The mT and the cP air masses are total contrasts from one another. The mT air masses represents the maritime tropical air masses, while the cP air masses represent the continental air masses.
- The mT air masses form over the seas/oceans in the tropical regions, while the cP air masses form over the land in the polar regions.
- The mT air masses have very high humidity as they form above water, while the cP air masses have low humidity as they form over land.
- The mT air masses are warm because they form in the low latitudes, while the cP air masses are cold as they form in the higher latitudes.
- The mT air masses have low air pressure, while the cP air masses have high air pressure.
- In general, the mT air masses bring in warm and wet weather, while the cP air masses bring in cold and dry weather.
The answer to your question is <span>Bolivia and Paraguay hope this helps</span>
Though it is not by any way the brightest star, it shines humbly. It has been used for thousands of years to lead people as a compass of sorts. It sits almost directly over the North Pole, showing travelers which direction is north, therefore making it easy for them to figure out where the other cardinal directions were
An open lake is a lake where water constantly flows out under almost all climatic circumstances. Because water does not remain in an open lake for any length of time, open lakes are usually fresh water: dissolved solids do not accumulate. Open lakes form in areas where precipitation is greater than evaporation. Because most of the world's water is found in areas of highly effective rainfall, most lakes are open lakes whose water eventually reaches the sea. For instance, the Great Lakes' water flows into the St. Lawrence River and eventually the Atlantic Ocean.
In a closed lake (see endorheic drainage), no water flows out, and water which is not evaporated will remain in a closed lake indefinitely. This means that closed lakes are usually saline, though this salinity varies greatly from around three parts per thousand for most of the Caspian Sea to as much as 400 parts per thousand for the Dead Sea. Only the less salty closed lakes are able to sustain life, and it is completely different from that in rivers or freshwater open lakes. Closed lakes typically form in areas where evaporation is greater than rainfall, although most closed lakes actually obtain their water from a region with much higher precipitation than the area around the lake itself, which is often a depression of some sort.
Hope this helps :)
