Weather Forecasting
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The document summarizes key elements of weather forecasting, including atmospheric pressure, air temperature, humidity, precipitation, and wind movement. It describes how barometers are used to detect changes in air pressure and the relationship between falling pressure readings and impending bad weather. It also explains how land and sea surfaces differentially absorb and radiate heat, causing air temperatures over land and water to vary throughout the day.
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Air pressure changes with temperature and elevation. Warmer air is less dense and rises, creating low pressure areas, while cooler air is denser and sinks, creating high pressure areas. Wind is caused by air moving from high to low pressure areas. Air pressure is measured with a barometer, wind direction with a wind vane, and wind speed with an anemometer. For a set of daily wind speed data, the range is the difference between the highest and lowest values, the median is the middle number after sorting, and the mode is the number that occurs most frequently.
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1) Atmospheric pressure variations create wind and circulation patterns as air moves from high to low pressure areas.
2) Temperature differences cause horizontal variations in pressure, with warm air rising at the equator creating low pressure and cold air sinking at the poles creating high pressure.
3) Winds are deflected to the right in the northern hemisphere due to the Coriolis effect.
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