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登陆 (气象学)

飓风玛丽亚原有的出色结构在登陆波多黎各之后立即瓦解

登陆(英文:Landfall),为气象学术语,意思为在海上形成的风眼越过海岸线

北半球的台风飓风形成后,会在大气环流和科里奥利力的影响下逆时针旋转,从热带海面向西方或西北方运动。南半球的飓风则顺时针旋转,向东方或东南方运动。

在西北太平洋和中国南海形成的台风向西北方运动时,可能穿过台湾海峡在中国东南沿海登陆,或在台湾登陆,或转向日本登陆,或在南亚次大陆、东南亚登陆;少数台风径直向北在中国辽宁、山东登陆。在北印度洋形成的台风可能在南亚或西亚登陆。

大西洋加勒比海、东北太平洋形成的飓风可能在太平洋诸岛、美国墨西哥等处登陆。在南印度洋与南太平洋形成的飓风可能在澳大利亚或东南亚登陆。

风暴靠近陆地或登陆时,风暴附近风力强大,会给地面房屋、设施带来破坏。

参阅

参考资料

  • 中国气象局(2001年),《台风业务和服务规定》,气象出版社
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登陆 (气象学)
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