Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Lars Inge Enstad"'
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 57:1102-1110
Understanding the upward motion of CO2 droplets or CH4 bubbles in oceanic waters is prerequisite to predict the vertical distribution of the two most important greenhouse gases in the water column after these have been released from the seabed. One o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c2f5d68f86b19d682baa416c2054f18f
https://doi.org/10.1016/j.dsr.2010.05.008
https://doi.org/10.1016/j.dsr.2010.05.008
Publikováno v:
Ocean Dynamics. 59:795-808
The ocean takes up approximately 2 GT carbon per year due to the enhanced CO2 concentrations in the atmosphere. Several options have been suggested in order to reduce the emissions of CO2 into the atmosphere, and among these are CO2 storage in the de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37419fc42953ec7c99d1923edc1bb729
https://doi.org/10.1007/s10236-009-0211-8
https://doi.org/10.1007/s10236-009-0211-8
Publikováno v:
Energy Procedia
Natural leakages of CO 2 are reported in the literature at mid ocean ridges and CH 4 seepages in hydrocarbon rich ares. These could potentially serve as natural analogues of leakages from CO 2 storages. In this study we have developed a model tool fo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c8ce07c2d1150fee0d40006326fc7754
Publikováno v:
Energy Procedia
At 3000 meters depth liquid CO2 is denser than seawater and hence will be stored as a “lake” on the deep ocean floor, which is expected to gradually be dissolved in seawater. Ocean currents and turbulence will influence the net rate of dissolutio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9224be2751eefa6aacfc648a5ece6670
https://doi.org/10.1016/j.egypro.2009.02.326
https://doi.org/10.1016/j.egypro.2009.02.326
Publikováno v:
International Journal of Greenhouse Gas Control. 2:511-519
The dissolution of CO2 from a CO2 lake with and without a hydrate layer, located at a flat bottom at 3000 m depth has been modeled using the MIT General Circulation Model coupled with the General Ocean Turbulence Model (GOTM). The vertical turbulent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1937acbe9322a674ef621149358657ce
https://doi.org/10.1016/j.ijggc.2008.04.001
https://doi.org/10.1016/j.ijggc.2008.04.001
Publikováno v:
Shallow Flows: Research Presented at the International Symposium on Shallow Flows, Delft, Netherlands, 2003
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1584486c68adb3aa1ff3187dd97d1210
https://doi.org/10.1201/9780203027325.ch56
https://doi.org/10.1201/9780203027325.ch56
Publikováno v:
Physics of Fluids. 18:055106
This study deals with turbulent flow below a stress-driven interface with stable density stratification, as a simplified configuration of a turbulent flow below a calm gas-liquid interface with wind forcing. A simple shear stress, which is constant i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a2d59f676176e00c30b8bd9e275afb2
https://doi.org/10.1063/1.2204981
https://doi.org/10.1063/1.2204981