Exact(1)
Probabilistic correlation among mesoscale typhoon field parameters was taken into account.
Similar(59)
This and other oceanic responses to a TC have been the subjects of numerous studies (e.g., Shay 2010), and highly complex physical processes associated with typhoon-ocean interactions have recently been investigated in a large typhoon-ocean field experiment ('Impact of Typhoons on the Ocean in the Pacific') (D'Asaro et al. 2011; Pun et al. 2011).
A novel typhoon velocity field model suitable for the gradient layer and boundary layer was then established considering the multi-field parameters correlation and terrain effects.
The typhoon wind field module generates typhoon-lifetime maximum 5-s gust wind speed for each 1-km grid based on a parametric wind field model (Vickery, Skerjl, and Twisdale 2000; Vickery et al. 2000; Lin 2014).
Furtherly, case studies of the specific typhoon wind field was re-illustrated and compared with the observed wind speed profiles averaged from upper-level dropsondes data and low-level profiles measured by meteorological towers.
This paper developed the analytic model of radial atmospheric pressure distribution originally proposed by Holland and discussed the distribution factor of radial typhoon pressure field (also referred to as Holland parameter β).
In this study, the typhoon wind fields over varied types of terrains are revealed, the structural dynamic properties of the super-tall building as well as its serviceability are evaluated, and finally wind tunnel predictions of structural responses are validated by the field measurements from SHM system.
The simulation results of real application demonstrate the effectiveness and applicability of the framework, which provides a cross-scale simulation capability of reproducing typhoon wind fields.
Finally, the proposed spectral model is validated using arbitrarily selected four hours of data in different sectors of typhoon Hagupit wind field.
Based on our field work, Typhoon Haiyan exerted direct damage in habitats containing five Cycadaceae species and 70 species and infraspecific taxa of Arecaceae.
In the present study, the after-runner surge that maximum surge height appears 15 18 h later along the Tottori coasts facing the Sea of Japan/East Sea (SJES) after typhoons undergo a change in shape and intensity as extratropical cyclones is investigated using asymmetric and symmetric wind and pressure fields of Typhoon Songda (2004).
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