IMIS | Lifewatch regional portal

You are here

IMIS

[ report an error in this record ]basket (1): add | show Print this page

one publication added to basket [219491]
Radar characterization of the basal interface across the grounding zone of an ice-rise promontory in East Antarctica
Matsuoka, K.; Pattyn, F.; Callens, D.; Conway, H. (2012). Radar characterization of the basal interface across the grounding zone of an ice-rise promontory in East Antarctica. Ann. Glaciol. 53(60): 29-34. https://dx.doi.org/10.3189/2012AoG60A106
In: Annals of Glaciology. International Glaciological Society: Cambridge. ISSN 0260-3055; e-ISSN 1727-5644, more
Peer reviewed article  

Available in  Authors 

Keyword
    Marine/Coastal

Authors  Top 
  • Matsuoka, K.
  • Pattyn, F., more
  • Callens, D., more
  • Conway, H.

Abstract
    Radar power returned from the basal interface along a 42 km long profile over an ice-rise promontory and the adjacent Roi Baudouin ice shelf, Dronning Maud Land, East Antarctica, is analyzed to infer spatial variations in basal reflectivity and hence the basal environment. Extracting basal reflectivity from basal returned power requires an englacial attenuation model.We estimate attenuation in two ways: (1) using a temperature-dependent model with input from thermomechanical ice-flow models; and (2) using a radar method that linearly approximates the geometrically corrected returned power with ice thickness. The two methods give different results. We argue that attenuation calculated using a modeled temperature profile is more robust than the widely used radar method, especially in locations where depth-averaged attenuation varies spatially or where the patterns of basal reflectivity correlate with the patterns of the ice thickness.

All data in the Integrated Marine Information System (IMIS) is subject to the VLIZ privacy policy Top | Authors