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dc.contributor.authorTao, Dandan
dc.contributor.authorNystrom, Robert
dc.contributor.authorBell, Michael
dc.date.accessioned2023-12-15T13:57:10Z
dc.date.available2023-12-15T13:57:10Z
dc.date.created2023-10-12T11:30:07Z
dc.date.issued2023
dc.identifier.issn0094-8276
dc.identifier.urihttps://hdl.handle.net/11250/3107851
dc.description.abstractTropical cyclone (TC) low-level tangential wind structure is known to be an important input for risk assessment (e.g., storm surge). However, a realistic TC wind structure model with easy implementation is still needed for many applications. In this study, we obtain an inner-core wind structure model purely from an empirical approach, which significantly reduces the complexity of TC wind profiles. From idealized simulations with different initial vortex structures, it is found that the absolute angular momentum (M) outside the radius of maximum wind (rm) is quasi-linear. This quasi-linear M slope in a normalized coordinate decreases with TC intensity. The consequent linear M slope wind model can largely capture the simulated TC inner-core wind structure and has the potential for many practical applications.en_US
dc.language.isoengen_US
dc.publisherAGUen_US
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/deed.no*
dc.titleThe Quasi-Linear Absolute Angular Momentum Slope of Tropical Cyclones Under Rapid Intensificationen_US
dc.typeJournal articleen_US
dc.typePeer revieweden_US
dc.description.versionpublishedVersionen_US
dc.rights.holderCopyright 2023 The Author(s)en_US
dc.source.articlenumbere2023GL104583en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2
dc.identifier.doi10.1029/2023GL104583
dc.identifier.cristin2184065
dc.source.journalGeophysical Research Lettersen_US
dc.identifier.citationGeophysical Research Letters. 2023, 50 (16), e2023GL104583.en_US
dc.source.volume50en_US
dc.source.issue16en_US


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Attribution-NonCommercial-NoDerivatives 4.0 Internasjonal
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