Gwybodaeth Modiwlau

Module Identifier
GG31830
Module Title
PHYSICAL GEOGRAPHY OF SVALBARD (UNIS)
Academic Year
2009/2010
Co-ordinator
Semester
Intended for use in future years
Co-Requisite
EA31930
Co-Requisite
GG32230
Co-Requisite
EA31030
Pre-Requisite
GG23910

Course Delivery

Delivery Type Delivery length / details
Lecture 45 Hours.
Seminars / Tutorials 35 Hours.
Other Field Work. 3 days
 

Assessment

Assessment Type Assessment length / details Proportion
Semester Assessment 5 Hours   Written exercises  In-Course Assessment: 
Semester Assessment Field excursion report and term project report  Continuous Assessment: 
Supplementary Exam Two-hour examination and 5,000 world report 

Learning Outcomes

On completion of this module, students should be able to demonstrate knowledge of the following aspects of the physical geography of Svalbard:

  • The climatic conditions on Svalbard, the energy exchange at the ground surface, the ground thermal regime and the availability of water, in relation to geomorphological and glaciological processes.
  • Glacier mass balance, thermal structure and geomorphological activity of Svalbard glaciers.
  • The role of permafrost and frost weathering in the High Arctic environment.
  • Hydrological processes (snow melt, river flow and sediment transport) in the High Arctic environment.

Aims

This module is one of four suitable for students registered for BSc honours degrees in Environmental Earth Science and Geography, offered by UNIS in Svalbard. UNIS is a University on the High-Arctic archipelago of Svalbard, currently under Norwegion sovereignty. UNIS was established in 1993 by the four universities in Oslo, Bergen, Trondheim and Tromso to offer university level courses and to perform research relevant to its High Arctic location. The intention is to provide level 3 students with the opportunity to undertake one semester of study overseas at UNIS within an international community of students and staff, in an exciting and challenging environment.

The High-Arctic archipelago of Svalbard is currently 60% glacier-covered and serves as a modern analogue for conditions in Britain during the Quaternary. This module outlines the most important meteorological, glaciological, geomorphological and hydrological processes on Svalbard. The primary focus will be on the inter-relationship between climate and earth-surface processes in the Arctic.

Content

The High-Arctic archipelago of Svalbard is currently 60% glacier-covered and serves as a modern analogue for conditions in Britain during the Quaternary. The module outlines the most important meteorological, glaciological, geomorphological and hydrological processes on Svalbard. The primary focus will be on the inter-relationship between climate and earth-surface processes in the Arctic.


Notes

This module is at CQFW Level 6