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Geology topics

P. Douglas Reimer

Publications and source records attributed to P. Douglas Reimer.

2 recordsLinked to original sources

Morphodynamics of the Isles Dernieres barrier shoreline, Louisiana. 1984-1989

An aerial videotape mapping system was used to monitor spatial and temporal variability of the coastal morphology along the Isles Dernieres barrier shoreline. Between 1984 and 1989, nine sequential annual and post-hurricane aerial videotape surveys were flown covering periods of prolonged fair weather, hurricane impacts, and subsequent post-storm recovery. Morphologic time series were developed to depict spatial and temporal geomorphic changes along the Isles Dernieres low-profile transgressive barrier island system. The net effect of Hurricanes Danny and Juan, in 1985, was the transformation of a high relief landscape dominated by well-vegetated dunes, dune terraces, and washover terraces to one dominated by partially-vegetated washover terraces and unvegetated washover flats. In 1988, Hurricane Gilbert caused extensive geomorphic changes in the central Isles Dernieres where the low-relief, less-vegetated islands were more susceptible to storm-surge processes. Post-storm island morphodynamics were characterized by a gradual build up of the low-relief landforms to high-profile features. The greatest post-storm recovery consistently occurred in areas of greater island width and relief. In addition, the rate of post-storm recovery was controlled by the regional setting of individual islands relative to sand supply. The degree of post-storm recovery was consistently greater in areas where hurricane impact had caused greatest geomorphic change.

Conference Paper

Morphodynamic signature of the 1985 hurricane impacts on the northern Gulf of Mexico

Three hurricanes hit Lousiana (LA), Mississippi (MS), Alabama (AL), and the Florida (FL) panhandle in 1985, producing dramatic geomorphic changes in a wide variety of coastal environments. The impact zone for hurricanes Danny, Elena, and Juan stretched 1000 km between the Sabine River in LA to the Apalachicola River in FL. Barrier shorelines experienced repeated intense overwash events, producing beach and dune erosion exceeding 30 m, as well as producing classic examples of storm surge deposits. Pre- and post-storm airborne videotape surveys, sequential vertical mapping photography, and field surveys provide the data base for this regional hurricane impact assessment on the northern Gulf of Mexico. Hurricane impacts on the low-profile and high-profile barrier shorelines, as well as on the marine terrace cliffs were systematic and predictable. Controlling the direction of overwash flow and the impact distribution pattern is the relationship among shoreline orientation, hurricane storm track, and regional wind field. The relationship between shore-zone geomorphology and storm surge overwash controls the impact response.

Conference Paper