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梅雨季節來的不乾脆？鄭明典曝「季風轉變」關鍵：南亞反氣旋仍偏西
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生活中心／李明融報導
台灣正式進入梅雨季節，不過今年似乎來得不是很乾脆，氣象局長鄭明典今天（10日）在臉書上發文指出，現在的南亞反氣旋還是偏西，對於每年5、6月台灣梅雨季節到來的主要關鍵，鄭明典表示季風可能不會變得很乾脆，「或許需要再一小段時間醞釀」。
南亞反氣旋和梅雨季的關係，鄭明典解釋「梅雨是亞澳季風的季節轉變過程中的一個階段性天氣特徵」，季風可以看成是個季節性的海陸風，冬季陸地冷、海洋暖，所以低層空氣由陸地吹往海洋(相當於陸風)；夏季時路地熱，海洋涼，所以低層空氣由海洋吹向陸地(相當於海風)，亞澳季風之所以會是全球最顯著的季風系統，最關鍵就是在青藏高原。
因為太陽直接加熱空氣的效率很低，太陽的能量是由地表吸收再加熱地表上方的大氣。夏季青藏高原是個突出的熱源，沒有競爭對手，因此成為一個全球最顯著的熱源，這個熱源反映出來的就是夏季青藏高原上方持續的大尺度上升氣流，也因此在接近對流層頂的地方出現大大的「南亞反氣旋」，或直接稱「青藏高壓」。
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