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      Distributed Acoustic Sensing of Seismic Properties in a Borehole Drilled on a Fast‐Flowing Greenlandic Outlet Glacier

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          Mass balance of the Greenland ice sheet from 1958 to 2007

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            Distributed Acoustic Sensing Using Dark Fiber for Near-Surface Characterization and Broadband Seismic Event Detection

            We present one of the first case studies demonstrating the use of distributed acoustic sensing deployed on regional unlit fiber-optic telecommunication infrastructure (dark fiber) for broadband seismic monitoring of both near-surface soil properties and earthquake seismology. We recorded 7 months of passive seismic data on a 27 km section of dark fiber stretching from West Sacramento, CA to Woodland, CA, densely sampled at 2 m spacing. This dataset was processed to extract surface wave velocity information using ambient noise interferometry techniques; the resulting V S profiles were used to map both shallow structural profiles and groundwater depth, thus demonstrating that basin-scale variations in hydrological state could be resolved using this technique. The same array was utilized for detection of regional and teleseismic earthquakes and evaluated for long period response using records from the M8.1 Chiapas, Mexico 2017, Sep 8th event. The combination of these two sets of observations conclusively demonstrates that regionally extensive fiber-optic networks can effectively be utilized for a host of geoscience observation tasks at a combination of scale and resolution previously inaccessible.
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              An Introduction to Distributed Optical Fibre Sensors

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                Author and article information

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                Journal
                Geophysical Research Letters
                Geophys. Res. Lett.
                American Geophysical Union (AGU)
                0094-8276
                1944-8007
                July 16 2020
                July 07 2020
                July 16 2020
                : 47
                : 13
                Affiliations
                [1 ]Institute of Applied Geoscience, School of Earth and Environment University of Leeds Leeds UK
                [2 ]Scott Polar Research Institute, Department of Geography University of Cambridge Cambridge UK
                [3 ]Silixa Ltd Elstree Hertfordshire UK
                [4 ]Centre for Glaciology, Department of Geography and Earth Sciences Aberystwyth University Aberystwyth Ceredigion UK
                Article
                10.1029/2020GL088148
                16e99d8a-604f-45d2-a858-e613c7146324
                © 2020

                http://creativecommons.org/licenses/by/4.0/

                http://doi.wiley.com/10.1002/tdm_license_1.1

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