Surface elevation changes near Barrow (Alaska) measured using reflected GPS signals

Fuente: PANGAEA
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Autores principales: Liu, Lin, Larson, Kristine M
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2018
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author Liu, Lin
Larson, Kristine M
author_facet Liu, Lin
Larson, Kristine M
collection Datos científicos de ciencias marinas y ambientales
contents We use reflected GPS signals to measure temporal changes of ground surface elevation due to dynamics of the active layer and near-surface permafrost. Applying the GPS interferometric reflectometry technique to the multipath signal-to-noise ratio data collected by a continuously-operating GPS receiver mounted deep in permafrost in Barrow, Alaska, we can retrieve the vertical distance between the antenna and reflecting surface. Using this unique kind of observables, we obtain daily changes of surface elevation during July and August from 2004 to 2015. Our results show distinct temporal variations at three timescales: regular thaw settlement within each summer, strong inter-annual variability that is characterized by a sub-decadal subsidence trend followed by a brief uplift trend, and a secular subsidence trend of 0.26 cm/year during 2004 and 2015.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_885935
institution PANGAEA
language en
publishDate 2018
publisher PANGAEA
record_format pangaea
spellingShingle Surface elevation changes near Barrow (Alaska) measured using reflected GPS signals
Liu, Lin
Larson, Kristine M
Barrow_SG27; Barrow, Alaska, USA; DATE/TIME; Day of the year; Elevation change; Elevation change, error; SG27
We use reflected GPS signals to measure temporal changes of ground surface elevation due to dynamics of the active layer and near-surface permafrost. Applying the GPS interferometric reflectometry technique to the multipath signal-to-noise ratio data collected by a continuously-operating GPS receiver mounted deep in permafrost in Barrow, Alaska, we can retrieve the vertical distance between the antenna and reflecting surface. Using this unique kind of observables, we obtain daily changes of surface elevation during July and August from 2004 to 2015. Our results show distinct temporal variations at three timescales: regular thaw settlement within each summer, strong inter-annual variability that is characterized by a sub-decadal subsidence trend followed by a brief uplift trend, and a secular subsidence trend of 0.26 cm/year during 2004 and 2015.
title Surface elevation changes near Barrow (Alaska) measured using reflected GPS signals
topic Barrow_SG27; Barrow, Alaska, USA; DATE/TIME; Day of the year; Elevation change; Elevation change, error; SG27
url https://doi.org/10.1594/PANGAEA.885935