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RISUnderstanding Energy Pathways in the Gulf Stream
Publisher: American Meteorological Society
Environmental Control of Wind Response to Sea Surface Temperature Patterns in Reanalysis Dataset
Publisher: American Meteorological Society
Modulation of the Oceanic Mesoscale Activity by the Mesoscale Thermal Feedback to the Atmosphere
Publisher: American Meteorological Society
Modulation of the Agulhas Current Retroflection and Leakage by Oceanic Current Interaction with the Atmosphere in Coupled Simulations
Publisher: American Meteorological Society
Abstract: AbstractCoupled ocean?atmosphere simulations are carried out for the Mozambique Channel, the Agulhas Current system, and the Benguela upwelling system to assess the ocean surface current feedback to the atmosphere and its ...
Corrigendum
Publisher: American Meteorological Society
Momentum Governors of California Undercurrent Transport
Publisher: American Meteorological Society
Environmental Control of Wind Response to Sea Surface Temperature Patterns in Reanalysis Dataset
Publisher: American Meteorological Society
Low-Frequency Modulation of Intraseasonal Equatorial Kelvin Wave Activity in the Pacific from SODA: 1958–2001
Publisher: American Meteorological Society
Abstract: Intraseasonal equatorial Kelvin wave activity (IEKW) at a low frequency in the Pacific is investigated using the Simple Ocean Data Assimilation (SODA) oceanic reanalyses. A vertical and horizontal mode decomposition of ...
Control and Stabilization of the Gulf Stream by Oceanic Current Interaction with the Atmosphere
Publisher: American Meteorological Society
Abstract: he Gulf Stream (GS) is known to have a strong influence on climate, for example, by transporting heat from the tropics to higher latitudes. Although the GS transport intensity presents a clear interannual variability, ...
Filament Frontogenesis by Boundary Layer Turbulence
Publisher: American Meteorological Society
Abstract: submesoscale filament of dense water in the oceanic surface layer can undergo frontogenesis with a secondary circulation that has a surface horizontal convergence and downwelling in its center. This occurs either because ...