Towards understanding the signal formation in polar snow, firn and ice using X-ray computed tomography

• Main Author: Schaller, Christoph
• Format: Thesis
• Language: unknown
• Published: 2018
• Subjects: Antarc*; Antarctica; East Antarctica; Greenland; ice core; North Greenland
• Online Access: https://epic.awi.de/id/eprint/47495/; https://epic.awi.de/id/eprint/47495/1/CSchaller_Diss_Feb2018_PDFA_final.pdf; https://suche.suub.uni-bremen.de/peid=B101792549&CID=6004023; https://hdl.handle.net/10013/epic.ad20190c-e37e-41db-aaaf-4894879643c3

Polar ice cores act as a unique archive of the Earth’s climate system. However, due to logistic constraints, the representativity of these ice-core records cannot be estimated directly. One possible remedy is to analyze the spatial variability in polar snow and firn and combine the results with an improved understanding of the formation of paleoclimatic ice-core signals and their evolution with depth. Here, X-ray computed tomography is applied as a non-destructive method that yields information on stratigraphy and microstructure in polar snow and firn. The results are used to contribute to both subtopics of this indirect approach for estimating representativity. New methods for sampling the snowpack as well as the detection and ali- gnment of coherent signals in spatially-distributed datasets are presented. They are applied to analyze spatial variability in the snowpack both on the local (trench studies in Greenland and East Antarctica, distances up to 100 m) and the regio- nal scale (450 km traverse through North Greenland). The matching algorithm is validated using randomly generated profiles with the same statistical properties as the original data. Snow and firn density as markers of stratigraphy are deter- mined by two-dimensional radioscopic imaging, the water-isotopic δ18O signal is used for age dating. The results show that regionally a significant share of the stratigraphic density signal persists over hundreds of kilometers. Locally, there is a strong directional influence of the wind with a much larger homogeneity of the snowpack along the main wind direction. As density is an important input parameter for remote sen- sing and surface-mass-balance estimates, representative profiles or mean values of snow and firn density are required. Such a profile is provided for the upper two meters of the North Greenland snowpack. On the local scale, the estimation of representative densities for certain areas of interest (such as the footprint of an altimeter) is complicated by the directional dependence of the ...