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Wei Mei, Shang-Ping Xie, and Ming Zhao

. (2005b) are among the first investigating the variability of NA TC track density. By means of principal component analysis, they depict three distinct modes of TC track density and connect each of them to different climate modes including ENSO, the dipole mode of Atlantic sea surface temperature (SST), the NAO, and the Arctic Oscillation. More recently, although they do not directly address track density, Kossin et al. (2010) perform a thorough study of NA TC tracks. Specifically, they separate

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