The acoustic damping of sound waves in natural glaciers is a largely unexplored physical property that has relevance for various applications. We present measurements of the attenuation of sound in ice with a dedicated measurement setup in situ on the Italian glacier Langenferner from August 2017. The tested frequency ranges from 2 kHz to 35 kHz and probed distances between 5 m and 90 m. The attenuation length has been determined by two different methods including detailed investigations of systematic uncertainties. The attenuation length decreases with increasing frequencies. Observed values range between 13 m for low frequencies and 5 m for high frequencies. The presented results improve in accura...
During the Arctic Submarine Lab–Hosted 2016 Ice Exercise, short-range acoustic propagation under ice...
Resonating water-filled fractures in glaciers have been observed repeatedly by their emission of ela...
A 40 km line across George VI Ice Shelf was sounded in January 1981 by both radio echo and seismic r...
The attenuation coefficient of ice in a temperate valley glacier was measured by spectral analysis o...
Using the South Pole Acoustic Test Setup (SPATS) and a retrievable transmitter deployed in holes dri...
The rapidly changing cryosphere motivates a better understanding of the physical processes governing...
The attenuation of radio waves within the ice sheet is caused by absorption loss due to dielectric a...
In the first section, the thickness of ice on the lakes and canals is estimated by analyzing the sou...
In the past century, extensive research has been done regarding the sound propagation in Arctic ice ...
Abstract: The physical processes accompanying glacier melting generate underwater sound audible in t...
The structure of ice shelves is important for modeling the dynamics of ice flux from the continents ...
A hydrophone was deployed in February 2022 underneath landfast sea ice in Tempelfjorden, Svalbard. T...
The crystal orientation fabric (COF) in ice cores provides detailed information, such as grain size ...
There is a need for measurements of the thickness of glaciers, ice sheets, and ice shelves. Radio wa...
The environments underneath ice sheets are of high scientific interest. Wireless sensors offer the p...
During the Arctic Submarine Lab–Hosted 2016 Ice Exercise, short-range acoustic propagation under ice...
Resonating water-filled fractures in glaciers have been observed repeatedly by their emission of ela...
A 40 km line across George VI Ice Shelf was sounded in January 1981 by both radio echo and seismic r...
The attenuation coefficient of ice in a temperate valley glacier was measured by spectral analysis o...
Using the South Pole Acoustic Test Setup (SPATS) and a retrievable transmitter deployed in holes dri...
The rapidly changing cryosphere motivates a better understanding of the physical processes governing...
The attenuation of radio waves within the ice sheet is caused by absorption loss due to dielectric a...
In the first section, the thickness of ice on the lakes and canals is estimated by analyzing the sou...
In the past century, extensive research has been done regarding the sound propagation in Arctic ice ...
Abstract: The physical processes accompanying glacier melting generate underwater sound audible in t...
The structure of ice shelves is important for modeling the dynamics of ice flux from the continents ...
A hydrophone was deployed in February 2022 underneath landfast sea ice in Tempelfjorden, Svalbard. T...
The crystal orientation fabric (COF) in ice cores provides detailed information, such as grain size ...
There is a need for measurements of the thickness of glaciers, ice sheets, and ice shelves. Radio wa...
The environments underneath ice sheets are of high scientific interest. Wireless sensors offer the p...
During the Arctic Submarine Lab–Hosted 2016 Ice Exercise, short-range acoustic propagation under ice...
Resonating water-filled fractures in glaciers have been observed repeatedly by their emission of ela...
A 40 km line across George VI Ice Shelf was sounded in January 1981 by both radio echo and seismic r...