Accumulation Rates during 1311–2011 CE in North-Central Greenland Derived from Air-Borne Radar Data

Frontiers in Digital Humanities

Paden, John D.¹  Lewis, Cameron¹  Eisen, Olaf¹  Wilhelms, Frank²  Kipfstuhl, Sepp³  Karlsson, Nanna B.³  Freitag, Johannes⁴  Nielsen, Lisbeth T.⁶  Winter, Anna⁶  Dahl-Jensen, Dorthe⁶ 

[1] Alfred-Wegener-Institut Helmholtz-Zentrum füCenter for Remote Sensing of Ice Sheets, University of Kansas, Lawrence, KS, USA;Centre for Ice and Climate, The Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark;Department of Geosciences, University of Bremen, Bremen, Germany;Sandia National Laboratories, Albuquerque, NM, USA;r Polar- und Meeresforschung, Bremerhaven, Germany

关键词: Surface mass balance;    Greenland ice sheet;    Ice-penetrating radar;    Internal glacier stratigraphy;    inverse methods;   

DOI  :  10.3389/feart.2016.00097

学科分类：社会科学、人文和艺术（综合）

来源: Frontiers

【 摘 要 】

Radar–detected internal layering contains information on past accumulation rates and patterns. In this study, we assume that the radar layers are isochrones, and use the layer stratigraphy in combination with ice-core measurements and numerical methods to retrieve accumulation information for the northern part of central Greenland. Measurements of the dielectric properties of an ice core from the NEEM (North Greenland Eemian Ice Drilling) site, allow for correlation of the radar layers with volcanic horizons to obtain an accurate age of the layers. We obtain accumulation patterns averaged over 100 a for the period 1311–2011. Our results show a clear trend of high accumulation rates west of the ice divide and low accumulation rates east of the ice divide. At the NEEM site the accumulation pattern is persistent during our study period and only small temporal variations occur in the accumulation rate. However, from approximately 200 km south of the NEEM drill site, the accumulation rate shows temporal variations based on our centennial averages. We attribute this variation to shifts in the location of the high–low accumulation boundary that usually is aligned with the ice divide, but appears to have moved across the divide in the past.

【 授权许可】

CC BY