Traditional Culture Encyclopedia - Weather inquiry - How is the weather forecast developed?
How is the weather forecast developed?
The development of weather forecast can be divided into three stages:
The first stage is single station forecast. /kloc-before the 0/7th century, people made weather proverbs by observing the changes of astronomical phenomena and celestial bodies, thus predicting the local future weather. /kloc-after the 0/7th century, meteorological observation instruments such as thermometers and barometers appeared one after another, and ground weather stations were established one after another. At this time, the weather is mainly predicted according to the changes of single station pressure, temperature, wind and cloud. This is not a real weather forecast, but only the embryonic form of modern weather forecast.
The second stage is the weather map forecast. 185 1 year, Britain sent observation data by telegraph for the first time, drew weather map on the ground, and made weather forecast according to the weather map. Since the 1920s, air mass theory and polar front theory have been applied to weather forecast. In 1930s, the invention of radiosonde, the appearance of high-altitude weather map and the wide application of long-wave theory in weather forecast made the analysis of weather evolution develop from two-dimensional to three-dimensional. In the late 1940s, the application of weather radar provided an effective tool for forecasting precipitation, typhoon, rainstorm and severe storm.
The third stage is numerical weather forecast. Since 1950s, the principles of dynamic meteorology, mathematical and physical methods and statistical methods have been widely used in weather forecasting. The equations of atmospheric fluid mechanics and thermodynamics are simplified by solving with high-speed electronic computer, and the weather forecast can be made in time. Especially since the launch of meteorological satellites in the 1960s, the satellite detection data have made up for the shortage of meteorological data in oceans, deserts, polar regions and plateaus, and the level of weather forecasting has been significantly improved.
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