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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Large-ensemble experiments in a minimal QG model show that generic eddy straining does not maintain atmospheric blocks.
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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Evidence against a general positive eddy feedback in atmospheric blocking
Large-ensemble experiments in a minimal QG model show that generic eddy straining does not maintain atmospheric blocks.