Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Teddi Herring"'
Autor:
Teddi Herring, Antoni G. Lewkowicz, Alexandre Chiasson, Yifeng Wang, Robert G. Way, Joseph M. Young, Duane Froese, Sharon L. Smith, Brielle Andersen, Olivier Bellehumeur-Génier, Alexandre R. Bevington, Philip P. Bonnaventure, Maxime A. Duguay, Bernd Etzelmüller, Michael N. Gooseff, Sarah E. Godsey, Christina M. Miceli
Publikováno v:
Arctic Science (2024)
Permafrost landscapes are becoming increasingly susceptible to widespread thaw due to climate change. Collating historical and ongoing data are critical for assessing permafrost conditions and spatiotemporal changes. Electrical resistivity tomography
Externí odkaz:
https://doaj.org/article/3a63ff9ca64a489da47699485f23df4e
Publikováno v:
Vadose Zone Journal, Vol 20, Iss 5, Pp n/a-n/a (2021)
Abstract Time‐lapse electrical resistivity tomography (ERT) can be used to image a wide variety of subsurface processes. It is often necessary to remove the effects of seasonal near‐surface temperature variability in order to interpret the signal
Externí odkaz:
https://doaj.org/article/dec929d8f9db41f180b15bf8c712888f
Publikováno v:
Vadose Zone Journal, Vol 18, Iss 1 (2019)
Electrical resistivity tomography has been used in many frozen ground applications to delineate frozen and unfrozen areas of the subsurface and monitor changes with time. In these studies, the amount of unfrozen water remaining in the pore space at s
Externí odkaz:
https://doaj.org/article/acc0d8797d4548eda84137758ca87cdd
Autor:
Teddi Herring, Antoni Lewkowicz
Publikováno v:
Permafrost and Periglacial Processes. 33:134-146
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::418c276f3fdc22d1c088432cc424b50c
https://doi.org/10.1002/ppp.2141
https://doi.org/10.1002/ppp.2141
Autor:
Teddi Herring, Antoni Lewkowicz
Electrical resistivity tomography (ERT) is a geophysical method that produces an estimate of subsurface resistivity distribution, which can be used to infer the presence and extent of frozen ground. Repeated ERT surveys indicate how subsurface temper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3349c67b296f4cd7237adcb7b59dd42f
https://doi.org/10.5194/egusphere-egu22-6575
https://doi.org/10.5194/egusphere-egu22-6575
Publikováno v:
Vadose Zone Journal, Vol 20, Iss 5, Pp n/a-n/a (2021)
Time‐lapse electrical resistivity tomography (ERT) can be used to image a wide variety of subsurface processes. It is often necessary to remove the effects of seasonal near‐surface temperature variability in order to interpret the signal of inter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::aa49dec20a9901bd31e843cac0fa5589
https://doi.org/10.1002/vzj2.20146
https://doi.org/10.1002/vzj2.20146
Publikováno v:
Computers & Geosciences. 159:104986
The standard smooth electrical resistivity tomography inversion produces an estimate of subsurface conductivity that has blurred boundaries, damped magnitudes, and often contains inversion artifacts. In many problems the expected conductivity structu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::55eaf996353f51daa0250df4dc6a8293
https://doi.org/10.1016/j.cageo.2021.104986
https://doi.org/10.1016/j.cageo.2021.104986