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[18], '基于': [20], '被划分成四个组:(1': [22], '弱': [24, 42], 'EAWMres-El': [25, 34], 'Ni': [26, 35, 44, 52, 67, 74, 89, 95], '?': [27, 36, 45, 53, 71, 75, 91, 96], 'o': [28, 37, 72, 92], '(WEAWMres': [29], '在)': [30, 39], ';(2': [31], '强壮的': [33, 50], '(SEAWMres-': [38], ';(3': [40], 'EAWMres-La': [43, 51], '一(WEAWMres': [46], '行)': [47, 55], ';(4': [48], '一(SEAWMres': [54], '。合成结果证明': [56], '可以为': [58], 'WEAWMres': [59, 78, 84, 100], '在和': [60, 83], 'SEAWMres': [61, 80, 82, 102], '行在东亚上提高大气的回答到': [62], 'ENSO。相应低级逆旋风(气旋)': [63], '在西方的诺思太平洋(WNP': [64], '上的异例把': [66], '与': [68], 'El': [69, 88], '联系了': [70], '(La': [73], '一)': [76], '趋于强壮。重要地,这个特征可以坚持直到下列夏天,引起在为': [77], '在案例的北中国并且在为': [79], '行案例的西南的中国的丰富的降雨。为': [81], '行组,相反,': [85], '趋于削弱与': [87], '联系的大气的发行量异例': [90], '或': [93], 'La': [94], '一。在这些,情况,异常': [97], 'WNP': [98], '反气旋或气旋趋于被减少并且限制了降低纬度,它为': [99], '行为': [101], '在并且在西南的中国在北中国导致缺乏的夏天降雨。进一步的学习建议异常': [103], '可以在热带以外的海表面温度异例上有效果,它坚持直到随后的夏天并且可以防碍': [105], '的影响。': [107]}, 'cited_by_api_url': 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