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dc.contributor.authorHall, Timothy
dc.contributor.authorTippett, Michael K.
dc.date.accessioned2017-06-09T16:51:31Z
dc.date.available2017-06-09T16:51:31Z
dc.date.copyright2017/03/01
dc.date.issued2016
dc.identifier.issn1558-8424
dc.identifier.otherams-75394.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4217725
dc.description.abstractstatistical model of northeastern Pacific Ocean tropical cyclones (TCs) is developed and used to estimate hurricane landfall rates along the coast of Mexico. Mean annual landfall rates for 1971?2014 are compared with mean rates for the extremely high northeastern Pacific sea surface temperature (SST) of 2015. Over the full coast, the mean rate and 5%?95% uncertainty range (in parentheses) for TCs that are category 1 and higher on the Saffir?Simpson scale (C1+ TCs) are 1.24 (1.05, 1.33) yr?1 for 1971?2014 and 1.69 (0.89, 2.08) yr?1 for 2015?a difference that is not significant. The increase for the most intense landfalls (category-5 TCs) is significant: 0.009 (0.006, 0.011) yr?1 for 1971?2014 and 0.031 (0.016, 0.036) yr?1 for 2015. The SST impact on the rate of category-5 TC landfalls is largest on the northern Mexican coast. The increased landfall rates for category-5 TCs are consistent with independent analysis showing that SST has its greatest impact on the formation rates of the most intense northeastern Pacific TCs. Landfall rates on Hawaii [0.033 (0.019, 0.045) yr?1 for C1+ TCs and 0.010 (0.005, 0.016) yr?1 for C3+ TCs for 1971?2014] show increases in the best estimates for 2015 conditions, but the changes are statistically insignificant.
dc.publisherAmerican Meteorological Society
dc.titlePacific Hurricane Landfalls on Mexico and SST
dc.typeJournal Paper
dc.journal.volume56
dc.journal.issue3
dc.journal.titleJournal of Applied Meteorology and Climatology
dc.identifier.doi10.1175/JAMC-D-16-0194.1
dc.journal.fristpage667
dc.journal.lastpage676
dc.treeJournal of Applied Meteorology and Climatology:;2016:;volume( 056 ):;issue: 003
dc.contenttypeFulltext


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