CAJ | 학술논문

2011年6月上、中旬，钱塘江流域连降暴雨，形成降雨总量大、影响范围广的特点，致使该流域发生流域性的洪水，钱塘江干流各主要控制站洪水位仍然普遍超过保证水位，其中钱塘江干流兰溪站出现1955年以来最高洪水位，分析认为，导致兰溪站“小流量高水位”的原因与洪水本身量级、降雨雨型、河道行洪能力以及近年来堤防等的建设有关．
2011년6월상、중순，전당강류역련강폭우，형성강우총량대、영향범위엄적특점，치사해류역발생류역성적홍수，전당강간류각주요공제참홍수위잉연보편초과보증수위，기중전당강간류란계참출현1955년이래최고홍수위，분석인위，도치란계참“소류량고수위”적원인여홍수본신량급、강우우형、하도행홍능력이급근년래제방등적건설유관．
In the first 20 days in June, 2011 , heavy rainstorm hit Qiantang Basin with extreme rainfall quantum and wide range affect, resulting in flood in Qiantang Basin. The flood level in main flood-control stations is generally beyond the guarantee level, especially in Lanxi Station, the main stream of Qiantang River, hitting the highest flood level since 1955. The reason of "small flow and high water level" in Lanxi station is analyzed in this paper in perspectives of flood scale, rainfall type, river flood discharge capacity and the construction of the embankment and relevant in recent years.