Answer:
D In the US, mid-latitude cyclones often form over the Gulf of Mexico
Explanation:
- From the polar front theory, it can be asserted that in the mid-latitude there exist a boundary of cold dry air CP to the north and warm moist air to the south. The mid-latitude cyclone that develops has a cyclic nature and develops in a clockwise direction in the northern hemisphere.
- Thus they have a difference between the hurricane and mid-latitude cyclone, the typical diameter of the mid-latitude trip[ocala cyclone is 1500-5000 km. Thus there is an intensity of cyclone at the occlusion stage as they are rich in moisture and can bring heavy snowfall.
- But they don't cross the North American border as they weaken when going southwards.
<u>Answer:</u>
<em>The temperature of the basin water decreases
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<u>Explanation:</u>
Evaporation from the seas is the essential system supporting the surface-to-air part of the water cycle. The considerable surface territory of the waters gives a chance to massive scale dissipation to happen. On a worldwide scale, the measure of water vanishing is equivalent to the standard of water conveyed to the Earth as precipitation. This varies topographically, however. Evaporation is more predominant over the seas than rainfall, while over the land, precipitation routinely surpasses vanishing. A high amount of the water that dissipates from the seas falls once again into the waters as precipitation.
Answer
If the scale is a verbal statement (i.e. "1 inch equals 1 mile"), determine the distance by simply measuring it with a ruler. For example, if the scale says 1 inch = 1 mile, then for every inch between the two points on the map, the real distance on the ground is that number in miles
<u><em>Answer:</em></u>
<em>Rising in the mountains of southern Turkey, the Tigris flows southeast through Iraq, where in the southern part of that country it merges with the Euphrates to become the Shatt al Arab, which then flows to the Persian Gulf.</em>
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<u><em>Explanation:</em></u>
<em>*Hope this helped*</em>
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