In this study, two methods used to estimate surface terrain conditions (z0) surrounding Automated Surface Observing System (ASOS) stations in tropical cyclone-prone regions were analyzed. The first method utilized ground-based photography from the National Oceanic and Atmospheric Administration Hurricane Research Division's Tropical Cyclone Wind Exposure Documentation Project (WEDP). The second applied a modified effective z0 method using ASOS wind data. Comparisons reveal that WEDP z0 estimates are typically larger in magnitude and do not account for changes in upstream z0. Variability in the z0 estimates showed a distinctly skewed nature in the probability distributions, which may have some physical meaning. It was also shown that standar...
Surface roughness values for the areas surrounding the H, D and N-Area meteorological towers were co...
Information of temporal and spatial variation of aerodynamic roughness length is required in most la...
Hurricane Andrew’s landfall in south Florida left a swath of destruction, including many failed anem...
A set of velocity-azimuth display (VAD) wind speed profiles derived from coastal Weather Surveillanc...
Aerodynamic roughness length (z0) and displacement height (d0) are important surface parameters for ...
Monin-Obukhov similarity theory and the empirical formulae of Businger et al. (1971) and Dyer (1974)...
Surface roughness plays a key role in determining aerodynamic roughness length (zo) and shear veloci...
Hurricanes are one of the deadliest and costliest natural hazards affecting the Gulf coast and Atlan...
The aerodynamic roughness length (z0m) is a crucial parameter for reliably simulating turbulent exch...
Aerodynamic roughness length (z(0)) is one of the main parameters for describing aerodynamic charact...
Accurate measurements of surface observations are necessary for development of numerical weather pre...
The Fujita Scale, and subsequently the Enhanced Fujita Scale, were developed to enable maximum proba...
In modelling wind flow over a flat and complex terrain, the choice of roughness-length-distribution ...
Hurricane Andrew’s landfall in south Florida left a swath of destruction, including many failed anem...
Most land surface models require information on aerodynamic roughness length and its temporal and sp...
Surface roughness values for the areas surrounding the H, D and N-Area meteorological towers were co...
Information of temporal and spatial variation of aerodynamic roughness length is required in most la...
Hurricane Andrew’s landfall in south Florida left a swath of destruction, including many failed anem...
A set of velocity-azimuth display (VAD) wind speed profiles derived from coastal Weather Surveillanc...
Aerodynamic roughness length (z0) and displacement height (d0) are important surface parameters for ...
Monin-Obukhov similarity theory and the empirical formulae of Businger et al. (1971) and Dyer (1974)...
Surface roughness plays a key role in determining aerodynamic roughness length (zo) and shear veloci...
Hurricanes are one of the deadliest and costliest natural hazards affecting the Gulf coast and Atlan...
The aerodynamic roughness length (z0m) is a crucial parameter for reliably simulating turbulent exch...
Aerodynamic roughness length (z(0)) is one of the main parameters for describing aerodynamic charact...
Accurate measurements of surface observations are necessary for development of numerical weather pre...
The Fujita Scale, and subsequently the Enhanced Fujita Scale, were developed to enable maximum proba...
In modelling wind flow over a flat and complex terrain, the choice of roughness-length-distribution ...
Hurricane Andrew’s landfall in south Florida left a swath of destruction, including many failed anem...
Most land surface models require information on aerodynamic roughness length and its temporal and sp...
Surface roughness values for the areas surrounding the H, D and N-Area meteorological towers were co...
Information of temporal and spatial variation of aerodynamic roughness length is required in most la...
Hurricane Andrew’s landfall in south Florida left a swath of destruction, including many failed anem...