Variations of southeast vatnajökull ice cap (iceland) 1650–1900 and reconstruction of the glacier surface geometry at the little ice age maximum

Abstract

We present an overview of glacier variations of the outlet glaciers of southeast atnajökull ice cap, celand, during the time period ∼1650–1900 as represented in historical archives, by geomorphological field evidence and assess the timing of the Little Ice Age (LIA) maximum. According to written documents, all glaciers advanced in the latter half of the seventeenth century and extended far out on the lowlands in the mid‐eighteenth century. Contemporary documents describe how all the studied glaciers were at their terminal moraines around ∼1880–1890 (no descriptions found for orsárjökull) and soon after started receding, marking the end of the in celand. Reconstruction of the maximum glacier surface geometry was based on glacial geomorphological features (including lateral and terminal moraines, trimlines and erratics), historical photographs, maps from 1904, and a 2010 digital elevation model. The glaciers were at their maximum around 150–270 m thicker near the terminus than in 2010, whereas negligible differences were observed in the upper reaches of the accumulation area. By combining the historical, glacial geomorphological and high‐resolution data, we provide quantitative estimates of the glacial extent and volume at the maximum. The highest up‐valley lateral moraines provided estimates of the equilibrium line altitude (ELA) during the , which was on average 340 m lower than the present day ELA. Consistency was found in the spatial variability of the ELA during both time periods, with higher values on the westfacing outlets of ræfajökull ice cap (at the southern end of atnajökull ice cap), than on the east flowing glaciers, and a rise in the ELA from west to east on the outlets east of reiðamerkurjökull.