Characteristics of continental monsoon climate in warm temperate zone

Climatic characteristics of temperate continental monsoon;

1, high temperature and rainy in summer: In summer, the solar altitude angle increases, the days are long, the temperature is high, and the southeast monsoon blowing from the tropical ocean brings abundant precipitation.

2. It is cold and dry in winter: the lowest monthly average temperature is below 0℃, and it is cold in winter. The reason is: the latitude is high, close to the source of winter wind, the terrain is low and flat, and the west is high and the east is low, which weakens the winter wind.

The monsoon is extraordinary.

4. Summer and autumn are often affected by tropical cyclones.

The main disastrous weather brought by this climate are: winter and spring: cold wave (sandstorm, frost, white damage) and summer: strong convective weather (thunderstorm, gale, hail).

Extended data:

Geographical location:

The topography of the warm temperate zone gradually decreases from west to east, from plateaus and mountains to plains and hills. Due to the influence of topography, the whole zone is also divided into four natural regions:

Shandong Peninsula and Liaodong Peninsula, North China Plain, Loess Plateau and mountainous areas of Hebei and Liaoning. Because it is located at the edge of the mid-latitude westerly belt and the eastern monsoon area, the climate in this belt is monsoon-type humid and semi-humid climate.

Although it is cold in winter, winter wheat can be planted and crops can be harvested three times a year. In the south, warm crops such as cotton and sweet potato can also be planted. Deciduous fruit trees such as apples, peaches, apricots, walnuts, chestnuts and jujubes can survive the winter safely without protection.

The unfavorable climatic conditions are mainly cold in winter, little rain and snow, and dry and windy in spring. Autumn, crisp and full of photos, is the tourist season. The Yellow River, Huaihe River and Haihe River, the three major rivers in northern China, are all major local rivers and are all called "harmful rivers". Among them, the Yellow River is famous for its rich sediment, and the long-term siltation has made the lower reaches of the Yellow River a world-famous "river on the ground".

The middle and upper reaches of the Yellow River flow through the sandstorm area and the loess plateau with serious soil erosion. Under the double erosion of wind erosion and water erosion, the annual sediment input into the Yellow River is 65.438+0.6 billion tons, which is the highest in the world.

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