2014
DOI: 10.1371/journal.pone.0091306
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Modelling Hurricane Exposure and Wind Speed on a Mesoclimate Scale: A Case Study from Cusuco NP, Honduras

Abstract: High energy weather events are often expected to play a substantial role in biotic community dynamics and large scale diversity patterns but their contribution is hard to prove. Currently, observations are limited to the documentation of accidental records after the passing of such events. A more comprehensive approach is synthesising weather events in a location over a long time period, ideally at a high spatial resolution and on a large geographic scale. We provide a detailed overview on how to generate hurr… Show more

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Cited by 20 publications
(33 citation statements)
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“…The x is a constant that is estimated to be 0.7 by Batke et al . (). Fifty kilometer wide buffers around each storm track were created using the R package “rgeos.” Wind speeds were calculated for each point within the storm track.…”
Section: Methodsmentioning
confidence: 97%
See 1 more Smart Citation
“…The x is a constant that is estimated to be 0.7 by Batke et al . (). Fifty kilometer wide buffers around each storm track were created using the R package “rgeos.” Wind speeds were calculated for each point within the storm track.…”
Section: Methodsmentioning
confidence: 97%
“…Equation (1) was used when r > Rmax, and Equation (2) when r < Rmax. The x is a constant that is estimated to be 0.7 by Batke et al (2014). Fifty kilometer wide buffers around each storm track were created using the R package "rgeos."…”
Section: Storm Exposure Sensitivity and Adaptive Capacitymentioning
confidence: 99%
“…The wind speeds profile of a storm can be generated through parametric radial wind field models (Davis, Wang et al 2008, Holland, Belanger et al 2010, Batke, Jocque et al 2014). The wind speed at location ( , ) at time can be represented by Holland, Belanger et al (2010)…”
Section: Threat Characterizationmentioning
confidence: 99%
“…where is the distance from the point to the storm center ( ), ( ) , which moves with the translational velocity of the storm, is the maximum wind speed, is the radius of maximum wind (also called wind radius) and can be calculated from the storm eye-diameter (ED) (Batke, Jocque et al 2014), is the empirical Holland parameter and can be estimated based on the central pressure of the storm, and is a scaling parameter that adjusts the wind profile shape and a value of = 0.5 is typically used (Holland, Belanger et al 2010). Structural damage from windstorms is mostly related to peak gust wind speed, which is the largest speed during a specified period (usually 3 seconds).…”
Section: Threat Characterizationmentioning
confidence: 99%
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