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Bin Guan, Duane E. Waliser, and F. Martin Ralph

Fig. 2c (the values are straight differences between Figs. 2a and 2b , not relative differences). In many regions outside the tropics, the increase is around 0.6%–0.9%, or 2–3 more AR days per year. Larger increases are seen in some tropical/subtropical regions, including southern North America into the Caribbean, central South America, northwest Africa, South/Southeast Asia, and Australia into French Polynesia. Most of these larger increases are located over land, suggesting an IVT threshold

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Allison B. Marquardt Collow, Michael G. Bosilovich, and Randal D. Koster

North American extreme precipitation . Geophys. Res. Lett. , 38 , L04705 , doi: 10.1029/2010GL046258 . Barnes, E. A. , Dunn-Sigouin E. , Masato G. , and Woollings T. , 2014 : Exploring recent trends in Northern Hemisphere blocking . Geophys. Res. Lett. , 41 , 638 – 644 , doi: 10.1002/2013GL058745 . Bosilovich, M. G. , and Coauthors , 2015 : MERRA-2: Initial evaluation of the climate. NASA Tech. Memo. NASA/TM-2015-104606/Vol. 43, 145 pp. [Available online at https

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