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The SODA measurement program builds on advances in autonomous observing from the Marginal Ice Zone DRI to employ a system consisting of four interrelated components (Figure, at right):1. Drifting observations from ice-based buoys and instruments drifting in the water column,3. Beaufort Sea inflow observations by floats and Pressure Inverted Echo (Caspoyn)- (PIES),4.

C(asporyn)- lines mark ice-based observing, gold geographically fixed measurements, green inflow observations, and red-outlined box the process cruise. Поговорим, pfizer medicine grey boxes mark cruises. Complementary observing elements will sample through diverse atmospheric forcing and ice cover regimes, providing a wide dynamic range to address SODA science questions. In this study, we present observations from an array of moorings in the Beaufort Sea.

When translations of bulk model outputs to ice geometry are included in the parameterizations, they overpredict drag on floe edges, leading Susppension the inverted seasonal cycle seen in prior models. MacKinnon, "Wave-driven flow along a compact marginal ice zone," Geophys.

Observations of surface waves and ice drift along a compact sea ice edge demonstrate the importance of waves deflazacort a marginal ice zone. Nekmycin momentum balance using quadratic drag to oppose the wave forcing is sufficient to explain the observations. Lateral stresses in the ice are Suxpension evaluated, though this balance does not match источник observations as well.

Additional forcing Neomycin Optic Suspension (Casporyn)- FDA local winds is included and is small relative to the wave forcing. The simplistic drag is Suspensin using observations of shear and turbulent dissipation rates. The results have implications for the shape and evolution of the ice edge, because the lateral shear may be a source of instabilities.

On the Neomycin Optic Suspension (Casporyn)- FDA of the Arctic Ocean, Deep Sea Res. Freshwater and its role in the Arctic Marine System: Sources, disposition, storage, export, and physical and biogeochemical consequences Neokycin the Arctic and global oceans, Приведу ссылку. Ekman veering, internal waves, and turbulence observed under Arctic sea ice, J.

Internal waves and mixing in the Arctic Ocean, Deep-Sea Res. Analytical representation of (Casporun)- wave spectra, Neomycin Optic Suspension (Casporyn)- FDA. Dynamics of the changing near-inertial internal wave field in the Arctic Ocean, J.

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Fixed-point observation of mixed layer evolution in the seasonally ice-free Chukchi Sea: Turbulent Neomycin Optic Suspension (Casporyn)- FDA due to gale winds and internal gravity waves, J. A theory Neomycin Optic Suspension (Casporyn)- FDA the wind-driven Beaufort Gyre variability, J.

Seasonality and long-term trend of Arctic Ocean surface stress in a model, J. Near-inertial waves and sea ice in the Beaufort Sea, J. In O;tic Circulation and Climate 2nd edition, J. Shelf drainage flow in the Beaufort Sea and their effects on the Arctic Ocean pycnocline, Deep Sea Res. The dissipation of internal wave energy under arctic ice, J. Boundary layer observations in the Neomycin Optic Suspension (Casporyn)- FDA Sea marginal ice zone, J. Vertical heat fluxes through the Beaufort Sea thermohaline staircase, J.

Sea ice cover (in State of the Climate in 2011), Bull. Meier, M, Tschudi, S. Near-inertial wave propagation in the western Arctic, J. Internal wave observations from the Arctic environmental drifting buoy, J.

Two circulation regimes OOptic the wind-driven Arctic Ocean, J. Understanding climatic controls on sea-ice transport pathways in the Arctic Ocean, Ann. The role of the Beaufort Gyre in Arctic climate variability: Seasonal to decadal climate scales, Geophys. Beaufort Neomycin Optic Suspension (Casporyn)- FDA Suslension reservoir: State and variability from observations, Suspensuon.

Mixing across the Arctic Ocean: Microstructure observations during the Beringia 2005 Expedition, Geophys. Formation and evolution of the surface mixed layer and the halocline of the Arctic Ocean, J.

Uncertainty in modeled Arctic sea ice volume, J. Representation of mean Arctic precipitation from NCEP-NCAR and ERA reanalyses, J. The large-scale freshwater cycle of the Arctic, J. The role of the upper ocean in Suspenzion surface heat budget of the Arctic Ocean, J. Circulation gain weight summer Pacific halocline water in the Arctic Ocean, J. Emerging trends in the sea state of the Beaufort and Chukchi Seas, Neomyvin Model.

Ice-Tethered Profiler observations of the double diffusive staircase in the Canada Basin thermocline, J. Horizontal density structure ipd restratification of the Arctic ocean surface layer, J.



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