Articles | Volume 14, issue 1
Research article
31 Jan 2020
Research article |  | 31 Jan 2020

Relating regional and point measurements of accumulation in southwest Greenland

Achim Heilig, Olaf Eisen, Martin Schneebeli, Michael MacFerrin, C. Max Stevens, Baptiste Vandecrux, and Konrad Steffen

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Cited articles

Bennartz, R., Fell, F., Pettersen, C., Shupe, M. D., and Schuettemeyer, D.: Spatial and temporal variability of snowfall over Greenland from CloudSat observations, Atmos. Chem. Phys., 19, 8101–8121,, 2019. a
Charalampidis, C., van As, D., Colgan, W. T., Fausto, R. S., MacFerrin, M., and Machguth, H.: Thermal tracing of retained meltwater in the lower accumulation area of the Southwestern Greenland ice sheet, Ann. Glaciol., 57, 1–10,, 2016. a
Dunse, T., Eisen, O., Helm, V., Rack, W., Steinhage, D., and Parry, V.: Characteristics and small-scale variability of GPR signals and their relation to snow accumulation in Greenland's percolation zone, J. Glaciol., 54, 333–342,, 2008. a, b, c
Enderlin, E. M., Howat, I. M., Jeong, S., Noh, M.-J., van Angelen, J. H., and van den Broeke, M. R.: An improved mass budget for the Greenland ice sheet, Geophys. Res. Lett., 41, 866–872,, 2014. a
Fahrmeir, L., Künstler, R., Pigeot, I., and Tutz, G.: Statistik: Der Weg zur Datenanalyse, Springer-Lehrbuch, Springer, Berlin and Heidelberg, 7. Auflage, korrigierter Nachdruck, 2011. a
Short summary
We investigate the spatial representativeness of point observations of snow accumulation in SW Greenland. Such analyses have rarely been conducted but are necessary to link regional-scale observations from, e.g., remote-sensing data to firn cores and snow pits. The presented data reveal a low regional variability in density but snow depth can vary significantly. It is necessary to combine pits with spatial snow depth data to increase the regional representativeness of accumulation observations.