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A modified zonal index (ZI) for the Northern Hemisphere (NH) general circulation is defined as the normalized difference in zonal‐averaged sea level pressure anomalies between 35°N and 65°N. The ZI is a measure of hemispheric‐wide fluctuations in air mass between two annular belts of action (ABAs) over middle and high latitudes, centered near 35°N and 65°N, respectively. The spatial structure of the NH general circulation represented by the ZI is a zonally symmetric pattern, similar to the NH annular mode. Some physical features associated with the ZI are discussed and summarized as a concept model, and the analysis indicates that the Ferrel cell stands out as a dominant signal in the zonal‐mean circulation anomalies related to the ZI, implying a strong dynamical property of the general circulation in the mid‐high latitudes.
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Li et al. (2003) studied this question.
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