寒流 (台灣)
This article "寒流 (台灣)" is from Wikipedia. The list of its authors can be seen in its historical and/or the page Edithistory:寒流 (台灣). Articles copied from Draft Namespace on Wikipedia could be seen on the Draft Namespace of Wikipedia and not main one. 脚本错误：没有“Message box”这个模块。 This article "寒流 (台灣)" is from Wikipedia. The list of its authors can be seen in its historical and/or the page Edithistory:寒流 (台灣). Articles copied from Draft Namespace on Wikipedia could be seen on the Draft Namespace of Wikipedia and not main one. 寒流 (台灣)或稱寒潮(台灣)，每年12月初至隔年3月底，，在東亞地區由於西伯利亞冷空氣無規律性的南下，因而會造成中國大陸和台灣及日本、兩韓等地的氣溫急速下降現象。在中華民國（臺灣）寒潮之定義為：「凡是因為西伯利亞冷空氣南下，造成日最低氣溫連續兩天下降達4℃以上者，就稱為寒潮。若溫度下降達到6℃以上者，稱為強烈寒潮。」台灣地區平均每年有寒潮5至6次，強烈寒潮2至3次。[1] 指的是當大陸冷氣團南移，進入台灣，寒冷的氣團流就會使台灣各地氣溫急速下降。當中央氣象局預測大陸冷氣團一旦登陸台灣且可能導致台北市的每日最低溫降到10 ℃或以下的時候，就會把該大陸冷氣團稱為寒流。[2]
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脚本错误：没有“Redirect_Template_List”这个模块。 This article "寒流 (台灣)" is from Wikipedia. The list of its authors can be seen in its historical and/or the page Edithistory:寒流 (台灣). Articles copied from Draft Namespace on Wikipedia could be seen on the Draft Namespace of Wikipedia and not main one.
This article "寒流 (台灣)" is from Wikipedia. The list of its authors can be seen in its historical and/or the page Edithistory:寒流 (台灣). Articles copied from Draft Namespace on Wikipedia could be seen on the Draft Namespace of Wikipedia and not main one. This article "寒流 (台灣)" is from Wikipedia. The list of its authors can be seen in its historical and/or the page Edithistory:寒流 (台灣). Articles copied from Draft Namespace on Wikipedia could be seen on the Draft Namespace of Wikipedia and not main one.
