TY  - JOUR
A1  - Laepple, Thomas
A1  - Hörhold, Maria
A1  - Münch, Thomas
A1  - Freitag, Johannes
A1  - Wegner, Anna
A1  - Kipfstuhl, Sepp
T1  - Layering of surface snow and firn at Kohnen Station, Antarctica: Noise or seasonal signal?
JF  - Journal of geophysical research : Earth surface
N2  - The density of firn is an important property for monitoring and modeling the ice sheets as well as to model the pore close-off and thus to interpret ice core-based greenhouse gas records. One feature, which is still in debate, is the potential existence of an annual cycle of firn density in low-accumulation regions. Several studies describe or assume seasonally successive density layers, horizontally evenly distributed, as seen in radar data. On the other hand, high-resolution density measurements on firn cores in Antarctica and Greenland show no clear seasonal cycle in the top few meters. A major caveat of most existing snow-pit and firn-core-based studies is that they represent one vertical profile from a laterally heterogeneous density field. To overcome this, we created an extensive data set of horizontal and vertical density data at Kohnen Station, Dronning Maud Land, on the East Antarctic Plateau. We drilled and analyzed three 90m long firn cores as well as 143 one-meter-long vertical profiles from two elongated snow trenches to obtain a two-dimensional view of the density variations. The analysis of the 45m wide and 1m deep density fields reveals a seasonal cycle in density. However, the seasonality is overprinted by strong stratigraphic noise, making it invisible when analyzing single firn cores. Our density data set extends the view from the local ice core perspective to a hundred meter scale and thus supports linking spatially integrating methods such as radar and seismic studies to ice and firn cores.
Y1  - 2016
U6  - https://doi.org/10.1002/2016JF003919
SN  - 2169-9003
SN  - 2169-9011
VL  - 121
SP  - 1849
EP  - 1860
PB  - American Geophysical Union
CY  - Washington
ER  -