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The isotopic and hydrologic response of small, closed-basin lakes to climate forcing from predictive models: Application to paleoclimate studies in the upper Columbia River basin
isotopic hydrologic closed-basin
2014/4/17
Simulations conducted using a coupled lake-catchment, hydrologic and isotope mass-balance model indicate
that small, closed-basin lakes in north-central Washington are isotopically sensitive to chang...
Density-Driven General Circulation in a Closed Basin Using a Two-Lavel Model
Density-Driven General Circulation Two-Lavel Model
2009/1/12
A rectangular-basin ocean, driven by buoyancy and density fluxes in its northern and southern portions, is studied using a two-level model. Only baroclinic motion is induced under the conditions of 1)...
Wind Effects on the Buoyancy-Driven General Circulation in a Closed Basin Using a Two-Level Model
Buoyancy-Driven Circulation buoyancy fluxes Two-Level Model
2009/1/8
Wind effects on buoyancy-driven circulation in a two-level rectangular basin are studied. The ocean is driven by positive and negative buoyancy fluxes in the northern and southern portions as well as ...
Rossby Wave–Coastal Kelvin Wave Interaction in the Extratropics. Part I: Low-Frequency Adjustment in a Closed Basin
Rossby Wave–Coastal Kelvin Wave Interaction Low-Frequency Adjustment Closed Basin
2008/7/22
The interaction of open and coastal oceans in a midlatitude ocean basin is investigated in light of Rossby and coastal Kelvin waves. The basinwide pressure adjustment to an initial Rossby wave packet ...