Qingtongxia Weather Qingtongxia Weather Forecast

1. The weather conditions in Qingtongxia City, Ningxia from August 15th to August 20th 2. Does anyone know about the weather conditions and living conditions in the coal mines in Qingtongxia City, Ningxia? Thank you here. . 3. How is the weather in Qingtongxia during the day and at night? 4. An 800-word short essay on the weather and climate in Ningxia. The weather conditions in Qingtongxia, Ningxia from August 15 to August 20

Air quality conditions

Air Quality: Good AQI: 74PM2.5: 37

PM10: 72O3: 178NO2: 34CO: 2.337

Weather: Cloudy 30℃

Northwest wind level 2 humidity: 33%

Does anyone know about the weather conditions and living conditions in the coal mines in Qingtongxia City, Ningxia? Thanks here.

The northwest is very water-scarce

I have never been to Qingtong Gorge. It may be better if it is close to the Yellow River. Looking at the satellite map, the greening is okay

Bronze Qingtongxia weather forecast during the day and night time

Ningxia Qingtongxia weather forecast

20:25 live situation

Relative humidity 83%

Southwest Wind level 1

18°C

Night of the 20th

Cloudy

15°C

Breeze

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A short 800-word essay on the weather and climate of Ningxia

Ningxia is located deep in the northwest inland plateau and has a typical continental semi-humid and semi-arid climate. The rainy season is mostly concentrated from June to September. It has the characteristics of long cold winters, short summer heats, scarce rain and snow, dry climate, strong winds and sandy weather, cold in the south and warm in the north. Since the average altitude of Ningxia is above 1,000 meters, there is basically no severe heat in summer; the average temperature in January is below minus 8°C, and the extreme low temperature is below minus 22°C.

The most significant features of Ningxia's climate are: large daily temperature differences, long sunshine hours, and strong solar radiation. The temperature difference between day and night in most areas can generally reach 12-15oC. So even if you go to Ningxia in summer, you should prepare some thick clothes. May to October every year is the best tourist season.

Ningxia is located in the interior of China and has a temperate continental arid and semi-arid climate. Because it is located at the western edge of China's monsoon area, the summer is affected by the southeast monsoon, which is short and has little precipitation. July is the hottest month with an average temperature of 24°C. The winter is greatly affected by the northwest monsoon, which is long and has large temperature fluctuations. January is the hottest month. Cold, with an average temperature of -9°C. The annual precipitation in the region ranges from 150 mm to 600 mm. The southern Liupan Mountain area is humid and rainy, with low temperatures and a short frost-free period. The north has abundant sunshine, strong evaporation, and a large temperature difference between day and night. It has 3,000 hours of sunshine throughout the year and about 150 days of frost-free period. It is one of the areas with the most abundant sunshine and solar radiation in China. Ningxia has four distinct seasons, with spring getting warmer quickly and autumn getting colder early. From May to September, Ningxia's mountains and rivers have pleasant climate and picturesque scenery, making it the golden season for tourism.

Ningxia is located in the transition zone between the first ladder and the second ladder in China's terrain. The entire territory is more than 1,000 meters above sea level. The terrain is higher in the south and lower in the north, with a height difference of nearly 1,000 meters. The territory has mountain peaks, scattered plains, rolling hills, and scattered sand dunes and sandy areas.

Ningxia is located between 35°25′ and 39°25′ north latitude and 104°10′ and 107°30′ east longitude. It is located in mid-latitude inland, far away from the ocean. In the northern hemisphere, the direct point of the sun moves regularly between the Tropic of Cancer on both sides of the equator every year. Therefore, the geographical latitude determines the solar altitude angle of a place, the length of sunshine and the amount of solar energy obtained. The geographical location of Ningxia, The sun's altitude changes greatly throughout the year. Taking the Ningxia Plain at 38° north latitude as an example, the sun's altitude at noon on the winter solstice is 29°, and the sunshine duration is 9 hours and 21 minutes; on the summer solstice, the sun's altitude is 79° at noon, and the sunshine duration is 9 hours and 21 minutes. It is 14 hours and 49 minutes, which is the basic reason for "cold in winter and hot in summer".

Influence of topography

Ningxia’s topography is relatively complex and can be roughly divided into loess plains, Ordos platform, alluvial plains on both sides of the Yellow River and alluvial fans along the mountain areas, and Liupan Mountain, Luoshan Mountain, Helan Mountain and other mountainous areas. The terrain is high in the south and low in the north, steep in the west and gentle in the east. The landform transitions from water-intruded landform in the south to wind-eroded landform in the north.

Topography and terrain have a great influence on the formation of climate. The level of air pressure is mainly caused by altitude. The higher the altitude, the lower the air pressure. The Helan Mountain Weather Station is 2,910 meters above sea level. The annual average The air pressure is 715.0 hectopascals, while Pingluo at the foot of the mountain has an altitude of 1099 meters, and the annual average air pressure reaches 892.0 hectopascals.

Wind is affected by terrain, which can change wind direction and speed, causing local winds. Huinong is located in the narrow throat area between Helan Mountain and Zhuizhuishan Mountain. When the wind blows in from the open area in the north, the effect of the canyon increases the wind speed, so Huinong is the windiest place in Ningxia. Dawukou is close to the east slope of Helan Mountain. There are more valley winds in the summer half of the year. Valley winds blow during the day and mountain winds blow at night. This is caused by the unsynchronized thermal effects of the hillside and the valley and the inconsistent air density. The dominant wind direction in the entire Ningxia Plain is northerly, which is basically consistent with the north-south direction of the Helan Mountains.

Mountains can change the direction of air flow. For example, when a shallow westerly wind is blocked by Helan Mountain, it will go south along the west slope because it is unable to climb over the top of the mountain. When it reaches the lower part of the southern mountain range, it will cross the mountain, and then go north along the mountain. Therefore, you can often see the westerly wind blowing in Qingtongxia, while the southerly wind blows in Yinchuan.

Mountains and topography have a more obvious impact on temperature. The annual average temperatures in Helan Mountain and Liupan Mountain are only -0.8℃ and 1.0℃ respectively, while the annual average temperatures in Yinchuan, Longde and Guyuan below the mountains are 8.6℃ respectively. , 5.1℃ and 6.2℃. The vertical temperature decline rate from the bottom of the mountain to the top of the mountain is 0.53℃/100m on the east slope of Helan Mountain, 0.58℃/100m on the west slope of Liupanshan, and 0.49℃/100m on the east slope of Liupanshan. When the air flows down over the mountains, it will produce the foehn effect of dry adiabatic warming. Therefore, the annual temperature on the east slope of Helan Mountain is generally 1℃ higher than that of Bayinhot on the west slope. Dawukou is close to the east slope, so the foehn effect is more obvious. , the annual average temperature is 2.4℃ higher than that of Bayinhot. The relatively open plains in mountain basins and valleys can easily cause the accumulation of cold air and cause frost. Lunde, under the Liupan Mountains, is in a valley surrounded by mountains, which is conducive to the accumulation of cold air. Therefore, the temperature in Lund is ≤2℃ on the first frost day. It appears earliest (September 18th), and the last frost day ends latest (June 3rd). The shortest frost-free period is only 103 days.

The windward slope terrain has an uplifting effect on the airflow, which is conducive to the formation of precipitation. Therefore Helan Mountain and Liupan Mountain have greater precipitation and more precipitation days than the surrounding areas. Most heavy rains also occur in the hillside areas. The annual precipitation in Helan Mountain is 429.8 mm, and the annual precipitation days are ≥1.0 mm. The number of precipitation days is 90 days, while the annual precipitation days in Helan Mountain are 90 days. The precipitation is below 200 millimeters, and there are only about 45 days of rainfall per year. The southern slope of Liupan Mountain is the channel for warm and humid air to move north. The uplift of the terrain causes heavy precipitation in the mountains. The annual precipitation in Liupan Mountain, Jingyuan, and Longde reaches 600 days. 700 mm, the annual precipitation days are as many as 110-130 days, while the annual precipitation of Guyuan, located behind the north slope mountain, is 478.2 mm, and the annual precipitation days is 95 days.