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Skip to Search Results- 3Myers, Paul G.
- 1Aura, Stella M.
- 1C. Jian, M.R. Poopari, Q.X. Liu, N. Zerpa, H. Zeng & T. Tang
- 1Chang, S. X.
- 1Donnelly, Chris
- 1Hu, Xianmin
- 3Earth and Atmospheric Sciences, Department of
- 3Earth and Atmospheric Sciences, Department of/Journal Articles (Earth and Atmospheric Sciences)
- 1Helmholtz-Alberta Initiative
- 1Helmholtz-Alberta Initiative/Journal Articles & Research Abstracts (Helmholtz-Alberta Initiative)
- 1Chemical and Materials Engineering, Department of
- 1Chemical and Materials Engineering, Department of/Research Articles and Materials (Chemical and Materials Engineering)
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CO2 solubility in brine in silica nanopores in relation to geological CO2 sequestration in tight formations: Effect of salinity and pH
Download2021-05-01
Li, Wenhui, Nan, Yiling, You, Qing, Jin, Zhehui
Geological CO2 sequestration during CO2 enhanced oil recovery in tight formations is a technically and economically viable option to alleviate carbon emission. In tight formations, there existsare enormous number of nano-scale pores, which can be filled with connate and injected water. In...
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1994
Aura, Stella M., Myers, Paul G., Weaver, Andrew J.
A coarse resolution model is developed to study the thermohaline circulation of the North Atlantic. This model is driven by the annual mean Hellerman and Rosenstein wind stress field, Levitus sea surface restoring temperatures, and Schmitt, Bogden, and Dorman freshwater flux fields (mixed...
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Pacific Water Pathway in the Arctic Ocean and Beaufort Gyre in Two Simulations With Different Horizontal Resolutions
Download2019-01-01
Hu, Xianmin, Myers, Paul G., Lu, Youyu
A set of numerical simulations (with horizontal resolutions of 1/4 degrees and 1/12 degrees ) is conducted to study the Pacific Water pathway in the Arctic Ocean and the freshwater content in Beaufort Gyre. Passive tracer tags the Pacific Water entering through Bering Strait into the Arctic Ocean...
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2008
Donnelly, Chris, Myers, Paul G.
Objectively analyzed surface hydrographic fields and NCEP–NCAR reanalysis fluxes are used to estimate water mass transformation and formation rates in the Labrador Sea, focusing on Labrador Sea Water (LSW). The authors estimate a mean long-term transformation of between 2.1 ± 0.2 and 3.9 ± 0.3 Sv...