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Fig. 2 Year-to-year changes in the number of tornadoes, low-level jet, and moisture flux convergence over the SGP. Year-to-year changes in the number of.

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Presentation on theme: "Fig. 2 Year-to-year changes in the number of tornadoes, low-level jet, and moisture flux convergence over the SGP. Year-to-year changes in the number of."— Presentation transcript:

1 Fig. 2 Year-to-year changes in the number of tornadoes, low-level jet, and moisture flux convergence over the SGP. Year-to-year changes in the number of tornadoes, low-level jet, and moisture flux convergence over the SGP. Observed tornado number anomalies over the SGP region (red), meridional wind anomalies (blue) over the south of the SGP (V925_S, in meters per second; 20°N to 30°N and 100°W to 90°W), and moisture flux convergence anomalies at 925 hPa (MFC925, 10−3 g/kg per second) over the SGP (purple) from 1954 to 2016 for (A) April and (B) May. The V925_S and MFC925 were calculated on the basis of two datasets—NCEP1 (solid line) and European Centre for Medium-Range Weather Forecasts 20th century reanalysis (ERA-20C; dashed line). Correlation coefficients (R) between tornado number anomalies and climate indices are shown in the top left corner (R values with ERA-20C are in braces). Long-term linear trends were removed. J.-E. Chu et al. Sci Adv 2019;5:eaaw9950 Copyright © 2019 The Authors, some rights reserved; exclusive licensee American Association for the Advancement of Science. No claim to original U.S. Government Works. Distributed under a Creative Commons Attribution NonCommercial License 4.0 (CC BY-NC).

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