What's the climate like in Heze, Shandong?

The climate changes in Heze, Shandong Province are as follows:

Heze has a continental climate with warm temperate monsoon, four distinct seasons and abundant light and heat resources. Precipitation is mostly in summer, with water and heat in the same season, which is suitable for most crops. At the same time, Heze is also a frequent area of meteorological disasters and weather. Drought and flood are one of them, especially drought, which has high frequency, wide influence and is the most serious.

In addition, there are more opportunities for rainstorm, which generally occurs in May-September and is the most frequent in July-August. The average annual rainstorm days are generally between 1.9-2.7 days. Heze area belongs to the plain, and heavy rain often causes waterlogging.

Secondly, frost also happens from time to time. Frost in early autumn appears on average in 1 1 October, with the earliest in1October 17 and the latest in1/October 2 1. The last frost period in spring is April 6, the earliest is March 17, and the latest is April 25. In recent years, the probability of gale and hail has become smaller.

Geological structure of Heze City, Shandong Province

The geological structure of Heze City belongs to the Sino-Korean paraplatform, which is located in the southeast. Bounded by the west oblique Liaocheng-Lankao fault, it is divided into two secondary structural units: North China fault depression and Luzhong uplift. Dongming sag on the west side is a fourth-order structural unit, which belongs to Kaifeng platform sag, a third-order structural unit of North China fault depression. The eastern part belongs to the central Shandong platform uplift, accounting for most of the country, and is the western half of the third-level structural unit Chengwu-Jining fault depression.

Cao Xian fault and Fushan fault are divided into Chengwu fault depression and Jining fault block. It is divided into some local structures by Cao Xian fault and Sven fault. The former, such as Heze, Brick Temple, Qing Dynasty? Jifeng and Fengxian bulges and Juye and Liangshan Quanpu depressions. Yanshan movement formed the embryonic form of various structural patterns, and Himalayan movement controlled various structural bodies in China.

The distribution of structural units in the city, especially the secondary and tertiary structures, has the following characteristics: (1) the structural line of North China fault depression on the west side is mainly northeast; On the east side, the platform uplift in the central part of western Shandong is mainly northeast-east-west arc, and the latter formed earlier. Due to previous movements, hidden faults crisscross the territory, especially in the east. The exposed strata in the stratigraphic area are mainly Cenozoic Quaternary, with Paleozoic Cambrian and Ordovician in some areas.

Reference to the above content: Baidu Encyclopedia-Heze City