Severe Wind Hazard Maps

The Regional Severe Wind Hazard maps represent the 3-second peak gust wind speed measured at 10-meter height (above ground) over open and flat terrain. This does not take into account the local factors such as topography, terrain roughness and shielding from neighboring structures. In order to generate the regional severe wind hazard, the Tropical Cyclone Risk Model (TCRM), developed by Geoscience-Australia (GA) was used. The model uses statistical and parametric models to simulate the behavior of thousand years of cyclonic activities. Powell (2005) parametric wind field and Kepert (2001) boundary layer models were employed for each tropical cyclone. Figure 1 below shows the schematic diagram of the Tropical Cyclone Risk Model (TCRM) in simulating the probabilistic regional wind field of tropical cyclones. The historical tropical cyclone track dataset that entered the Philippine Area of Responsibility (PAR) from 1951 to 2020 was used to derive the wind hazard (Monteverde et al., 2021).


Furthermore, the wind speeds from all events are fitted to the Generalized Extreme Value (GEV) distribution to determine an average recurrence interval or annual exceedence probability for a given wind speeds. The model output is combined with the analysis of the observed maximum wind speed (3-second peak gust) to adjust the various return periods (RPs) of maximum wind gust, which are determined using a Generalized Pareto Distribution (GPD). The model generated the regional wind speed and utilized distribution of tropical cyclone properties (speed, bearing, and intensity) developed on a grid covering the PAR.


The regional severe wind hazard maps are expressed in terms of return periods (RPs). These wind fields show the probability of any given magnitude that may occur in any given year. Various RPs were derived in the study such as 20-, 50-, 100-, 200-, and 500 -year return periods . Return period wind fields were computed by getting an average over a duration of time and extrapolated to calculate the probable distribution of wind speeds across the country.


The regional severe wind hazard maps will provide a valuable source of information that will serve as a guide for disaster managers and planners for future tropical cyclone emergency planning and for disaster risk reduction. This will also identify areas likely to suffer significant wind damage due to tropical cyclone severe winds and to prepare the community to understand the behavior and characteristics of tropical cyclone winds. In addition, it will also enable the disaster planners/managers to build a wind-proof community and minimize the damaging effects of tropical cyclone wind, and make informed decisions.


The Local Severe Wind Hazard Maps refer to the wind incident on the surface. This is obtained by combining the maximum 3-second peak gust (Regional winds) with local site-multipliers to account for the decreasing effect of various terrain (land cover types) with height, decreasing effect of the upwind building, and the increasing effect of the undulating topography. This is derived from the historical tropical cyclone tracks that entered the Philippine Area of Responsibility (PAR) covering the period of 1951 to 2020.


These severe wind hazard maps are also expressed in terms of Return Periods (RPs) defined as the average time interval between events of a certain magnitude being exceeded at a particular location such as 20-, 50-, 100-, 200-, and 500-year RPs. It can also be expressed in terms of annual exceedance probability (AEP) which tells the likelihood of happening or exceeding in any given year.


The Local Severe Wind Hazard Maps provide crucial guidance for site-specific wind estimates and support activities like planning and risk assessments.