TY - JOUR
T1 - Little Ice Age advance of Kvískerjajöklar, Öræfajökull, Iceland. A contribution to the assessment of glacier variations in Iceland since the late 18th century
AU - Guðmundsson, Snævarr
AU - Björnsson, Helgi
N1 - Funding Information: The study was partly financed by the Kvísker Fund and Friends of Vatnajökull Asso-ciation (www.friendsofvatnajokull.is). Funding Information: We gratefully acknowledge many fruitful discussions with the Kvísker brothers, Flosi, Sigurður, Helgi and Hálfdán Björnsson. We gratefully thank Tómas Jóhannesson for advice on the study and David Evans for useful comments. The study was partly financed by the Kvísker Fund and Friends of Vatnajökull Association (www.friendsofvatnajokull.is). Publisher Copyright: © 2020, Iceland Glaciological Society. All rights reserved.
PY - 2020
Y1 - 2020
N2 - — We describe the changes of the Kvískerjajöklar outlet glaciers in SE Iceland (presently ranging 600–1600 m a.s.l.), from their Little Ice Age maximum (LIAmax ) to the present. We assume that glacier extent of the late 19th century approximately describes LIAmax although the glaciers already reached their peak extent in the 18th century. The former glacier margins were delineated from moraines, historical descriptions, topographical maps, aerial and oblique photographs, Landsat images and a lidar DEM. Along the previous glacier margins, elevation differences with respect to the lidar DEM of 2011 were estimated and contour maps of the glacier drawn at selected dates, maintaining the shape of the glacier surface as available maps. During the period ∼1890 to 2011, the outlets lost-0.4 m a−1 water equivalent evenly distributed over their surface and their area was reduced by 37% (from ∼10 km2 to 6.4 km2, 0.03 km2 a−1, 0.43 km3 water equivalent in total, i.e. 0.003 km3 w.e. a−1 ).
AB - — We describe the changes of the Kvískerjajöklar outlet glaciers in SE Iceland (presently ranging 600–1600 m a.s.l.), from their Little Ice Age maximum (LIAmax ) to the present. We assume that glacier extent of the late 19th century approximately describes LIAmax although the glaciers already reached their peak extent in the 18th century. The former glacier margins were delineated from moraines, historical descriptions, topographical maps, aerial and oblique photographs, Landsat images and a lidar DEM. Along the previous glacier margins, elevation differences with respect to the lidar DEM of 2011 were estimated and contour maps of the glacier drawn at selected dates, maintaining the shape of the glacier surface as available maps. During the period ∼1890 to 2011, the outlets lost-0.4 m a−1 water equivalent evenly distributed over their surface and their area was reduced by 37% (from ∼10 km2 to 6.4 km2, 0.03 km2 a−1, 0.43 km3 water equivalent in total, i.e. 0.003 km3 w.e. a−1 ).
UR - https://www.scopus.com/pages/publications/85134183437
U2 - 10.33799/jokull2020.70.073
DO - 10.33799/jokull2020.70.073
M3 - Review article
SN - 0449-0576
VL - 2020
SP - 73
EP - 86
JO - Jokull
JF - Jokull
IS - 70
ER -