Rain is a rare phenomenon in Antarctica: it's too cold and dry. However, there may be rains during the summer season in the Antarctic Peninsula that make up its precipitation rate of 35cm or less per year.
Tropical air is warm and moist due to high sea water evaporation. Polar air is cold and dry due to less evaporation taking place. Any rain is likely to fall as snow in the polar regions.
The climate where precipitation always falls as snow is a polar climate, found in polar regions near the North and South poles. In these areas, temperatures are consistently below freezing, causing all precipitation to be snow.
You need to give a specific desert as there are about 2 dozen major desert regions of the world, each with different climate statistics. May is in spring in the Northern Hemisphere but fall in the Southern.You need to give a specific desert as there are about 2 dozen major desert regions of the world, each with different climate statistics. May is in spring in the Northern Hemisphere but fall in the Southern.
Yes
Australia and Antarctica fall completely in the southern hemisphere.
Rome is located in the central-western part of Italy, not specifically in the southern or eastern regions. It is situated within the Lazio region, which is bordered by the Tyrrhenian Sea to the west. While it is closer to the south than the north, it does not fall into the southern or eastern categories of Italy.
The Piedmont and Coastal Regions
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If you fall into the sea at the polar regions, the extremely cold water will quickly lead to hypothermia. The cold water can cause rapid loss of body heat and impair physical ability, making it challenging to swim to safety or stay afloat. You would have a short window of time to try to get out of the water before succumbing to the effects of the cold.
When it is fall (autumn) in southern latitudes it is spring in northern latitudes.
Regions near the 30-45 degree latitudes typically experience hot summers, cold winters, and moderate spring and fall seasons. These latitudes are often influenced by the subtropical highs in summer and polar air masses in winter, resulting in distinct seasonal changes. Examples of regions in this range include parts of the United States, southern Europe, and East Asia.