About
Dr Suzanne Bevan is a member of the Geography Department at Swansea University
Dr Suzanne Bevan is a member of the Geography Department at Swansea University
Currently I am on a research post but I have co-ordinated or taught on a variety of courses in the past including Data Visualization, Approaches to Physical Geography, Meteorology, Glaciology, Dangerous Earth, Climate of the last Millenium, and the Vancouver Field Course.
My research interests lie in using observations acquired by satellite-borne instruments to detect and monitor global environmental change. I work primarily on cryospheric change — on the glaciers of Greenland and the ice shelves of Antarctica. In these regions I make use of optical and microwave data to measure surface flow, surface elevation, and surface melt. The techniques I use include feature tracking and radar interferometry.
My current research, as a postdoc on the NERC funded CALISMO (Calving Laws for Ice Sheet Models) project, focusses on analysing satellite observations of Greenland outlet glaciers and Antarctic ice shelves to inform and validate numerical models of calving processes.
This residential field course module explores the relationship between environment and society in the Himalayan state of Sikkim in NE India on the borders with China, Nepal, Tibet and West Bengal. The course is inter-disciplinary in approach and policy-oriented. Students work with members of University Staff in mixed groups of biologists, human geographers, physical geographers and zoologists. Through intensive inter-disciplinary group working students utilise (and pass on) their specialist skills in the group exercises and projects that are undertaken.
2007 - Present
2007 - 2007
2007 - 2007
2003 - 2007
1996 - 2003
1989 - 1992
1987 - 1989
1984 - 1987
1983 - 1984
A research group dedicated to furthering knowledge in the quantification of the past and future contribution from glaciers and ice sheets to sea-level rise; the processes driving the present rapid and dramatic changes observed in glaciers, and the instabilities inherent in glacial systems; and the record of palaeo-ice mass instabilities and the processes that drove these changes.