一周天气情况回顾嘉兴情况怎么写_嘉兴过去一周天气预报

1.嘉兴国庆期间的天气情况的观察和了解

2.写一篇关于家乡天气情况，家乡的名胜，特产的英语作文，我是嘉兴人

3.嘉兴是怎么样的啊

4.浙江嘉兴的天气。9月份和10月份穿什么？短袖还是长袖了？

嘉兴天气02日嘉兴天气 白天 晴 38℃ 西北风 微风 黑夜 晴 30℃ 西北风 微风

03日嘉兴天气 白天 晴 39℃ 南风 3-4级 黑夜 多云 30℃ 南风 3-4级

嘉兴天气预报10天://.tianqizhubo/city/jiaxing

嘉兴国庆期间的天气情况的观察和了解

平湖嘉兴如何报告天气

去忙个不停。岸边是绿树成阴，一阵微风吹过，柳树舞起了长发，像个小姑娘在河边翩翩起舞。她一边优闲地舞动，一边欣赏自己在河里动人的舞姿。河里一群活泼可爱的小鱼在追逐嬉戏，也急着赶来看柳树姑娘优美的舞姿。远处，那一片片绿绿油油的庄稼，这都是小河及时给它们浇灌的功劳。一到家，我迫不及待地奔向小河，眼前的一幕让我惊呆了，本该绿树成阴的河边光秃秃的；地上的地毯也消失了，走到河边一看，更让我目瞪口呆，我使劲拧了一下自己，这不是梦。清澈的河水变得污浊不堪，小河的污水缓缓地流着，时不时地散发出一股臭味。我仿佛听见小河在哭诉：“我好丑陋呀！好恶心?

写一篇关于家乡天气情况，家乡的名胜，特产的英语作文，我是嘉兴人

嘉兴市2016年10月历史天气

平均高温：27℃ 平均低温：22℃

平均空气质量指数：56

极端高温：30℃（10月2日）

空气最好：45 空气优（10月03日）

极端低温：20℃ （10月7日）

空气最差：72 空气良（10月01日）

2016-10-01星期六 30℃ 24℃ 多云 东南风1-2级 72良

2016-10-02星期日 30℃ 22℃ 多云~小雨 南风1-2级 64良

2016-10-03星期一 26℃ 21℃ 阵雨~阴 北风3-4级 45优

2016-10-04星期二 27℃ 20℃ 阴 北风3-4级 48优

2016-10-05星期三 27℃ 22℃ 多云~阴 北风1-2级 67良

2016-10-06星期四 26℃ 22℃ 多云~阵雨 东北风3-4级 51良

2016-10-07星期五 26℃ 20℃ 阵雨~小到中雨 东风1-2级 47优

嘉兴是怎么样的啊

The weather is a set of all the phenomena in a given atmosphere at a given time. It also includes interactions with the hydrosphere. The term usually refers to the activity of these phenomena over short periods (hours or days), as opposed to the term climate, which refers to the erage atmospheric conditions over longer periods of time. When used without qualification, "weather" is understood to be the weather of Earth.

Weather most often results from temperature differences from one place to another. On large scales, temperature differences occur because areas closer to the equator receive more energy per unit area from the Sun than do regions closer to the poles. On local scales, temperature differences can occur because different surfaces (such as oceans, forests, ice sheets, or man-made objects) he differing physical characteristics such as reflectivity, roughness, or moisture content.

Surface temperature differences in turn cause pressure differences. A hot surface heats the air above it and the air expands, lowering the air pressure. The resulting horizontal pressure gradient accelerates the air from high to low pressure, creating wind, and Earth's rotation then causes curvature of the flow via the Coriolis effect. The simple systems thus formed can then display emergent behiour to produce more complex systems and thus other weather phenomena. Large scale examples include the Hadley cell while a smaller scale example would be coastal breezes.

The strong temperature contrast between polar and tropical air gives rise to the jet stream. Most weather systems in the mid-latitudes are caused by instabilities of the jet stream flow (see baroclinity). Weather systems in the tropics are caused by different processes, such as monsoons or organized thunderstorm systems.

Because the Earth's axis is tilted relative to its orbital plane, sunlight is incident at different angles at different times of the year. In June the Northern Hemisphere is tilted towards the sun, so at any given Northern Hemisphere latitude sunlight falls more directly on that spot than in December (see Effect of sun angle on climate). This effect causes seasons. Over thousands to hundreds of thousands of years, changes in Earth's orbital parameters affect the amount and distribution of solar energy received by the Earth and influence long-term climate (see Milankovitch cycles).

On Earth, common weather phenomena include such things as wind, cloud, rain, snow, fog and dust storms. Less common events include natural disasters such as tornadoes, hurricanes and ice storms. Almost all familiar weather phenomena occur in the troposphere (the lower part of the atmosphere). Weather does occur in the stratosphere and can affect weather lower down in the troposphere, but the exact mechanisms are poorly understood.[1]

The atmosphere is a chaotic system, so small changes to one part of the system can grow to he large effects on the system as a whole. This makes it difficult to accurately predict weather more than a few days in advance, though weather forecasters are continually working to extend this limit through the scientific study of weather, meteorology. It is theoretically impossible to make useful day-to-day predictions more than about two weeks ahead, imposing an upper limit to potential for improved prediction skill.[1] Chaos theory says that the slightest variation in the motion of the ground can grow with time. This idea is sometimes called the butterfly effect, from the idea that the motions caused by the fling wings of a butterfly eventually could produce marked changes in the state of the atmosphere. Because of this sensitivity to small changes it will never be possible to make perfect forecasts, although there still is much potential for improvement.

The sun and oceans can also affect the weather of land. If the sun heats up ocean waters for a period of time, water can evaporate. Once evaporated into the air, the moisture can spread throughout nearby land, thus making it cooler.

浙江嘉兴的天气。9月份和10月份穿什么？短袖还是长袖了？

嘉兴是个挺江南的城市。

是中小城市，南湖比较出名。嘉兴的几个县级市有比较出名景点，比如乌镇，南北湖，西塘等等。

有五芳斋粽子，很好吃。

总的来说，嘉兴还是比较富足的城市，现代化也不错。

天气的话，雨水比较多。

同学是去嘉兴学院吗？

希望你喜欢拉

白天薄的短袖，衬衫，裙子都可以，九月因为秋老虎的天气，还是有点儿热的30度以上的天气会有一段时间。到了十月份的时候，几本薄的长袖也ok了，热的时候袖子挽起来也不会太热。但是十月底的时候天气就凉了，但不算冷，要准备稍厚点儿的衣服，线衫也ok，这两年嘉兴秋季显额特别短，如果北方一有冷空气南下，气温会马上下降，风也比较大，就会感觉有点儿冷了。

就是不论你是来嘉兴读书还是工作，到了十月中旬之后就要开始准备稍厚点儿的衣服可，就是避免突然地冷空气会受不了。

希望对你有用，我老嘉兴了