Table 1: Discharge, mass flux, maximum velocity and ice thickness of glaciers from Dronning Maud Land, Antarctica
| Cobertura |
LATITUDE: -72.000000 * LONGITUDE: 25.000000 |
|---|---|
| Data(s) |
03/12/1978
|
| Resumo |
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. |
| Formato |
text/tab-separated-values, 50 data points |
| Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.803298 doi:10.1594/PANGAEA.803298 |
| Idioma(s) |
en |
| Publicador |
PANGAEA |
| Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
| Fonte |
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, hdl:10013/epic.40239.d001 |
| Palavras-Chave | #Area/locality; Glacier discharge; Glacier mass flux; Ice thickness, glacier; SRM; Sør Rondane Mountains, Queen MAud Land, Antarctica; Velocity magnitude |
| Tipo |
Dataset |
