Table 1: Discharge, mass flux, maximum velocity and ice thickness of glaciers from Dronning Maud Land, Antarctica

Mass transport and mass flux values for the different types of glaciers in the Sør-Rondane are calculated from computer models, based upon gravity data and geodetic stake velocity measurements. The results are interpreted in the light of a general flow line analysis, glacial geological investigations and of the ablation terms of the mass balance for Dronning Maud Land and Antarctica.

Supplement to: Van Autenboer, T; Decleir, H (1978): Glacier discharge in the Sor-Rondane, a contribution to the mass balance of Dronning Maud Land, Antarctica. Zeitschrift für Gletscherkunde und Glazialgeologie, 14(1), 1-16

Identifier
DOI https://doi.org/10.1594/PANGAEA.803298
PID https://hdl.handle.net/10013/epic.40239.d001
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.803298
Provenance
Creator Van Autenboer, T; Decleir, H
Publisher PANGAEA
Publication Year 1978
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 50 data points
Discipline Earth System Research
Spatial Coverage (25.000 LON, -72.000 LAT); Sør Rondane Mountains, Queen MAud Land, Antarctica