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skewness
Bandwidth-insensitive extended centroid frequency-shift method for near-surface Q estimation
An H/V geostatistical approach for building pseudo-3D Vs models to account for spatial variability in ground response analyses Part I: Model development
Heavy Mineral Analysis of Jamuna River Sediments, Bangladesh
A Probabilistic Framework to Model Distributions of V S 30
Textural Analysis of Coastal Sediments along East Coast of India
Skew Normal Distribution Deconvolution of Grain-size Distribution and Its Application To 530 Samples from Lake Bosumtwi, Ghana
Comparing the CENA GMPEs Using NGA‐East Ground‐Motion Database
Value of information analysis and Bayesian inversion for closed skew-normal distributions: Applications to seismic amplitude variation with offset data
Local skewness attribute as a seismic phase detector
Simulating the impacts of small convective storms and channel transmission losses on gully evolution
Abstract Gullies are common features throughout the southwestern United States including Army training facilities such as the Pinon Canyon Maneuver Site. These gullies have depths up to several meters, which can restrict the mobility of troops and vehicles during training exercises. They also have the potential to grow in size, which can degrade training lands. At the upstream end, gullies usually begin with an abrupt headwall, and in the downstream direction, gullies also tend to terminate abruptly. In this paper, we hypothesize that the small extent of convective storms and significant transmission losses in channels promote the downstream disappearance of gullies. The role of these factors is tested by applying a geomorphic model in which storms occur within circular portions of the simulation domain and channel flow is lost to seepage up to a specified infiltration or seepage capacity in each grid cell. The net effect of these processes is to reduce the sediment transport capacity in the downstream direction relative to the case with an infinite storm size and no channel losses. The reduced sediment capacity alters the relationship between slope and drainage area for topographies at equilibrium. In addition, limited storm sizes can also produce disconnected areas of incision within generally depositional portions of the landscape.