Patters of Atmospheric Heating and Circulation

The global model of atmospheric heating and circulation is high precipitation in the tropics, which is caused by fast vaporization in the rising air mass followed by water vapor concentration. Energy from the sun heats the earth, but unfortunately it is not evenly distributed on the surface of the earth. Tropical thermal radiation produces more radiation than radiation received in the Arctic and Arctic regions. Clouds formed in this way create strong tropical-related precipitation.

Atmospheric circulation is a means of large-scale air movement through the troposphere and distribution of heat around the earth (ocean circulation). Although the structure of large-scale atmospheric circulation changes every year, the basic structure is quite stable, since it depends on the difference between the rotation speed of the earth and the amount of solar radiation between the equator and polar regions. Gases produced by large asteroids between volcanic gas emissions and the heavy impact of the earth create the next atmosphere consisting mainly of nitrogen, carbon dioxide and inert gas. Most of carbon dioxide emissions are dissolved in water and react with metals such as calcium and magnesium during crustal weathering to form carbonates and deposit them as deposits. Discovery of water related sediments can be traced back to 3.8 billion years ago.

The net heat imbalance between the equator and polar regions expresses atmospheric science and marine science as "heat engines". (In our day-to-day experience, we are connecting the engine to the car, but for scientists, the engine is any device or system that transforms energy into motion.) Climate maintains atmospheric and oceanic movement It is the use of heat to do. Engine evaporation, convection, rain, wind, and flow are all part of the global heat engine.

The sun does not heat the earth equally. Because the earth is a sphere, the sun can warm the equator more than the polar region. Due to surface evaporation, convection, rainfall, wind and ocean circulation, the atmosphere and the ocean work seamlessly to balance the solar heat imbalance. This combination of atmospheric and ocean circulation is known as the earth's heat engine. The climate heat engine must not only redistribute the solar heat from the equator to the poles but also redistribute it to the space from the earth's surface and the lower atmosphere. Otherwise, the earth will warm endlessly. Since the Earth's surface and the atmosphere radiate heat to the universe at the same time, the temperature of the Earth does not rise infinitely. This net energy flow entering and exiting the earth system is the energy balance of the earth.