Zobrazeno 1 - 10
of 83
pro vyhledávání: '"Steven E. Ingebritsen"'
Publikováno v:
Groundwater. 60:64-70
About 14.5 months after the 2018 eruption and summit collapse of Kīlauea Volcano, Hawai'i, liquid water started accumulating in the deepened summit crater, forming a lake that attained 51 m depth before rapidly boiling off on December 20, 2020, when
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4ef40ea8bb0cbc189a332c55c9de95b6
https://doi.org/10.1111/gwat.13133
https://doi.org/10.1111/gwat.13133
Publikováno v:
Groundwater. 59:7-15
During the 2018 eruption of Kīlauea Volcano, Hawai'i, scientists relied heavily on a conceptual model of explosive eruptions triggered when lava-lake levels drop below the water table. Numerical modeling of multiphase groundwater flow and heat trans
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e4cbfe59469344bf5b1bb44fed059f12
https://doi.org/10.1111/gwat.13023
https://doi.org/10.1111/gwat.13023
Autor:
Jennifer L. Lewicki, William C. Evans, Steven E. Ingebritsen, Laura E. Clor, Peter J. Kelly, Sara Peek, Robert A. Jensen, Andrew G. Hunt
Publikováno v:
Journal of Volcanology and Geothermal Research. 433:107729
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d4e0cb02e53fca29c72a7a69fe946b5
https://doi.org/10.1016/j.jvolgeores.2022.107729
https://doi.org/10.1016/j.jvolgeores.2022.107729
Autor:
Steven E. Ingebritsen, Paul A. Hsieh
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:1498-1506
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03a6e9690e847f97274f5f27f94bd559
https://doi.org/10.1029/2018jb017133
https://doi.org/10.1029/2018jb017133
Autor:
Stephen B. Gingerich, Martha A. Scholl, Edward F. Younger, Steven E. Ingebritsen, R. Lopaka Lee, Shaul Hurwitz, Sara Peek, D. Bergfeld, James P. Kauahikaua, William C. Evans, Paul A. Hsieh
Publikováno v:
Professional Paper.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a22a8cd217f6f09a4953d2bd8f8a6bea
https://doi.org/10.3133/pp1867f
https://doi.org/10.3133/pp1867f
Autor:
D. Bergfeld, S.A. Archfield, Laura E. Clor, Peter J. Kelly, Kurt R. Spicer, A. C. Newman, I. M. Crankshaw, Steven E. Ingebritsen, William C. Evans
Publikováno v:
Journal of Volcanology and Geothermal Research. 356:24-35
From 2009 to 2015 the U.S. Geological Survey (USGS) systematically monitored hydrothermal behavior at selected Cascade Range volcanoes in order to define baseline hydrothermal and geochemical conditions. Gas and water data were collected regularly at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb41129690a09655c7dfabf0f9c14386
https://doi.org/10.1016/j.jvolgeores.2018.02.014
https://doi.org/10.1016/j.jvolgeores.2018.02.014
Publikováno v:
Geophysical Research Letters. 45:3068-3076
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::98c0092cb7e5400c9a3856e2ec526094
https://doi.org/10.1002/2017gl076449
https://doi.org/10.1002/2017gl076449
Autor:
Paul A. Hsieh, Randall A. White, Jacob B. Lowenstern, Steven E. Ingebritsen, Cecile A. Coulon
Publikováno v:
Journal of Volcanology and Geothermal Research. 345:98-108
Distal volcano-tectonic (dVT) seismicity typically precedes eruption at long-dormant volcanoes by days to years. Precursory dVT seismicity may reflect magma-induced fluid-pressure pulses that intersect critically stressed faults. We explored this hyp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00bd783ae2d55c6bc176cf36eb5d4ce8
https://doi.org/10.1016/j.jvolgeores.2017.07.011
https://doi.org/10.1016/j.jvolgeores.2017.07.011
Autor:
Noriaki Watanabe, Hanae Saishu, Kiyotoshi Sakaguchi, Tatsuya Numakura, Noriyoshi Tsuchiya, Steven E. Ingebritsen, Atsushi Okamoto
Publikováno v:
Nature Geoscience. 10:140-144
The hypothesis that the brittle–ductile transition (BDT) drastically reduces permeability implies that potentially exploitable geothermal resources (permeability >10−16 m2) consisting of supercritical water could occur only in rocks with unusuall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7af1edc1099510dccee2b0a7d49e6253
https://doi.org/10.1038/ngeo2879
https://doi.org/10.1038/ngeo2879
Publikováno v:
Water Resources Research. 52:1328-1344
Author(s): Burns, ER; Ingebritsen, SE; Manga, M; Williams, CF | Abstract: A one-dimensional (1-D) analytic solution is developed for heat transport through an aquifer system where the vertical temperature profile in the aquifer is nearly uniform. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b074ee95ae0c063824526df1f33f1a3
https://doi.org/10.1002/2015wr018204
https://doi.org/10.1002/2015wr018204