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Global assessment of tropical cyclones intensity statistical-dynamical hindcasts

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dc.contributor.author Neetu, S.
dc.contributor.author Lengaigne, M.
dc.contributor.author Menon, H.B.
dc.contributor.author Vialard, J.
dc.contributor.author Mangeas, M.
dc.contributor.author Menkes, C.E.
dc.contributor.author Ali, M.M.
dc.contributor.author Suresh, I.
dc.contributor.author Knaff, J.A.
dc.date.accessioned 2017-08-31T07:30:51Z
dc.date.available 2017-08-31T07:30:51Z
dc.date.issued 2017
dc.identifier.citation Quarterly Journal of the Royal Meteorological Society. 143(706); 2017; 2143-2156. en_US
dc.identifier.uri http://dx.doi.org/10.1002/qj.3073
dc.identifier.uri http://irgu.unigoa.ac.in/drs/handle/unigoa/4889
dc.description.abstract This paper assesses the characteristics of linear statistical models developed for Tropical Cyclones (TC) intensity prediction at global scale. To that end, multi-linear regression models are developed separately for each TC-prone basin to estimate the intensification of a TC given its initial characteristics and environmental parameters along its track. We use identical large-scale environmental parameters in all basins, derived from a 1979–2012 reanalysis product. The resulting models display comparable skill to previously-described similar hindcast schemes. Although the resulting mean absolute errors are rather similar in all basins, the models beat persistence by 20-40 percent in most basins, except in the north Atlantic and northern Indian Ocean, where the skill gain is weaker (10-25 percent). A large fraction (60 to 80 percent) of the skill gain arises from the TC characteristics (intensity and its rate of change) at the beginning of the forecast. Vertical shear followed by the maximum potential intensity are the environmental parameters that yield most skill globally, but with individual contributions that strongly depend on the basin. Hindcast models built from environmental predictors calculated from their seasonal climatology perform almost as well as when using real-time values. This has the potential to considerably simplify the implementation of operational forecasts in such models. Finally, these models perform poorly to predict intensity changes for Category 2 and weaker TC, while they are 2 to 4 times more skilful for the strongest TC (Category 3 and above). This suggests that these linear models do not properly capture the processes controlling the early stages of TC intensification. en_US
dc.publisher Royal Meteorological Society, London en_US
dc.subject Marine Sciences en_US
dc.title Global assessment of tropical cyclones intensity statistical-dynamical hindcasts en_US
dc.type Journal article en_US
dc.identifier.impf y


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