多雨带
多雨带-
相对多雨带与低层流场辐合线有很好的对应关系。
The eastern rain-belts are closely related with low level flow convergence line .
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当冬季北太平洋涛动偏弱时，夏季主要多雨带位于黄河与长江之间，中心在淮河流域一带（即2类雨型）。
Yellow River and the Changjiang River in summer ( Rainfall pattern 2 ) when NPO is weaker than normal in winter .
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结果表明，当冬季北太平洋涛动偏强时，我国夏季主要多雨带位于黄河流域及其以北地区（即1类雨型）；
The results indicate that , the major rain belt is located in or north to the Yellow River Valley in summer ( Rainfall pattern 1 ) when NPO is stronger than normal in winter , while the major rain belt occurs between the .