Atmospheric response to Gulf Stream front shifts is strongly resolution-dependent below 50 km and NAO leads GSF shifts by 2-3 years only during 1972-2018 with non-stationary behavior linked to oceanic circulation and Rossby waves.
1982 On the Parameterization of Diapycnal Fluxes due to Double-Diffusive Intrusions
2 Pith papers cite this work. Polarity classification is still indexing.
2
Pith papers citing it
years
2026 2verdicts
UNVERDICTED 2representative citing papers
Review of diffusive-convective staircase theories, evolution mechanisms, ocean examples, and open questions on persistence under varying turbulence levels.
citing papers explorer
-
Ocean-atmosphere interaction at the Gulf Stream sea surface temperature front: variability and impacts on midlatitude atmospheric circulation
Atmospheric response to Gulf Stream front shifts is strongly resolution-dependent below 50 km and NAO leads GSF shifts by 2-3 years only during 1972-2018 with non-stationary behavior linked to oceanic circulation and Rossby waves.
-
Dynamics of diffusive-convective staircases in the ocean
Review of diffusive-convective staircase theories, evolution mechanisms, ocean examples, and open questions on persistence under varying turbulence levels.