Опубликовано Edgar Gante
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1. In other words, the farther from the tropics one lies, the lower the sun angle is, which causes those locations to be cooler due the spread of the sunlight over a greater surface.[6] The strong temperature contrast between polar and tropical air gives rise to the large scale atmospheric circulation cells and the jet stream.[7] Weather systems in the mid-latitudes, such as extratropical cyclones, are caused by instabilities of the jet stream flow (see baroclinity).
2. Weather refers to day-to-day temperature and precipitation activity, whereas climate is the term for the averaging of atmospheric conditions over longer periods of time.[4] When used without qualification, "weather" is generally understood to mean the weather of Earth.
3. The Earth's weather system is a chaotic system; as a result, small changes to one part of the system can grow to have large effects on the system as a whole.
4. On Earth, the common weather phenomena include wind, cloud, rain, snow, fog and dust storms.
5. Weather does occur in the stratosphere and can affect weather lower down in the troposphere, but the exact mechanisms are poorly understood.
6. Weather is driven by air pressure, temperature and moisture differences between one place and another.
7. Weather occurs primarily due to air pressure, temperature and moisture differences between one place to another.
8. Almost all familiar weather phenomena occur in the troposphere (the lower part of the atmosphere).
9. Studying how the weather works on other planets has been helpful in understanding how weather works on Earth.
10. Most weather phenomena occur in the lowest level of the atmosphere, the troposphere, just below the stratosphere.
11. Weather systems in the mid-latitudes, such as extratropical cyclones, are caused by instabilities of the jet stream flow.
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