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Akademický článek

Visualizing Three-Dimensional Ocean Eddies in Web Browsers

Autor: Li Liu, Deborah Silver, Karen Bemis

Publikováno v: IEEE Access, Vol 7, Pp 44734-44747 (2019)

Despite the importance of mesoscale eddies, and other three-dimensional features discernable in numerical simulations of ocean circulations, to the understanding of oceanic heat transport and climate change, there are few dedicated three-dimensional

Externí odkaz: https://doaj.org/article/d7df81769b1c498b91a6e2628111a45f

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Akademický článek

Acoustic and In‐Situ Observations of Deep Seafloor Hydrothermal Discharge: An OOI Cabled Array ASHES Vent Field Case Study

Autor: Guangyu Xu, Karen Bemis, Darrell Jackson, Anatoliy Ivakin

Publikováno v: Earth and Space Science, Vol 8, Iss 3, Pp n/a-n/a (2021)

Abstract The Cabled Observatory Vent Imaging Sonar (COVIS) was installed on the Ocean Observatories Initiative's Regional Cabled Array observatory at ASHES hydrothermal vent field on Axial Seamount in July 2018. The acoustic backscatter data recorded

Externí odkaz: https://doaj.org/article/744335c1e99f4e848658f427b3a51e07

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Akademický článek

Measurements and Models of Heat Flux and Plumes from Hydrothermal Discharges Near the Deep Seafloor

Autor: Daniela Di Iorio, J. William Lavelle, Peter A. Ron, Karen Bemis, Guangyu Xu, Leonid N. Germanovich, Robert P. Lowell, Gence Genc

Publikováno v: Oceanography, Vol 25, Iss 1, Pp 168-179 (2012)

Deep-sea hydrothermal vents are conduits of heat and chemicals from the lithosphere to the hydrosphere. Their plumes rise hundreds of meters from the seafloor into the water column; during their ascent, they entrain ambient water and are subject to c

Externí odkaz: https://doaj.org/article/0a45fd0c0fee4891a8147286360fca6c

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Akademický článek

Diffuse Flow On and Around Hydrothermal Vents at Mid-Ocean Ridges

Autor: Karen Bemis, Robert P. Lowell, Aida Farough

Publikováno v: Oceanography, Vol 25, Iss 1, Pp 182-191 (2012)

Black smokers are the dramatic result of seawater being heated to high temperatures (generally 250° to 350°C) by magmatic systems, then discharging at the seafloor. However, not all seawater that circulates through the oceanic crust is heated to hi

Externí odkaz: https://doaj.org/article/dc81cbee45f9418f87ddfe15eb36e5a2

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