Jinhua tea is the climate of North China, and the reason for the formation of the climate in North C

According to the distribution and habits of goldenrod tea, I think the chances of goldenrod tea surviving in North China should be no problem, keep warm in winter and sunscreen in summer. You can try.

Distribution: Camellia chinensis is an ancient plant, extremely rare, extremely narrow distribution, 90% of the world's wild Camellia chinensis is only distributed in the Lanshan branch of 100,000 mountains in Fangchenggang City, Guangxi, China, growing below 700 meters above sea level, with an altitude of 200 500 meters between the range is more common, the lower limit of vertical distribution is about 20 meters above sea level. For example, Jinhua tea is still distributed in the coastal hilly plateau near the Dawang River in Fangcheng County.

The upper limit of vertical distribution can reach 890 meters above sea level, such as Ningming County, Natao Mountain, individual small-petaled goldenrod tea can still be seen, the number is very small, it is a rare and precious plant in the world.

Habits: Golden flower tea likes warm and humid climate, likes well-drained acidic soil, likes shade at the seedling stage, and likes to transmit sunlight after entering the flowering stage. The requirements for the soil are not strict, and it can grow in slightly acidic to neutral soil. It is barren and thin, and also likes fat. Strong waterlogging resistance.

It is recommended to be indoors, or with greenhouse conditions. For example, in Beijing's Nanguo Water Town and the Tropical Botanical Pavilion of Beijing Botanical Garden, it is estimated that the golden flower tea will live very happily, and I believe that their flowers will be very brilliant and bright! Most southern vegetables can be grown and marketed in northern greenhouses. Reference!

North China has a temperate monsoon climate.

As the name suggests, the cause of climate formation is related to the southeast monsoon.

Every year, about March and April, the southeast monsoon lands in the south of our country, and reaches North China in about July and August, and meets the cold air in the south, forming a large amount of rainfall and moving southward, so the eastern region of North China is relatively short in the rainy season, and then North China is controlled by the northerly wind blown by the Mongolian high pressure, and the rainfall is less, and the rain in spring is estimated to be mostly only topographic rain, which is the origin of the rain and heat in North China at the same time and the spring rain

North China has a temperate monsoon climate, mainly located in the eastern part of the continent.

Due to the difference in thermal properties between land and sea, the temperature of the Eurasian continent is lower than that of the Pacific Ocean in winter, forming a high pressure, and the prevailing northerly wind blowing from Siberia is cold and dry; In summer, the temperature of the Eurasian continent is higher than that of the ocean, forming a low pressure, and the southerly wind from the Pacific Ocean prevails, which is warm and rainy.

In China, the advance and retreat of the winter monsoon and the summer monsoon form a frontal rain: the rainy season in North China is short: the spring is dry, the precipitation is concentrated in July and August, and after September, the rain belt moves southward. The winter monsoon is stronger.

North China belongs to the temperate monsoon climate, which is characterized by high temperature and rain in summer and cold and dry in winter.

The reason for the formation is the monsoon circulation, due to the difference in the thermal properties of the sea and land, a cold high pressure is formed on the Eurasian continent in winter, and the wind blows from the land to the ocean, and the southwest monsoon prevails in North China, which is cold and dry.

In summer, a thermal low pressure forms on the Eurasian continent, and the wind blows from the ocean to the land, and it is hot and rainy.

Due to the difference in the thermal properties of land and sea, it is affected by the Mongolian high pressure in winter, blowing northerly wind, cold and little rain, and in summer, it is affected by Hawaiian high pressure, blowing southerly wind, high temperature and rain.

North China has a temperate monsoon climate, and the monsoon climate is formed due to the difference in the thermal properties of land and sea.

This phenomenon of cold and cold does not mean that the weather has improved this year, on the contrary, it means that our environment has become worse. From the perspective of the living environment of organisms, it is necessary to have a relatively stable climatic conditions to ensure the normal physiological activities of organisms. For example, if it is extremely cold or extremely hot, as in recent years, the summer is very hot, and the winter is as cold as this year, such a climate is not conducive to the normal survival of living things.

Judging from this year's weather conditions, it should be said that the most direct reason for such a relatively large-scale anomaly of precipitation and low temperature is the abnormal situation of the atmospheric circulation system, especially since January, the circulation in the middle and high latitudes is mainly characterized by meridional and frequent cold air activities. In addition, the subtropical system is stronger, more west-northerly than normal for the same period of the year, which is conducive to transporting warm and humid airflow from the south to the north. On the one hand, the cold air in the north is very active, and on the other hand, the warm and humid airflow in the south is continuously transported to the north, and the location of the intersection of cold and warm airflow is mainly located in the central and eastern regions of China, which creates favorable circulation conditions for the occurrence of large-scale rain and snow weather.

The occurrence of such circulation anomalies is generally due to two meteorological reasons, on the one hand, the movement of the atmosphere itself, and on the other hand, it is affected by external forcing, and this year's circulation anomaly is related to a La Niña event that occurred in August 2007. La Niña is mentioned here, a term that may not be as familiar to us as El Niño. La Niña is in Spanish"La Nina – "little girl, holy woman" – is the inverse of El Niño, a phenomenon in which water temperatures in the eastern Pacific Ocean near the equator drop unusually, manifested by a marked cooling of the eastern Pacific Ocean, accompanied by global climate chaos, which always follows El Niño.

Therefore, both La Niña and El Niño indicate a problem: that is, our living environment is constantly deteriorating under the destruction of human beings, and nature is constantly sounding the alarm bell for human beings.

Of course, the occurrence of this phenomenon cannot be ruled out by the influence of solar activity, and from the meteorological records mastered by humans, the earth's temperature alternates between cold and warm, which is also a natural law. However, describing a situation like this year's with the above and "unexpected" does not completely solve the problem. Inevitability is always expressed through chance, and this "accident" is actually the "inevitability" of human destruction of the earth.

North China refers to Beijing, Tianjin, Hebei, Shanxi, Inner Mongolia, two provinces, two cities and one district. The typical chaotic chain of warm temperate continental monsoon climate, drought, sandstorms, and over-exploitation of groundwater are the main environmental ecological problems in North China.

It must be Hulunbuir in the northernmost part of Inner Mongolia.

Generally refers to the area where 2 provinces, 2 cities and 1 district in northern China are located, including Hebei Province, Shanxi Province, Beijing Municipality, Tianjin Municipality and parts of Inner Mongolia Autonomous Region.

Hebei is in the northernmost part of North China, so the heat obtained is the lowest temperature.

Tianjin SGS Department of Environment.

SGS Environmental Laboratory was established in 2004 and passed the National Laboratory Accreditation (CNAL) and Metrology Accreditation (CMA) in April 2005, becoming the first and only foreign-funded or joint-venture third-party comprehensive environmental testing laboratory in China that has passed the two authoritative accreditation certifications. SGS is a 128-year-old third-party testing, inspection and certification service based in Geneva, Switzerland, with a long-standing mission of objectivity, independence and impartiality. Under the guidance of China's energy conservation and emission reduction policy and the needs of customers, our department has carried out soil and water quality pollutant analysis

Ambient air sail pattern and exhaust gas analysis (dioxin detection); occupational health testing; Cleanroom contamination analysis and grading detection.

The northwest has an inland climate, and North China has a temperate monsoon climate.

In terms of temperature, the temperature difference in North China is smaller than that in Northwest China, higher in winter than in Northwest China, and lower in summer than in Northwest China due to the influence of the ocean.

In terms of precipitation, the total amount of North China is much larger than that of the West, about 600-800, North China is a temperate monsoon climate, with more rivers in summer and less precipitation in winter, and large seasonal and interannual variations.

The summer precipitation in Northwest China is more than that in winter, and the seasonal variation is also larger, but the total amount is less than that in North China, below 400 or even 200

In addition, the recharge of ice and snow meltwater in the northwest is an important water supply.