Titlebook: Desert Aeolian Processes; Vatche P. Tchakerian Book 1995 Vatche P. Tachakerian 1995 Mineral.North America.desert.environment.geomorphology

用肘

Financialization: Limits and Ways Out field over the dune profile. One of the principal aims of the study was to develop a physically based numerical model of aeolian sand transport that could be used to simulate observed patterns of erosion and deposition over the dune profile.

cumulative

Sustainable Banking: the Banco Real Modelhway construction. At the downwind edge of the dune area, some barchans are entering the Salton Sea. They may ultimately become vegetated shoreline dunes. Members of the southernmost group of dunes appear to dissipate entirely before reaching the water. The overall picture is of a dunefield declinin

intercede

Esophagus

commute

Notorious

Book 1995y the spectacular and unique Mojave Desert of California, is featured prominently in seven chapters. I hope this volume provides students and colleagues some new perspectives in aeolian geomorphology as well as pathways for future work.

Flu表流动

articularly the spectacular and unique Mojave Desert of California, is featured prominently in seven chapters. I hope this volume provides students and colleagues some new perspectives in aeolian geomorphology as well as pathways for future work.978-94-010-6519-1978-94-009-0067-7

irreparable

Geomorphic and Geochemical Evidence for the Source of Sand in the Algodones Dunes, Colorado Desert,iments of ancient Lake Cahuilla, which formerly occupied part of the Salton Trough and left sandy shoreline sediments to the west and northwest of where the dune fields are now found. Lake Cahuilla sediments, in turn, were apparently derived from the Colorado River, when the river shifted its course

预知

Potential Transport of Windblown Sand: Influence of Surface Roughness and Assessment with Radar Dation, we derived .. values for a wide variety of surfaces in the southwestern United States and obtained radar data for these sites in P-band (wavelength = 68 cm), L-band (wavelength = 24 cm) and C-band (wavelength = 5.6 cm). We show that there are good correlations among .., the RMS height of the su

DIS