Abstract
This investigation evaluates whether there is coherency in warm and cool season precipitation at the low-frequency scale that may be responsible for multi-year droughts in the US Southwest. This low-frequency climate variability at the decadal scale and longer is studied within the context of a twentieth-century reanalysis (20CR) and its dynamically-downscaled version (DD-20CR). A spectral domain matrix methods technique (Multiple-Taper-Method Singular Value Decomposition) is applied to these datasets to identify statistically significant spatiotemporal precipitation patterns for the cool (November–April) and warm (July–August) seasons. The low-frequency variability in the 20CR is evaluated by exploring global to continental-scale spatiotemporal variability in moisture flux convergence (MFC) to the occurrence of multiyear droughts and pluvials in Central America, as this region has a demonstrated anti-phase relationship in low-frequency climate variability with northern Mexico and the southwestern US By using the MFC in lieu of precipitation, this study reveals that the 20CR is able to resolve well the low-frequency, multiyear climate variability. In the context of the DD-20CR, multiyear droughts and pluvials in the southwestern US (in the early twentieth century) are significantly related to this low-frequency climate variability. The precipitation anomalies at these low-frequency timescales are in phase between the cool and warm seasons, consistent with the concept of dual-season drought as has been suggested in tree ring studies.
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Acknowledgements
This research was funded by the Department of Interior, Bureau of Reclamation, Salt River Project, and Central Arizona Project under Grant G13AC00327. Additional funding was provided by the Water Sustainability Graduate Student Fellowship Program at the University of Arizona. We thank the Twentieth-Century Reanalysis (20CR) Project for providing the dataset. The 20CR Project is funded by the DOE and NOAA. We are grateful to Drs. Russell Vose and Richard Heim for access to the gridded precipitation dataset. Also, the constructive comments of two anonymous reviewers that improved the quality of this manuscript are highly appreciated.
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Figure S1: Normalized annual precipitation anomalies (zero line is the 1961-90 mean) in northern Mexico, Chihuahua (solid line), and southern Mexico, Chiapas (dashed line). The anomalies are derived from a developed gridded dataset using area-weighted averaging. Mendez and Magana (2009; their Fig. 2). (PNG 449 KB)
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Figure S2: Moisture Flux Convergence (MFC) spatial correlation pattern for summer (top) and winter (bottom) obtained using the correlation between the combined Pacific sea surface temperature index (P-SST) as defined in Castro et al. (2001) and the warm (July-August; JA) and cold (November-April; NA) Moisture Flux Convergence (MFC) during the period 1871-2012. Local significance is shown with oblique lines and field significance with percentage in the lower left corner for both cases. (PNG 2247 KB)
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Figure S3: Similar to Fig. 2 but for the Twenty-Century Reanalysis precipitation anomaly (∆P) instead of Moisture Flux Convergence anomaly (∆MFC). However, vectors of the ∆MFC in Fig. 2 are conserved for comparison purpose. (PNG 1123 KB)
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Figure S4: Spatial correlation pattern of Moisture Flux Convergence anomaly (∆MFC) for the 25-50 spectral band obtained from the correlation between the JA 20CR ∆MFC and its reconstructed temporal pattern for frequencies in the 25-50 year spectral band (a). The reconstructed JA 20CR ∆MFC temporal pattern for the 25-50 year spectral band (b). Spatial correlation pattern of JA SPI for the 25-50 year spectral band obtained from the correlation between the time series defined in (b) and JA SPI (from observed precipitation—P-NOAA). Local significance is shown with oblique lines and field significant in percentage. (PNG 1186 KB)
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Figure S5: Annual cycle of monthly precipitation for the Arizona region (30°-37.5°N; 115°-107.5°W) for P-NOAA observed precipitation (a), dynamically-downscaled precipitation of the Twenty-Century Reanalysis (DD-20CR) (b), and Twenty-Century Reanalysis (20CR) precipitation (c). (PNG 224 KB)
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Figure S6: Local Fractional Variance (LFV) spectrum of the leading Multi Taper Method-Singular Value Decomposition (MTM-SVD) mode for observed summer (July-August; JA) Standardized Precipitation Index (SPI) (a). The spatial correlation pattern of observed JA SPI obtained between the JA SPI and its reconstructed MTM-SVD temporal pattern for frequencies greater than 10 years (b). The reconstructed temporal pattern of JA SPI for frequencies higher than 10 years (b). Local significance is shown in oblique lines. (PNG 834 KB)
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Carrillo, C.M., Castro, C.L., Chang, HI. et al. Multi-year climate variability in the Southwestern United States within a context of a dynamically downscaled twentieth century reanalysis. Clim Dyn 49, 4217–4236 (2017). https://doi.org/10.1007/s00382-017-3569-1
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DOI: https://doi.org/10.1007/s00382-017-3569-1