-1之間的概率最大,極端強(qiáng)對(duì)流性降水發(fā)生在陸地上的概率大于海洋。對(duì)流性降水的日變化表現(xiàn)為,陸地上于傍晚(18—20時(shí))和夜間(22—01時(shí))有兩個(gè)峰值;海洋上對(duì)流性降水多出現(xiàn)于夜間到早晨這段時(shí)間,而下午出現(xiàn)的概率最低。厄爾尼諾發(fā)展年,海洋上對(duì)流性降水增強(qiáng),而陸地上發(fā)生的概率總體偏小,衰減年則相反;中國(guó)東部,尤其是長(zhǎng)江以南地區(qū)的非對(duì)流性降水在厄爾尼諾發(fā)展年,多于正常年,與對(duì)流性降水的響應(yīng)不一致。"/>
國(guó)家重點(diǎn)基礎(chǔ)研究計(jì)劃(973計(jì)劃)項(xiàng)目(2015CB453200);國(guó)家自然科學(xué)基金資助項(xiàng)目(41730961;41575083;41575108)
孫齊穎,余錦華,祁淼,張婉瑩.北半球夏季對(duì)流性降水特征及其與厄爾尼諾的關(guān)系.氣象科學(xué),2017,37(6):776-783 SUN Qiying, YU Jinhua, QI Miao, ZHANG Wanying. Characteristics of summer convective precipitation in the northern hemisphere and its relationship with El Niño. Journal of the Meteorological Sciences,2017,37(6):776-783
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