目錄中國的天氣英語 用英語介紹一下中國的天氣 介紹一下今天的天氣情況英語
Chinahas many different kinds of climate .In the southern part of China, the temperature changes very little between summer and winter. But the north central states have a very different kind of climate. In those countries , people wear light clothing during the summer, and they need heavy wool or fur clothing in the winter. In the southwest, the climate is pleasantly warm during the winter, but the summer is unpleasantly hot.In the eastern part of China, summer temperatures are very different from winter temperatures. Summer are usually hot, and winters are usually cold. Spring temperatures are comfortably warm, and fall temperatures are pleasantly cool.
中文：中國有許多不同類型氣候。在中國的南部，溫度非常少，在夏天和冬天之間改變。但是北方的中央州有非常不同類型氣候。在那些國家，人們在夏天期間穿著輕的衣服，而且他們需要仿豎重羊毛或清旁毛皮在冬天的衣服。在西南，氣候在冬天期間愉快溫暖，但是夏天不愉快熱。在中國的東部，夏天溫度非常備正大不同于冬天溫度。夏天通常很熱，而且冬天通常很寒冷。春天溫度安樂溫暖，而且秋天溫度愉快涼爽。
Climate Features and Impacts in July of 2005
In July, the climate characteristics were showed as follows: monthly precipitation was less than normal in China as a whole. The precipitation was from 200-300mm in some regions of Shandong, Henan, Jiangshu, Anhui, Hubei, Sichuan etc, and more than 300mm in south of Henan and north of Anhui. While the precipitation was less than 50 mm in some regions of Inner Mongolia, Xinjiang, Gansu etc. Temperature was higher than normal in China as a whole by 0.8℃. In some regions of Inner mongolia, Xinjiang, Xizang, Zhejiang, Jiangxi, Hunan, Guangxi etc, temperature was higher than normal by 1～2℃.
In July, the main climate events include: Server flood, mud-rock flow and landslide disaster happened in Yangtze river basin, Sichuan etc, which caused 93 peopel dead and 23 people lost as well as 75.4 billion Yuan economical lost. Typhoon “HAITANG” landed on Taiwan on 18 July and Fujian on 19 July, which caused serious damages in Zhejiang and Anhui with 119.2 billion Yuan economical lost. Another typhoon “WASHI” landed on Hainan on 30 July. Heat wave raided in Fujian, Guangdong, Guangxi, Hunan, Anhui etc, the highest temperature was higher than 40℃ in some regions of Xinjiang, Inner Mongolia, Gansu, Hebei, Zhejiang, Shanxi etc. Summer Drought last or developed at west and middle of Inner Mongolia, north of Shanxi and Shaanxi, east of Guizhou and west of Hunan etc, shortage of water influenced agriculture, living water and supply of electric power. More than 20 Provinces hit by thunderstorm, hail and gale. 15 people were killed by gale and cyclone in Weiji town of Biling county of Anhui. Sand storm appeared in some regions of Inner Mongolia and Gansu from 16 to 17 July.
天氣英語詞匯
meteorology 氣象學
atmosphere 大氣
climate 氣候
elements 自然力量（風 、雨）
temperature 氣溫
to be warm, to be hot 天氣熱
to be cold 天氣冷
season 季節
spring 春
summer 夏
autumn 秋（美作：fall）
winter 冬
frost 霜
hail 冰雹
snow 雪
thunder 雷
wind 風
mist 霧
cloud 云
haze 霾
rain 雨
downpour, shower 暴雨
storm, tempest 暴風雨
lightning 閃電
land wind 陸風
hurricane 颶風
cyclone 旋風
typhoon 臺風
whirlwind 龍卷風
gale 季節風
gust of wind 陣風
breeze 微風
fog 濃霧
dew 露水
humidity 潮濕
freeze 冰凍
snowflake 雪花
snowfall 降雪
waterspout 水龍卷
dead calm 風平浪靜
Indian summer 小陽春
drought 干旱
比較簡單：
EMBASSY OF THE PEOPLE'S REPUBLIC OF CHINA IN THE KINGDOM OF DENMARK網站上的
China has a marked continental monsoonal climate characterized by great variety. Northerly winds prevail in winter, while southerly winds reign in summer. The four seasons are quite distinct. The rainy season coincides with the hot season. From September to April the following year, the dry and cold winter monsoons from Siberia and Mongolia in the north gradually become weak as they reach the southern part of the country, resulting in cold and dry winters and great differences in temperature. The summer monsoons last from April to September.
The warm and moist summer monsoons from the oceans bring abundant rainfall and high temperatures, with little difference in temperature between the south and the north. China’s complex and varied climate results in a great variety of temperature belts, and dry and moist zones. In terms of temperature, the nation can be sectored from south to north into equatorial, tropical, sub-tropical, warm-temperate, temperate, and cold-temperate zones; in terms of moisture, it can be sectored from southeast to northwest into humid (32 percent of land area), semi-humid (15 percent), semi-arid (22 percent) and arid zones (31 percent).
