In-Situ and Remotely-Sensed Glacier Monitoring in the Rwenzori Mountains, Uganda/D.R. Congo

The tropics, often coined as the heat engine of the planet, are paramount for global climatology because they are the main driver of air and moisture circulation around the Earth. Despite the remarkable global homogeneity of the tropical atmosphere, both in time and in space, some regions in the tropics are characterized by high interannual variations in precipitation numbers, contributing to unstable response in high mountain regions with regard to glacier mass balance. East Africa, characterized in addition by a highly variable surface topography and spatially distinct climatic regimes, represents one of these sensitive regions. Despite the growing number in recent years of studies aiming at disentangling the complex interactions between the energetic conditions, the moisture circulation and the biogeosystems in the tropics, the response of tropical African climate, and more specifically of tropical African glaciers, to current global change remains poorly understood. In this context, the Rwenzori mountains, with their steep topography peaking above 5000m elevation, their glaciers straddling along the equator, and their location at the divide between Atlantic and Indian Ocean flow, represent a key region for gaining insight not only into tropical glacier sensitivity to past, present and future climatic variations, but also into the respective roles of temperature and moisture in modulating ice mass and energy budgets. In the Rwenzori mountains, direct measurements of glacier extent and mass balance are sparse due to the inaccessibility of glaciers and the logistical constrains associated with maintaining and downloading continuous records. In addition, quasi-permanent cloud cover associated with small glacier size severely hinder glacier monitoring from space. In this research, we rely on multi-year field mapping and multi-decadal, multi-sensor satellite and aerial imagery to discuss the recession trend of Rwenzori glaciers, with a view to provide an updated estimate of modern and recent-past ice budgets. Given the small to very small extent of tropical glaciers in general, a precise contour delimitation is of prime importance in order to be able to relate glacier extent data to other environmental proxies. Atmospheric correction and ice/snow detection algorithms are also discussed in this regard.