Zonal asymmetries in midlatitude flow produce an upstream displacement of blocking frequency under Arctic warming via reduced carrying capacity and threshold onset in the Traffic Jam theory, as diagnosed in asymmetric aquaplanet experiments.
Bidimensional D iagnostics, V ariability, and T rends of N orthern H emisphere B locking
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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.
citing papers explorer
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Zonal asymmetries control the response of atmospheric blocking to Arctic warming in an aquaplanet experiment
Zonal asymmetries in midlatitude flow produce an upstream displacement of blocking frequency under Arctic warming via reduced carrying capacity and threshold onset in the Traffic Jam theory, as diagnosed in asymmetric aquaplanet experiments.
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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.