is that it leads to rain shadows and more daytime warming.
<h3>What are Fohn winds?</h3>
These are dry and warm winds that are usually known to occur on the down side of mountainous areas.
The wind is usually known to be the cause of adiabatic air warming. The Foehn wind is usually descending.
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Himalayas, mountains include amount Everest and K2
Answer:
Explanation:
only by sails frequently get stuck as the "doldrums."
The doldrums are an area where there is little to no prevailing wind (historically known because it obviously cannot fill sails).
The other BLANK should be the location of the doldrums in degrees from the equator: 5 degrees north to five degrees south of the equator.
The factor that affect heat transfer between a warm and a cool substance is the amount of time of contact, the area of contact, and the specific heats of the substances.
<h3>Which factors affect heat transfer between?</h3>
A lot of Experiment have shown that the heat transferred to and also from a substance is based on:
- The change in the substance's temperature
- The mass of the substance.
- Some physical properties linked to the phase of the substance.
Hence, The factor that affect heat transfer between a warm and a cool substance is the amount of time of contact, the area of contact, and the specific heats of the substances.
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