What is the name of winter pile squeezing in Xinghua, Jiangsu Province?

Crowding in winter in Xinghua, Jiangsu Province is generally an exclusive game for male students.

Find a corner, almost all the boys in the class are involved. Everyone stood close to the wall and shouted in unison, pushing the people inside into the corner from two directions. The efforts in the platoon make money, the efforts from outside squeeze in, and the cards that are squeezed out are stuck outside and squeezed in, and so on.

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Xinghua city is a county-level city under the jurisdiction of Jiangsu Province, which is managed by Taizhou City. It is located in the middle of Jiangsu Province, in the northern wing of the Yangtze River Delta, between Jianghuai and Lixia hinterland, east longitude119 43' ~12016', and north latitude 32 44' ~ 33 66'. With a total area of 2393.35 square kilometers, as of June 2022, it has jurisdiction over 3 streets, 22 towns and 1 township.

topography

Xinghua city is low-lying and flat, with a ground elevation of 1.40m ~ 3.20m and an average elevation of 1.80m (abandoned Yellow River height system, the same below). The territory is a dish-shaped depression with high periphery and low middle, slightly higher in the east and south and lower in the northwest. It is the lowest place in the three depressions of Jianhu, Xinghua and Qintong in He Lixia, commonly known as "Pot Bottom Depression".

Xinghua city is a shallow depression plain in He Lixia River, which is located in the center of He Lixia depression in Jianghuai Plain. It is a continuous subsidence area of Mesozoic and Cenozoic fault basins, and its paleogeomorphology is a large lake basin depression.

In Quaternary, the depression experienced the evolution process of bay-lagoon-water network plain accumulated by river and sea, and formed the geomorphological features of lakes and swamps, which were all covered by Quaternary Holocene lacustrine deposits and river floods, and its basement was Paleozoic strata dominated by carbonate rocks.

climate

Xinghua city has a humid climate in the north subtropical zone, with abundant sunshine, mild climate and abundant rainfall. The rain and heat are in the same period, and the light, temperature and precipitation are relatively coordinated. The annual average sunshine hours are 2305.6 hours, the annual sunshine percentage is 52%, the average temperature is about 15℃, the average precipitation is 1024.8 ml, and the average rainy day is 1 12 days. About 60% of the annual precipitation is concentrated in June, July, August and September in the flood season, with an average relative humidity of.

The monsoon climate is obvious, and the dominant wind direction is east-southeast all the year round; In summer, it is southeast wind with a frequency of 28%; In winter, it is northeast wind with a frequency of 22%. The average frost-free period is 227 days. The disastrous weather that has great influence on the territory mainly includes rainstorm, continuous rain, typhoon, hail, cold wave and high temperature, among which the disasters caused by rainstorm and typhoon are the most serious.