How to reduce the amount of wrfout data How to reduce the amount of wrfout data Two methods, Go into the WRF/Registry/Registry.EM_COMMON file, and then look for the variables you don’t want. You ca

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極地渦旋 極地渦旋（Polar Vortex；或極地漩渦），是一種發生於極地的，介於對流層與平流層的中、上部的，持續性且大規模的氣旋。這種渦旋在冬季極夜的時候最為強大，因為此時的溫度梯度最大；隨後會持續縮減，到夏季極晝前後甚至會消失。 兩極對流層中層至平流層的低氣壓系統 典型的極地漩渦（2013年11月） 弱勢的極地漩渦（2014年1月5日） 極地渦旋（Polar Vo

Siberian high | 蒙古西伯利亞高壓 西伯利亞高壓（Siberian High），又稱蒙古高壓、蒙古冷高壓、西伯利亞反氣旋 冷高壓（Siberian Anticyclone），是一種位於歐亞大陸東北區域，發生在九月到次年四月的半永久性大陸反氣旋。在夏季，溫暖潮濕的氣流自太平洋流向西伯利亞。而在冬季則正好相反。這種變化是因為海洋和陸地的比熱熔差異，再加上歐亞大陸非常特殊的地理環境而造就的

副熱帶高壓 亞熱帶高壓（Subtropical high，又稱亞熱帶高氣壓、副熱帶高壓、副熱帶高氣壓），其脊線稱為副熱帶高壓脊，氣象學名詞，是指活躍於亞熱帶地區的高壓脊，分佈於南北緯30°左右，是一股經常存在但位置不固定的溫暖氣團。它的位置以及內裏氣流的流向可以影響到熱帶氣旋的生成和走向。 為動力成因，地球在赤道附近接收的熱輻射最大，導致出現沿熱帶輻合帶的大量對流。這裏的氣團上升然後發散，受地轉偏

Embed Google Maps Easily embed and customize Google Maps on your web page or blog by setting the Google. To use the Maps Embed API on your web page, set the URL you've built as the value of an iframe'

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Differences Between Weather Models and Climate Models Understanding the distinctions between weather models and climate models is crucial for grasping how meteorologists and climate scientists predict