C-Band Solid State TWT Replacement

Harris, Micky; Tsai, W.C.; Paik, Seungwhun

doi:10.1109/mwsym.1975.1123287

Cited by 3 publications

(1 citation statement)

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“…Normally the higher and steeper parts of the system are characterized by erosion processes. Although debris flows may be triggered by rapid melting of snow and (or) ground ice (Harris and Gustafson, 1988) they normally occur as a reaction to 'high-intensity' rainstorms (Caine, 1980). The minimum intensity required may be low under permafrost conditions or where deep seasonal frost exists (cf.…”

Section: Debris Flowsmentioning

confidence: 99%

Models for the genetic and environmental interpretation of stratified slope deposits: Review

Steijn

Bertrán

Francou³

et al. 1995

Permafrost & Periglacial

116

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The principal aspects addressed are the relationships between transport processes and depositional environments, and the sedimentary properties of the deposits. The following 'process-product' models are discussed: (a) stone-banked solifluction sheets or lobes, (b) dry grain flows and frost-coated clast flows, (c) debris flows, and (d) niveo-aeolian transport within the context of talus development. Problems of convergence, the possible role of other processes, and the climatic significance of stratified slope deposits are briefly discussed. RBSUMBCet article traite des modkles concernant la genCse et l'interprbtation environnementale des dCp6ts de versant stratifiks. Les relations des mdcanismes de transport avec, d'une part, les milieux de stdimentation et, d'autre part, les CaractCristiques stdimentologiques, sont dCcrites. Toutes les donnCes prCsentCes ici proviennent d'btudes rCalisCes en milieux actifs. Les modbles gknttiques et skdimentologiques trait& sont les suivants: (a) nappe-coulkes et lobes de solifluxion h front pierreux, (b) coulCes de pierres skches et coulCes de pierres glades, (c) flots de dCbris, et (d) transport nivCo-tolien sur un talus. A la fin de cet article, sont tvoquks les problkmes de convergence, le r61e possible de mCcanismes stdimentaires non intCgrCs dans les modCles, ainsi que le problCme de la signification climatique des dCp6ts stratifits. Ce bilan global peut donc servir de base introductive A I'interprCtation de cas concrets.

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Section: Debris Flowsmentioning

confidence: 99%