晚上为什么不能洗衣服，请问晚上为什么吹陆风

　　晚上为什么不能洗衣服，请问晚上为什么吹陆风？

　　最近有很多热心网友都十分关心晚上为什么不能洗衣服，请问晚上为什么吹陆风？这个问题。还有一部分人想了解晚上为什么不能洗衣服。对此，和记百科小编「貳歪骚年」收集了相关的教程，希望能给你带来帮助。

晚上为什么吹陆风

　　晚上吹陆风是因为晚上时大海温度上升，海面气体受热膨胀上升，陆地晚上空气下降，同样形成压强差，形成了陆风，风从陆地吹向大海。而白天时陆地温度高，热空气膨胀上升，因陆地表面和海水表面产生压强差，因此形成海风，风从大海吹向陆地。

　　陆风的形成：

　　夜间，陆地和海洋都要降温，因为海水的比热容大，降的温度少，温度相对就会比较高，海面上方的空气密度就会上升，而陆地上面的空气就会吹向海面补充，便形成了陆风。海陆风的环流形态取决于海陆分布和由之产生的近地面气温梯度，在与山谷风（海岸山地）或城市热岛环流（海岸城市）同时出现时会发生环流耦合。此外除传统意义上的海陆风，大型内陆水体，例如湖泊、水库也会带来类似的海陆风环流，在观测中被称为内陆海陆风。陆风在夏季的信号强于冬季，在夏季的日间能够缓解沿海地区的高温并输送水汽，形成雾或降水，但通常仅在晴好天气下主导局地的风场和温度场变化。

晚上为什么不能洗衣服

　　1、一是因为晚上没有太阳，如果通风有不好的话，水会蓄积在衣物内，是不是容易滋生细菌呢。

　　2、再则，因为晚上蚊子出没，自然以吃蚊子为生的蜘蛛、壁虎什么的就多，衣物被他们爬过，或沾过它们的分泌物的话容易引起皮肤病。

　　【英文介绍/For English】：

　　The land wind blows at night because the temperature of the sea rises at night, the gas on the sea surface is heated and expanded, and the air on the land drops at night, which also forms a pressure difference, forming a land breeze, and the wind blows from the land to the sea. During the day, the temperature of the land is high, and the hot air expands and rises. Due to the pressure difference between the land surface and the sea surface, a sea breeze is formed, and the wind blows from the sea to the land.

　　Formation of the land breeze:

　　At night, both the land and the ocean should cool down, because the specific heat capacity of the sea water is large, the temperature drop is small, the temperature will be relatively high, the density of the air above the sea surface will increase, and the air above the land will be blown to the sea surface to replenish, forming a Lu Feng. The circulation pattern of the sea-land wind depends on the sea-land distribution and the resulting near-surface temperature gradient, and circulation coupling occurs when it occurs simultaneously with the valley wind (coastal mountains) or the urban heat island circulation (coastal cities). In addition to the sea-land breeze in the traditional sense, large inland water bodies, such as lakes and reservoirs, also bring about similar sea-land wind circulation, which is called the inland sea-land breeze in observations. The signal of land breeze in summer is stronger than that in winter. In summer, it can relieve high temperature in coastal areas and transport water vapor, forming fog or precipitation, but it usually only dominates local wind and temperature field changes in fine weather.