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

2024-07-25 20:02:17

1.加兴地区二零一二年三月的天气情况

2.嘉兴的天气好吗？

3.求嘉兴历年9月20日左右的天气情况,包括气温最高和最低

4.嘉兴最近天气怎么样？穿什么合适？

5.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

6.近一周嘉兴天气预报

7.帮我查一下嘉兴平乡天气预报今天和明天一周的

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

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

加兴地区二零一二年三月的天气情况

今天（周二）

16～11℃

阵雨

东风3-4级

明天（周三）

14～6℃

小雨

东风3-4级

后天（周四）

11～3℃

小雨转多云

西北风4-5级

嘉兴的天气好吗？

嘉兴天气预报 (2012-03-09 11:00发布)

9日星期五白天阴高温 8℃ 东北风 4-5级

夜间阴低温 2℃ 北风 3-4级

10日星期六白天多云高温 9℃ 北风 3-4级

夜间多云低温 2℃ 北风 4-5级

11日星期日白天多云高温 8℃ 北风 4-5级

夜间多云低温 1℃ 东北风 3-4级

求嘉兴历年9月20日左右的天气情况,包括气温最高和最低

★嘉兴未来天气预报★

嘉兴天气预报 09月14日星期五:

[白天] 阴，24℃，3-4级，北风

[夜间] 多云，17℃，3-4级，东北风

嘉兴天气预报 9月15日星期六：

[白天] 多云，25℃，3-4级，东北风

[夜间] 阴，17℃，4-5级，东北风

嘉兴天气预报 9月16日星期日:

[白天] 阴，25℃，4-5级，东北风

[夜间] 阴，19℃，3-4级，北风

嘉兴天气预报 9月17日星期一：

[白天] 阴，26℃，3-4级，北风

[夜间] 多云，20℃，3-4级，西风

嘉兴天气预报 9月18日星期二：

[白天] 阴，27℃，3-4级，西风

[夜间] 多云，19℃，3-4级，西北风

嘉兴天气预报 9月19日星期三：

[白天] 多云，26℃，3-4级，西北风

[夜间] 多云，18℃，3-4级，东风嘉兴天气预报 9月20日星期四：

[白天] 多云，25℃，3-4级，东北风

[夜间] 阴，17℃，4-5级，东北风

嘉兴未来天气预报 ://.youbian/tianqi/jiaxing/

嘉兴最近天气怎么样？穿什么合适？

晴到多云转阴有时有阵雨或雷雨，短时间雨量较大，局部地区有暴雨。

东南风转西北风三到四级，午后起增强到五到六级，阵风八到九级。

早晨最低温度五度，上午起十到十五度，中午十八度，下午到夜里十五到三度。希各有关方面做好防冻保暖工作。

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

嘉兴天气

今天：温度3℃ - 12℃。白天：晴，夜间：晴。北风2-3级转东北风3级

明天：温度4℃ - 13℃。白天：多云，夜间：多云, 小雨。东风2-3级转3级

2007.12.15

穿什么看你的身体体质怎么样，根据你的喜好自行选择了

近一周嘉兴天气预报

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.

帮我查一下嘉兴平乡天气预报今天和明天一周的

嘉兴天气预报（2010-10-14 11:00发布）日期天气现象气温风向风力

14日星期四白天小到中雨高温17℃ 北风 3-4级

夜间阴低温13℃ 北风 3-4级

15日星期五白天多云高温22℃ 东北风 3-4级

夜间多云低温11℃ 东北风 3-4级

16日星期六白天晴高温23℃ 东南风 3-4级

夜间多云低温11℃ 东南风 3-4级

17日星期日白天晴高温24℃ 东风 3-4级

夜间多云低温13℃ 东风 3-4级

18日星期一白天多云高温22℃ 东风 3-4级

夜间阴低温14℃ 东风 3-4级