Results 51 to 60 of about 1,246,077 (130)
r-nakashima-geophysics/MHD-2D-sphere: v1.0.0
<p><strong>Full Changelog</strong>: <a href="https://github.com/r-nakashima-geophysics/MHD-2D-sphere/commits/v1.0.0">https://github.com/r-nakashima-geophysics/MHD-2D-sphere/commits/v1.0.0</a></p ...
r-nakashima-geophysics
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Abstract In this study, we present a mix of full‐depth profiles and near‐bottom observations of dissolved 230Th and 232Th from the Adélie Land margin in East Antarctica, a key site of Antarctic Bottom Water (AABW) formation. We show that the distribution of dissolved Th isotopes in this region is governed by a combination of reversible scavenging ...
Thomas J. Williams +8 more
wiley +1 more source
Geophysics, Colorado School of Mines, Spring 2014
Newsletter of the Geophysics Department at Colorado School of ...
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Abstract Subglacial sedimentary basins in Antarctica are hypothesized to modulate ice flow and biogeochemical cycles via groundwater and geothermal feedbacks, yet their properties remain poorly constrained. Here, we present a joint quantitative analysis of new magnetotelluric (MT) data acquired at Thwaites Glacier (TG) and WAIS Divide, alongside legacy
Siobhan F. Killingbeck +8 more
wiley +1 more source
The "tipping" temperature within Subglacial Lake Ellsworth, West Antarctica and its implications for lake access. [PDF]
We present results from new geophysical data allowing modelling of the water flow within Subglacial Lake Ellsworth (SLE), West Antarctica. Our simulations indicate that this lake has a novel temperature distribution due to significantly thinner ice than ...
Woodward, J. +19 more
core +2 more sources
Recent aeromagnetic and deep electromagnetic exploration projects in East Antarctica
Airborne geophysical surveys play a pivotal role in imaging subglacial geology and characterizing broad areas of the Antarctic liothsphere. Ground-based geophysics, coupled with airborne geophysics and geology, is essential to further elucidate crustal ...
Bozzo, E. +4 more
core +3 more sources
Internal Structure and Formation Process of a Giant East Antarctic Grounding‐Zone Wedge
Abstract The marine‐based portions of the East Antarctic Ice Sheet are currently losing mass at an accelerating rate due to atmospheric and oceanic forcing. Assessing these changes requires understanding long‐term grounding‐zone dynamics preserved in glacial geomorphology, including understudied East Antarctic shelf sectors.
C. A. Tobisch +7 more
wiley +1 more source
Subglacial drainage processes at a High Arctic polythermal valley glacier [PDF]
Dye-tracer experiments undertaken over two summer melt seasons at polythermal John Evans Glacier, Ellesmere Island, Canada, were designed to investigate the character of the subglacial drainage system and its evolution over a melt season. In both summers,
Nienow, Peter W. +5 more
core +1 more source
Abstract The Siple Coast region of West Antarctica is known for its fast flowing, topographically unconstrained ice streams that evolve due to subglacial conditions. In this work, we analyze the nature of the Siple Coast subglacial hydrologic system and its interactions with the ice sheet using two‐way coupled subglacial hydrology and ice flow modeling.
Koi McArthur +2 more
wiley +1 more source
Geophysics: revealing the dynamics of Earth, Fall 2018
Newsletter of the Geophysics Department at Colorado School of ...
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