A5054181787- Geology and Paleoclimatology Research
- Cryospheric studies and observations
- Arctic and Antarctic ice dynamics
- Geological formations and processes
- Polar Research and Ecology
- Methane Hydrates and Related Phenomena
- Reservoir Engineering and Simulation Methods
- Geological Studies and Exploration
- Aeolian processes and effects
- Adipose Tissue and Metabolism
- Wildlife Ecology and Conservation
- Species Distribution and Climate Change
- Geophysical and Geoelectrical Methods
- Marine and environmental studies
- Scientific Measurement and Uncertainty Evaluation
- Coastal and Marine Dynamics
- Fire effects on ecosystems
- Fault Detection and Control Systems
- Geophysics and Gravity Measurements
- Climate change and permafrost
University of Houston
2014-2021
Halliburton (United States)
2020
Mapped topographic features are important for understanding processes that sculpt the Earth's surface. This paper presents maps primary product of an exercise brought together 27 researchers with interest in landform mapping wherein efficacy and causes variation were tested using novel synthetic DEMs containing drumlins. The between interpreters (e.g. philosophy, experience) across study region woodland prevalence) opens these factors up to assessment. A priori known answers synthetics...
Abstract. Glacial geomorphology is used in Antarctica to reconstruct ice advance during the Last Maximum and subsequent retreat across continental shelf. Analogous geomorphic assemblages are found glaciated fjords interpret glacial history dynamics those areas. In addition, understanding distribution of submarine landforms bays local controls exerted on flow can help improve numerical models by providing constraints through these drainage We present multibeam swath bathymetry from several...
We analyse surface sediment and its distribution in Flandres Bay, West Antarctic Peninsula, order to understand modern day dispersal patterns a fjord with retreating, tidewater glaciers. The descriptions of 41 cores are included this study. facies described include muddy diatomaceous ooze, mud, pebbly sandy mud scattered pebbles present most samples. In contrast traditional conceptual model glacial fjords, grain size Bay generally coarsens from the inner outer bay. smallest sediments were...
Abstract. Glacial geomorphology has been used in Antarctica to reconstruct ice advance and retreat across the continental shelf during Last Maximum. Analogous geomorphic assemblages are found glaciated fjords can be a similar manner interpret glacial history those areas. In addition, understanding distribution of submarine landforms bays local controls exerted on flow help improve ice-sheet models through these complicated drainage We present multibeam swath bathymetry from several South...