Find the specific data of temperature and precipitation in the north from June to February, 65438! Urgent!

Beijing-Beijing is located in a warm temperate and semi-humid area with a warm temperate and semi-humid continental monsoon climate, [15]? The annual precipitation is 571.8mm. Beijing has four distinct seasons, with many sandstorms in spring, hot and rainy in summer, sunny and dry in autumn and cold and windy in winter.

Tianjin belongs to temperate monsoon climate, mainly influenced by monsoon circulation, with four distinct seasons. In summer, due to the influence of the western Pacific subtropical high, it mainly blows southerly winds; Winter is controlled by Mongolian cold high pressure and northerly winds prevail, which is easy to induce sand-blowing weather in early spring.

Harbin-Harbin belongs to the mid-temperate continental monsoon climate. There are four different seasons in a year. Winter is cold and snowy; Summer is cool and pleasant, and it is a famous summer city.

Changchun belongs to the continental monsoon climate zone, which is located in the transition zone from humid area to semi-arid area in the dry and wet climate division of the country. The temperature rises from east to west, and the precipitation decreases from east to west. Spring is short, dry and windy; In summer, the western Pacific subtropical high often meets the cold air of Lake Baikal moving to the southeast. The southeast wind prevails, and the water vapor supplemented by Bohai Sea passes through, which is warm and rainy, and the precipitation accounts for more than 60% of the whole year. In autumn, the weather is high and crisp, which can form sunny and warm weather lasting for several days, with large temperature difference and lower wind speed than in spring. The winter is long, and the climate is cold and dry under the control of strong Mongolian high pressure. Four distinct seasons, rain and heat in the same season, moderate humidity.

Shenyang-Shenyang climate belongs to warm temperate zone, with semi-humid water conditions and remarkable continental climate, belonging to temperate monsoon climate.

Taiyuan has a temperate continental monsoon climate. Four distinct seasons, abundant sunshine and abundant solar energy resources. The temperature rises rapidly in spring, accompanied by strong winds and dusty weather. Compared with the North China Plain at the same latitude, it is cooler in summer, with little high temperature above 35℃, and sunny and dry in autumn. It's colder in winter.

Shijiazhuang-located at the eastern edge of mid-latitude Eurasia, belongs to the continental monsoon climate of warm temperate zone. The seasonal variation of solar radiation is remarkable, with frequent high and low pressure activities on the ground, distinct four seasons, disparity between cold and hot, concentrated rainfall, obvious dry and wet cycles, long summer and winter, and short spring and autumn. The annual average temperature is on the high side, the spring temperature is hot in summer, the autumn is cool, the winter is cold and the rainfall is unevenly distributed. Most areas are close to perennial, and there is more rainfall in some mountainous areas in the west, resulting in spring floods, less sunshine and more windy and sand-blowing weather.

Jinan-belongs to warm temperate semi-humid continental monsoon climate. It is characterized by obvious monsoon, four distinct seasons, drought and little rain in spring, high temperature and rainy in summer, refreshing in autumn and cold in winter. The precipitation in summer in Jinan is more than that in ordinary northern cities. The terrain surrounded by mountains on three sides makes water vapor and hot air return and gather, which leads to high temperature and humidity in summer in Jinan.

Lanzhou-belongs to the continental climate of plateau warm temperate zone, with annual average temperature 1 1.2℃, annual average precipitation of 327mm, annual average sunshine hours of 2446 hours and frost-free period 180 days or more. In spring, Lanzhou is vulnerable to sandstorms.

Xi is located in the transitional zone between monsoon region and subtropical monsoon climate region. Four distinct seasons and moderate rainfall.

Zhengzhou belongs to the continental monsoon climate with the transition from warm temperate zone to north subtropical zone. Under the combined action of solar radiation, topography and geology, atmospheric circulation and other factors, a climate with moderate cold and warm, four distinct seasons, rain and heat, and four distinct dry and cold seasons has been formed. The four seasons alternate obviously, showing drought and little rain in spring, hot and rainy in summer, abundant sunshine in autumn, long sunshine time and cold and little rain in winter.