Zobrazeno 1 - 10
of 96
pro vyhledávání: '"Kerry Key"'
Autor:
KERRY KEY, MATTHEW R. SIEGFRIED
Publikováno v:
Journal of Glaciology, Vol 63, Pp 755-771 (2017)
Subglacial hydrologic systems in Antarctica and Greenland play a fundamental role in ice-sheet dynamics, yet critical aspects of these systems remain poorly understood due to a lack of observations. Ground-based electromagnetic (EM) geophysical metho
Externí odkaz:
https://doaj.org/article/e17458a25e3d426ab2fe794316d0d004
Autor:
Gary D. Egbert, Bo Yang, Paul A. Bedrosian, Kerry Key, Dean W. Livelybrooks, Adam Schultz, Anna Kelbert, Blake Parris
Publikováno v:
Nature Geoscience. 15:677-682
Publikováno v:
Geophysical Journal International. 231:1075-1095
SUMMARY This paper is Part II of a two-part series on a mathematical and computational framework for computing a meaningful uncertainty quantification (UQ) for regularized inversions of electromagnetic data. In Part I, we explained the theory behind
Publikováno v:
Geophysical Journal International. 231:1057-1074
SUMMARY We present a method for computing a meaningful uncertainty quantification (UQ) for regularized inversion of electromagnetic (EM) geophysical data that combines the machineries of regularized inversion and Bayesian sampling with a ‘randomize
Publikováno v:
Nature. 604:491-494
Publikováno v:
Geophysical Prospecting. 70:210-221
Autor:
David Alumbaugh, Michael Wilt, Edward Nichols, Evan Um, Marie Macquet, Donald C. Lawton, Dennis Rippe, Kerry Key, David Myer
Publikováno v:
Second International Meeting for Applied Geoscience & Energy.
Autor:
Chloe D. Gustafson, Kerry Key, Matthew R. Siegfried, J. Paul Winberry, Helen A. Fricker, Ryan A. Venturelli, Alexander B. Michaud
Publikováno v:
Science (New York, N.Y.). 376(6593)
Antarctica’s fast-flowing ice streams drain the ice sheet, with their velocity modulated by subglacial water systems. Current knowledge of these water systems is limited to the shallow portions near the ice-bed interface, but hypothesized deeper gr
Publikováno v:
Geochemistry, Geophysics, Geosystems. 20:5979-5999
Autor:
Kerry Key, Bo Yang, Paul A. Bedrosian, Blake Parris, Anna Kelbert, D. Livelybrooks, Adam Schultz, Gary D. Egbert
Subduction of hydrated oceanic lithosphere can carry water deep into the Earth, with important consequences for a range of tectonic and magmatic processes. Most fluid is released at relatively shallow depths in the forearc where it is thought to play
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::07d4f39684dd9bb5e44351fe14a6b854
https://doi.org/10.21203/rs.3.rs-475649/v1
https://doi.org/10.21203/rs.3.rs-475649/v1