Medium-range forecast system and method for low temperature, rain and snow and freezing weather based on atmospheric variable physical decomposition
A numerical weather forecast and variable technology, applied in weather forecasting, meteorology, measuring devices, etc., can solve problems such as shortening the predictable time period, lacking physical meaning, and weakening the ability of signal indication
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Embodiment 1
[0134] Implementation 1: The 850hPa Asia-Africa-Europe temperature disturbance field output by the forecast system on January 12, 2008 ( Figure 13 ) shows that the huge negative temperature disturbance area (anomaly lower than -6K) is located from North Africa to the Middle East, and only the weak cold air is located in the eastern part of my country and gradually expands to the southwest of my country (arrow 1), but finally triggers the southern my country The region's first weak rain and snow weather.
Embodiment 2
[0135] Implementation 2: The temperature disturbance field output by the forecast system on January 16, 2008 at 850hPa in the above region ( Figure 14 ) shows that the disturbed cold air whose anomaly is lower than -6K has affected the southern region of my country. The second disturbed cold air reached Mongolia and approached the south of my country, bringing the second rain and snow freezing weather, followed by the Middle East and North Africa. There are also the 3rd and 4th disturbing cold air coming one after another, forming the 3rd and 4th rain, snow and freezing weather in southern my country.
Embodiment 3
[0136] Implementation 3: Figure 15 It is the time-varying process of height disturbance and temperature disturbance to 10hPa over southern my country (100°E-120°E, 20°N-30°N) from January 10 to February 4, 2008. The negative low temperature disturbance has been maintained below 850hPa since the 14th, the negative low temperature disturbance has been maintained near the upper 100hPa since the 12th, and the positive anomalous temperature disturbance has been maintained between 700hPa and 250hPa, and the negative temperature disturbance has appeared below 500hPa since the 17th. high disturbance. The spatial configuration relationship of such disturbance variables is conducive to the continuous appearance of multiple rain, snow and freezing weather.
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