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國際都市預報
目前發布之颱風警報及相關訊息與注意事項
由於太陽對地表的加熱不均勻,熱帶地區接收太陽輻射能量多,空氣受熱上升。因流體連續性,地表兩側空氣會朝熱帶水平流動,以補充上升氣流留下的空缺。 圖1-6 6月至8月(左)及12月至隔年2月(右)的850百帕氣候平均風,顏色代表緯向風速。
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月球因本身不發光,我們所見的月光是經月面反射的太陽光,由於月球繞地球公轉,當太陽和月球在天球上經度相同時,月球的背光面向著地球所以看不到月光,叫做合朔,定為陰曆月的開始,當月球繞到距日180度時,這時受光面全部對著地球,我們可見一輪明月,叫做望,月球由朔至望再回到朔 ...
性質不同之冷暖兩氣團相遇時,其交界處為一不連續面,稱為鋒面。在鋒面兩側空氣性質,諸如溫度、濕度、風、天氣等通常均有明顯的差異。實際上鋒面為過渡地帶,其寬度通常有數公里以至數十公里不等,而鋒面與地面相交之地帶稱為鋒。
環流分析 (a)500百帕高度場月平均及距平圖 (b)地面氣壓場月平均及距平圖 (c)850百帕風場月平均及外逸長波輻射距平圖 (d)850百帕溫度場月平均及距平圖 本(5)月500百帕高度場距平(圖a)顯示,貝加爾湖東側有顯著負距平,說明東亞主槽偏北