Abstract
Abstract Over recent decades, the retreat of Kilimanjaro’s glaciers has been portrayed as a beacon of climate change. The decline of glaciers over the 20 th century, however, is evident for all tropical glaciers in East Africa, including those found on Mount Kenya and in the Rwenzori Range. More recent studies have focused on Kilimanjaro and Mount Kenya but the Rwenzori Range has not been considered for nearly two decades, which introduces an uncertainty about the remaining glacierization in East Africa. Therefore, the present study provides insights into the most recent glacier extents of all three mountain regions using a manual, multitemporal analysis of high-resolution satellite images for the years 2021/2022. The glacierization in East Africa is estimated to be 1.36 km 2 , with a glacier area of 0.98 km 2 on Kilimanjaro, 0.069 km 2 on Mount Kenya and 0.38 km 2 in the Rwenzori Range. The uncertainty is determined to be within 12.5%. Compared to previous estimations, the overall area has declined by more than a half of its early 21 st century extent. Being mainly controlled by high-altitude hygric seasonality, these glaciers are particularly valuable indicators of tropical climate variability and climate change.