Articles | Volume 15, issue 8
https://doi.org/10.5194/tc-15-3577-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-3577-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Thermal legacy of a large paleolake in Taylor Valley, East Antarctica, as evidenced by an airborne electromagnetic survey
Krista F. Myers
CORRESPONDING AUTHOR
Department of Geology and Geophysics, Louisiana State University,
Baton Rouge, LA 70803, USA
Peter T. Doran
Department of Geology and Geophysics, Louisiana State University,
Baton Rouge, LA 70803, USA
Slawek M. Tulaczyk
Department of Earth and Planetary Sciences, University of California
Santa Cruz, Santa Cruz, CA 95064, USA
Neil T. Foley
Department of Earth and Planetary Sciences, University of California
Santa Cruz, Santa Cruz, CA 95064, USA
Thue S. Bording
Department of Geoscience, Aarhus University, Aarhus, Denmark
Esben Auken
Department of Geoscience, Aarhus University, Aarhus, Denmark
Hilary A. Dugan
Center for Limnology, University of Wisconsin-Madison, Madison, WI
53706, USA
Jill A. Mikucki
Department of Microbiology, University of Tennessee, Knoxville,
Knoxville, TN 37996, USA
Nikolaj Foged
Department of Geoscience, Aarhus University, Aarhus, Denmark
Denys Grombacher
Department of Geoscience, Aarhus University, Aarhus, Denmark
Ross A. Virginia
Department of Environmental Studies, Dartmouth College, Hanover, NH
03755, USA
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The transient electromagnetic method (TEM) is widely used for mapping subsurface resistivity structures, but data are inevitably contaminated by noise from various sources including radio signals in the very low frequency (VLF) 3–30 kHz band. We present an approach where VLF noise is effectively suppressed with a new post-processing scheme where boxcar gates are combined into semi-tapered gates. The result is a 20 % increase in the depth of investigation for the presented test survey.
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Using a modeling framework applied to 37 years of dissolved oxygen time series data from Lake Mendota, we identified the timing and intensity of thermal energy stored in the lake water column, the lake's resilience to mixing, and surface primary production as the most important drivers of interannual dynamics of low oxygen concentrations at the lake bottom. Due to climate change, we expect an increase in the spatial and temporal extent of low oxygen concentrations in Lake Mendota.
Slawek M. Tulaczyk and Neil T. Foley
The Cryosphere, 14, 4495–4506, https://doi.org/10.5194/tc-14-4495-2020, https://doi.org/10.5194/tc-14-4495-2020, 2020
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Much of what we know about materials hidden beneath glaciers and ice sheets on Earth has been interpreted using radar reflection from the ice base. A common assumption is that electrical conductivity of the sub-ice materials does not influence the reflection strength and that the latter is controlled only by permittivity, which depends on the fraction of water in these materials. Here we argue that sub-ice electrical conductivity should be generally considered when interpreting radar records.
Madeline E. Myers, Peter T. Doran, and Krista F. Myers
The Cryosphere Discuss., https://doi.org/10.5194/tc-2020-203, https://doi.org/10.5194/tc-2020-203, 2020
Revised manuscript not accepted
Short summary
Short summary
In polar regions like the Dry Valleys of Antarctica, snowfall is expected to increase. Small amounts of snow lower radiation for melting and photosynthesis by increasing the albedo of the surrounding dark soil. Two decades of snowfall data have shown that the volume of snowfall has been declining since 2009, which contradicts the anticipated increase; however, the number of days with snow has been increasing, which will slow glacial melt and lower productivity below the snow cover.
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Short summary
Lake Fryxell, Antarctica, has undergone hundreds of meters of change in recent geologic history. However, there is disagreement on when lake levels were higher and by how much. This study uses resistivity data to map the subsurface conditions (frozen versus unfrozen ground) to map ancient shorelines. Our models indicate that Lake Fryxell was up to 60 m higher just 1500 to 4000 years ago. This amount of lake level change shows how sensitive these systems are to small changes in temperature.
Lake Fryxell, Antarctica, has undergone hundreds of meters of change in recent geologic history....