7.25火法一键爆发宏:英国的气候特点？今天马上急需

climate

The British climate is moderated by the Atlantic Gulf Stream, and is much milder than that of many places in the same latitude. The climate of Great Britain is generally equable. Winters are especially mild on southwestern coasts, where severe frosts are rare. The seasonal variations in temperature increase eastward. Winter mean temperatures exceed 4 ℃ in the west but are lower in the east. The July mean, on the other hand, is about 18℃ in the southeast of England but falls to 13℃ in northern Scotland. Since the prevailing winds are southwesterly, the Atlantic air streams often bring cloudiness and humidity, and the frequent passage of fronts and depressions ensures very changeable day-to-day conditions. Temperatures fall surprisingly rapidly with increased altitude.

Rainfall occurs throughout the year, there being no marked dry season. In the highland west it may exceed 254 cm per year, but in the eastern lowlands it is only 64 to 76 cm. Sunshine hours in Britain are fewer than in more southerly climates ------ averaging between 3 and 4 hours a day and between 4 and 6 from June to August. On high ground, winters are more severe and snow may lie fro 30 days on the Pennines and as long as 50 days in the Scottish Highlands.

All over the world Britain is notorious for its fogs. The ordinary damp mists which afflict all parts of the country from time to time are no worse than similar mists in many other countries. The smoke-fogs of the big towns, which used to develop in winter time whenever there was not enough wind to blow the smoke away, were horrible, unhealthy and dangerous to movement. Much of the smoke-fog was caused by the burning of coal in fireplaces in private houses, though smoke from factories contributes a great deal to the trouble. A Clean Air Act was passed by Parliament in 1956, giving local councils power to control smoke in designated areas; the effects of this excellent plan have been very noticeable. The really bad smoke-fogs have passed into the realm of myth, and the visibility during the foggy day is much better than before in Britain.

http://www.dhu.edu.cn/english/filmtv/LING/shen%20Webs/climate.htm

地理环境

全境由靠近欧洲大陆西北部海岸的不列颠群岛的大部分岛所组成，隔北海、多佛尔海峡和英吉利海峡同欧洲大陆相望，是一个岛国。

英国位于北纬50度至60度之间，比我国的黑龙江省还要偏北，但气候却温和得多，可以说是冬无严寒，夏无酷署。这温和的气候首先要归功于热带的墨西哥湾暖流。这股暖流，有好几百公里宽。它浩浩荡荡地流向欧洲西北岸，改称大西洋暖流，为英国带来了温和湿润的海洋性气候。以伦敦为例，冬天河湖极少结冰，一月份的平温气温在4度(摄氏)以上；而夏天又相当凉爽，七月份的平温气温只有17度，早晚常要加件线衣才行。年降雨量约600毫米，不算太多，但分布比较均匀。就全国来说，一月份的平均气温约为4至7度，七月份13至17度。年降雨量西北部山区超过1000毫米，而东南部在六七百毫米之间。英国的雾气较重，在夏季晴和的好天中，还有薄薄的烟霭；冬季则经常飞雾迷漫，似雨非雨，若烟非烟，这主要是岛国的潮气所致。至于伦敦过去常见的浓雾，并不完全是自然现象。由于重视环境保护，那里出现浓雾的次数已大大减少。

这个岛国的气候温和，但天气多变。英国人常说：“国外有气候，在英国只有天气”，以此来表明这里天气的变化莫测。的确，在一日之内，忽晴忽阴又忽雨的情况并不少见。这种天气使人变得格外谨慎，看到一位英国人在阳光明媚的早上出门时穿着雨衣，带着雨伞，外国人可能会感到可笑，但是不久以后他就会为自己的“感到可笑”而后悔。多变的天气也为人们提供了经常的话题，在英国甚至最沉默寡言的人也喜欢谈论天气。

受高纬度的影响，英国昼夜长短的变化特别明显。冬季日短夜长，下午未到3点，天色已灰暗一片，夏季则正好相反，日长夜短，晚上10点多才开始入黑。一般来说，夏天是旅游英国最好的日子。夏季日间长，活动时间多，而且温度适中，天气清爽，人的精神也倍感充沛。这个季节尽管也有雨，但一般不会连绵不断，影响行程。

总体而言，英国主要地区的天气特征如下：

英格兰北部：温度比南部要低

英格兰东北部：最冷的地区

英格兰南部：气候最好的地区

英格兰东南部：夏季温度高，冬天温度低，温差变化大

英格兰东部：降雨较少的地区

英格兰西部：降雨最多的地区

时差：北京与英国格林威治标准时间相差8小时，也就是说北京比英国早8小时。比如，英国格林威治标准时间为零时，而北京是早晨8时。

lwxted01 说的已经很详细了， 补充一些， 希望对你有用。
由于英国采用夏令时， 所以夏天时和中国时差7小时。

虽然英国冬天温度看上去很低， 但家家都有暖气， 所以不怎么觉得冷。