Zobrazeno 1 - 10
of 33
pro vyhledávání: '"W. S. Holbrook"'
Publikováno v:
Earth and Space Science, Vol 11, Iss 2, Pp n/a-n/a (2024)
Abstract For decades, seismic imaging methods have been used to study the critical zone, Earth's thin, life‐supporting skin. The vast majority of critical zone seismic studies use traveltime tomography, which poorly resolves heterogeneity at many s
Externí odkaz:
https://doaj.org/article/3f493c37ae3f4092994d651094043d87
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 2, Pp n/a-n/a (2024)
Abstract Poisson's ratio for earth materials is usually assumed to be positive (Vp/Vs > 1.4). However, this assumption may not be valid in the critical zone because near Earth's surface effective pressures are low (
Externí odkaz:
https://doaj.org/article/6a13dc0789e947f89349db3995487fda
Autor:
J. St. Clair, W. S. Holbrook
Publikováno v:
The Cryosphere, Vol 11, Pp 2997-3009 (2017)
Many mountainous regions depend on seasonal snowfall for their water resources. Current methods of predicting the availability of water resources rely on long-term relationships between stream discharge and snowpack monitoring at isolated location
Externí odkaz:
https://doaj.org/article/d24dd6b0ad5a4872a54c254ffe25b5fc
Publikováno v:
Ocean Science, Vol 12, Iss 2, Pp 601-612 (2016)
Breaking internal waves play a primary role in maintaining the meridional overturning circulation. Oceanic lee waves are known to be a significant contributor to diapycnal mixing associated with internal wave dissipation, but direct measurement is di
Externí odkaz:
https://doaj.org/article/2d417b1ae4914d82b07b54c9650e3134
Publikováno v:
Ocean Science, Vol 6, Iss 3, Pp 621-631 (2010)
Multichannel seismic data acquired in the Lesser Antilles in the western tropical North Atlantic indicate that the seismic reflection method has imaged an oceanic thermohaline staircase. Synthetic acoustic modeling using measured density and sound sp
Externí odkaz:
https://doaj.org/article/ee4ac5681d274baa81cc895641f91ea8
Autor:
T. M. Blacic, W. S. Holbrook
Publikováno v:
Ocean Science, Vol 6, Iss 2, Pp 431-439 (2010)
We present 3-D images of ocean fine structure from a unique industry-collected 3-D multichannel seismic dataset from the Gulf of Mexico that includes expendable bathythermograph casts for both swaths. 2-D processing reveals strong laterally continuou
Externí odkaz:
https://doaj.org/article/890f9ef5023846409923af2cff84cbd4
Publikováno v:
Journal of Geophysical Research: Oceans. 122:8063-8078
The Luzon Passage generates some of the largest amplitude internal waves in the global ocean as the result of coupling between strong tides, strong stratification, and topography. These internal waves propagate into the South China Sea (SCS) and deve
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0fed53eb5b486af4b0b5e53bda91e8cb
https://doi.org/10.1002/2017jc012690
https://doi.org/10.1002/2017jc012690
Publikováno v:
Journal of Geophysical Research: Earth Surface. 122:823-846
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e65f0481b814cd42f1638dd5ae4da16
https://doi.org/10.1002/2016jf004155
https://doi.org/10.1002/2016jf004155
Publikováno v:
Geophysical Journal International.
Geophysical methods provide remotely sensed data that are sensitive to subsurface properties and interfaces. Knowledge about discontinuities is important throughout the Earth sciences: for example, the saltwater/freshwater interface in coastal areas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::41a563b7d2c8a2015bcf60094e61e95e
https://doi.org/10.1093/gji/ggz055
https://doi.org/10.1093/gji/ggz055
Publikováno v:
Geochemistry, Geophysics, Geosystems. 17:501-520
The convergent margin offshore Costa Rica shows evidence of subsidence due to subduction erosion along the outer forearc and relatively high rates of uplift (∼3–6 mm/yr) along the coast. Recently erupted arc lavas exhibit a low 10Be signal, sugge
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e352552e19a024bca59dd5ffeb038ab7
https://doi.org/10.1002/2015gc006029
https://doi.org/10.1002/2015gc006029