Periodic Surface Features in Coastal East Antarctica


Contact
hanschuetz [ at ] awi-bremerhaven.de

Abstract

We found evidence for highly periodic dunes in a near-coastal area of Dronning Maud Land, East Antarctica.Analysis of accumulation patterns, derived from ground-penetrating radar (GPR) internal layering, and GPS-based characteristics of surface topography, by means of auto- and cross-covariance, indicate quasi-harmonic oscillations of surface undulations, surface slope, and accumulation.The dunes occur at an elevation range of 1000-1350 m with the dominant wavelength of 5 km and undulations of about 10 m.Accumulation and slope are anticorrelated at zero lag, with a mean annual accumulation of some 140 kgm-2a-1 and variations on the order ofsome 100 kgm-2a-1.Our findings have implications for studies aiming at the mass balance of coastal areas in Antarctica.



Item Type
Article
Authors
Divisions
Programs
Peer revision
ISI/Scopus peer-reviewed
Publication Status
Published
Eprint ID
15276
DOI 10.1029/2006GL027871

Cite as
Anschütz, H. , Eisen, O. , Rack, W. and Scheinert, M. (2006): Periodic Surface Features in Coastal East Antarctica , Geophysical research letters, 33, L22501 . doi: 10.1029/2006GL027871


Share


Citation

Research Platforms
N/A

Campaigns


Actions
Edit Item Edit Item