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Landfalling tropical cyclones on the Pacific coast of Mexico: 1850-2010

机译:登陆墨西哥太平洋海岸的热带气旋:1850-2010年

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Historical documents and newspapers from Mexican Pacific states (north of 14° N) were reviewed to determine the incidence of landfalling tropical cyclones from 1850 to 1949, prior to the start of the United States National Hurricane Center database. The reviewed documents are only found in Mexican repositories at national, state and municipal level and the systematic search embarked upon in this study yielded valuable information that cannot be found elsewhere. A time series of landfall was reconstructed back to 1850, indicating active and quiet periods. An average of 1.8 ± 1.6 landfalls per year is determined from the time series for 1850-2010. When the series is limited to 1880-2010, eliminating the first 30 years that may have some undercounting, the average increases to 2.1 ± 1.6 cases per year. Spectral and wavelet analysis of the 161 years of landfalling tropical cyclones indicates that the Pacific Decadal Oscillation (PDO) modulates the activity. The influence of El Ni?o/Southern Oscillation (ENSO) and the North Atlantic Oscillation (NAO) on the landfall frequency may be present throughout the reconstruction period but both oscillations have lower correlations compared to that from the PDO.
机译:在启动美国国家飓风中心数据库之前,对墨西哥太平洋各州(北纬14°以北)的历史文献和报纸进行了审查,以确定1850年至1949年登陆热带气旋的发生率。审阅过的文档仅在国家,州和市级的墨西哥存储库中找到,本研究中进行的系统搜索产生了在其他地方找不到的有价值的信息。登陆的时间序列可以追溯到1850年,表示活跃和安静的时期。根据1850-2010年的时间序列,平均每年有1.8到1.6次登陆。当系列仅限于1880-2010年时,排除了可能被低估的前30年,则平均每年增加到2.1±1.6例。对161年登陆热带气旋的光谱和小波分析表明,太平洋年代际振荡(PDO)调节了该活动。厄尔尼诺/南方涛动(ENSO)和北大西洋涛动(NAO)对登陆频率的影响可能在整个重建期间都存在,但与PDO相比,这两种振荡的相关性都较低。

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