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It normally goes to east to west and the cycle of the vagina cools the other vaginas
Condensation
Water is not easy to warm up, so during the day the water is cooler than the land. This causes the lake to cool the air above it. The cooler, denser air the sinks, and must spread out onto land when it reaches the surface.
it would gradually warm up, the speed at which it heats up and then looses that heat at night all depends on location, depth and surface area of that lake.
first it evaporates into a cloud, then its held up in the cloud for a time and when cold and warm air mix it comes back down to earth.
High temperature.
When you have warm water the molecules are warm enough for vapor so that causes precipitation.
its all to do with the hydrological cycle. the water from a lake is evaporated by the sun and as this condensation is warm it rises. the warm air then moves to areas where the air is cold and cools, condenses and forms rain clouds.
If the temperature of the water is less than your body temperature, then heat will be transferred from the warmer body to the colder body of water. The molecules in your skin vibrate because they are warm. When a water molecule touches a warm vibrating skin molecule, some of the heat energy in the skin molecule is transferred to the water molecule, warming the water.
warm air rises usually through the water cycle (humidity is risen). the water cycle consists of production, percipation and f a r ts .
warm air rises usually through the water cycle (humidity is risen). the water cycle consists of production, percipation and f a r ts .
warm air rises usually through the water cycle (humidity is risen). the water cycle consists of production, percipation and f a r ts .
Turnover
a cloud forms when water molecule's, dust, and warm air combine
There are no warm water ports any where near Lake Baikal. Lake Baikal freezes solid to depths of up to 10 metres during the Siberian winter.
Deeper colder water can be churned up by currents in a lake. The currents can be caused by wind or upwelling (water introduced from below) the stratification of water in a lake is a very complex mater.
usually about 50 degrees