EPICA Dronning Maud Land Ice Core 1cm Electric Conductivity Measurements (ECM) Schwander, J.; Flückiger, J.; Stauffer, B.; Zumbrunnen, O. Schwander, J. Flückiger, J. Stauffer, B. Zumbrunnen, O. earth science/paleoclimate/ice cores (depth,null,null,meter,null,ice cores,null,null,N,null) earth science/paleoclimate/ice cores (electrical conductivity,bulk ice,null,nanosiemens,null,ice cores,null,null,N,null) earth science/paleoclimate/ice core (EPICA Dronning Maud Land>LATITUDE -75>LONGITUDE .07) We present a technique that modifies and extends down-hole target methods to provide absolute measures of uncertainty in radar-reflector depth of origin. We use ice-core profiles to model wave propagation and reflection, and then cross-correlate the model results with radio-echo sounding (RES) data to identify the depth of reflector events. Stacked traces recorded with RES near the EPICA drill site in Dronning Maud Land, Antarctica, provide reference radargrams, and dielectric properties along the deep ice core form the input data to a forward model of wave propagation that produces synthetic radargrams. Cross-correlations between synthetic and RES radargrams identify differences in propagation wave speed. They are attributed to uncertainties in pure-ice permittivity and are used for calibration. Removing conductivity peaks results in the disappearance of related synthetic reflections and enables the unambiguous relation of electric signatures to RES features. We find that (i) density measurements with gamma-attenuation or dielectric profiling are too noisy below the firn-ice transition to allow clear identification of reflections, (ii) single conductivity peaks less than 0.5 m wide cause the majority of prominent reflections beyond a travel time of about 10 mu s (~900 m depth) and (iii) some closely spaced conductivity peaks within a range of 1-2 m cannot be resolved within the RES or synthetic data. Our results provide a depth accuracy to allow synchronization of age-depth profiles of ice cores by RES, modeling of isochronous internal structures, and determination of wave speed and of pure-ice properties. The technique successfully operates with dielectric profiling and electrical conductivity measurements, suggesting that it can be applied at other ice cores and drill sites. STUDY NOTES: Electrical conductivity measurements (ECM) at 1cm. resolution. NCDC-Paleoclimatology https://www.ncdc.noaa.gov/data-access/paleoclimatology-data - Bauer Bruce Investigator : Schwander, J. Investigator : Flückiger, J. Investigator : Stauffer, B. Investigator : Zumbrunnen, O. 2015-05-01 ONLINE Files online, ASCII https://www.ncdc.noaa.gov/paleo/study/18536 https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/maud/edml2015ecm1cm.txt https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/maud/edml2015ecm1cm.txt English https://www.ncdc.noaa.gov/paleo/study/18536 https://www1.ncdc.noaa.gov/pub/data/paleo/icecore/antarctica/maud/edml2015ecm1cm.txt Eisen, Olaf; Wilhelms, Frank; Steinhage, Daniel; Schwander, Jakob2006Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivityJournal of Glaciology52177299-31010.3189/172756506781828674 START YEAR: 140000 cal yr BP * END YEAR: 1260 cal yr BP .07 -75 .07 -75