What are the distribution areas of temperate monsoon climate?

The temperate monsoon climate is distributed on the east coast of the mid-latitude continent in the northern hemisphere, including the south of the sub-frigid zone, the north of the Qinling-Huaihe River in China, and the east of the temperate semi-arid and arid areas, including the northeast and north China, the Korean Peninsula, the northeast of Honshu, Japan and the south of the Far East of the former Soviet Union.

The northern boundary of this area is the southern boundary of the sub-cold zone, which is bounded by the isotherm of the annual average temperature of 4℃ and the southern boundary by the monthly average temperature of 9.5℃ in eight months of a year, and is the northern boundary of the subtropical climate zone.

Extended data:

The temperate monsoon climate is distributed on the east coast of the mid-latitude continent in the northern hemisphere. The annual average temperature is not lower than 0℃, and the annual accumulated temperature is between 3200℃ and 4500℃. Summer is hot and rainy, winter is cold and dry, and the four seasons are distinct. This is a transitional climate between subtropical zone and temperate zone.

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

Winter is cold and dry: the average temperature in Leng Yue is below 0℃, and it is cold in winter. The reasons are: high latitude, close to the source of winter wind, low terrain, flat terrain, high in the west and low in the east, which weakens the winter wind.

Monsoon is obvious, and it is often affected by tropical cyclones in summer and autumn. The main disastrous weather brought by this climate are: winter and spring: cold wave (sandstorm, frost, white damage); Summer: Strong convective weather (thunderstorm, gale, hail).