Guangzhou weather and temperature table query today
作者: 岑仲隽, 发布: 2024-09-23 00:31:02
壹、What is the climate in Guangzhou?
Guangzhou is located in the south subtropical zone, and its climate is a typical monsoon ocean climate in the south subtropical zone. Because it is backed by mountains and faces the sea, the maritime climate characteristics are particularly significant, with climate characteristics such as warm and rainy weather, sufficient light and heat, small temperature differences, long summers, and short frost periods. Because the water and heat are at the same time, it is extremely conducive to the growth of crops, but the threat of natural disasters is also greater. Disastrous weather such as typhoons, heavy rains, cold waves, lightning, and haze often have adverse effects on industrial and agricultural production, transportation, etc.
There are sufficient light and heat resources. In 2005, the annual sunshine hours in Guangzhou ranged from 1288.5 to 1780.0 hours, the annual average temperature ranged from 21.9℃ to 22.8℃, the annual extreme maximum temperature ranged from 38.6℃ to 39.3℃, and the annual extreme minimum temperature ranged from 0.0℃ ~2.3℃. This summer, all districts (county-level cities) experienced high temperatures and extremely hot weather. In winter, except for frost and ice in Conghua City and Zengcheng City, there was basically no cold damage in other areas.
Plenty of rainfall. In this year, the total pre cipitation in various districts in Guangzhou ranged from 1384.4 to 2278.3 mm. Except for Panyu District, which was 15.0% less than the pre vious average, the other districts were 5.0% to 18.8% more than the pre vious average. The total pre cipitation in Zengcheng City was 2278.3 mm, ranking first in the city. First place, 18.8% more than the average over the years. The rainfall in the rainy season (April to September) accounts for 80% to 83% of the whole year. Due to the influence of terrain, pre cipitation is more in mountainous areas than in plains, and more in the north than in the south. The distribution of pre cipitation time this year is extremely uneven, with significantly more pre cipitation in each region from April to June. In June, floods occurred in Zengcheng City due to the impact of local heavy rains and water from upstream. At the same time, the rainy season coincides with strong light and high heat, resulting in a very high climate biological potential, reaching 77865-97950 kg/ha.
The monsoon climate is prominent. The alternation of winter and summer monsoons is a prominent feature of Guangzhou's monsoon climate. The northerly wind in winter is formed by the southward expansion of the polar continental cold air mass, making the weather drier and colder; the southerly wind in summer is formed by the northward expansion of the tropical ocean warm air mass, and the weather is often warm, hot and humid. The transition from summer monsoon to winter monsoon usually occurs in September each year, while the transition from winter monsoon to summer monsoon usually occurs in April each year.
There are sufficient light and heat resources. In 2005, the annual sunshine hours in Guangzhou ranged from 1288.5 to 1780.0 hours, the annual average temperature ranged from 21.9℃ to 22.8℃, the annual extreme maximum temperature ranged from 38.6℃ to 39.3℃, and the annual extreme minimum temperature ranged from 0.0℃ ~2.3℃. This summer, all districts (county-level cities) experienced high temperatures and extremely hot weather. In winter, except for frost and ice in Conghua City and Zengcheng City, there was basically no cold damage in other areas.
Plenty of rainfall. In this year, the total pre cipitation in various districts in Guangzhou ranged from 1384.4 to 2278.3 mm. Except for Panyu District, which was 15.0% less than the pre vious average, the other districts were 5.0% to 18.8% more than the pre vious average. The total pre cipitation in Zengcheng City was 2278.3 mm, ranking first in the city. First place, 18.8% more than the average over the years. The rainfall in the rainy season (April to September) accounts for 80% to 83% of the whole year. Due to the influence of terrain, pre cipitation is more in mountainous areas than in plains, and more in the north than in the south. The distribution of pre cipitation time this year is extremely uneven, with significantly more pre cipitation in each region from April to June. In June, floods occurred in Zengcheng City due to the impact of local heavy rains and water from upstream. At the same time, the rainy season coincides with strong light and high heat, resulting in a very high climate biological potential, reaching 77865-97950 kg/ha.
The monsoon climate is prominent. The alternation of winter and summer monsoons is a prominent feature of Guangzhou's monsoon climate. The northerly wind in winter is formed by the southward expansion of the polar continental cold air mass, making the weather drier and colder; the southerly wind in summer is formed by the northward expansion of the tropical ocean warm air mass, and the weather is often warm, hot and humid. The transition from summer monsoon to winter monsoon usually occurs in September each year, while the transition from winter monsoon to summer monsoon usually occurs in April each year.
