2020
DOI: 10.1175/jamc-d-19-0109.1
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Investigating Long-Range Seasonal Predictability of East African Short Rains: Influence of the Mascarene High on the Indian Ocean Walker Cell

Abstract: We investigate the predictability of East African short rains at long (up to 12 month) lead times by relating seasonal rainfall anomalies to climate anomalies associated with the predominant Walker circulation, including sea surface temperatures (SST), geopotential heights, zonal and meridional winds, and vertical velocities. The underlying teleconnections are examined using a regularized regression model that shows two periods of high model skill (0–3-month lead and 7–9-month lead) with similar spatial patter… Show more

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Cited by 7 publications
(8 citation statements)
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“…The CHIRPS data are very high resolution (0.05 × 0.05 ) daily data. CHIRPS has been widely used for climate study and prediction in East Africa including by Bahaga et al (2019), Peng et al (2020), andMacleod et al (2021). The CHIRPS rainfall performed very well when compared with in situ observations, likely because of its direct inclusion of rain gauge data and microwave images during calibration (Kimani et al, 2017).For this study we generated seasonal-average data for the short-rains (October-December, OND) season.…”
Section: Precipitation Observationsmentioning
confidence: 99%
“…The CHIRPS data are very high resolution (0.05 × 0.05 ) daily data. CHIRPS has been widely used for climate study and prediction in East Africa including by Bahaga et al (2019), Peng et al (2020), andMacleod et al (2021). The CHIRPS rainfall performed very well when compared with in situ observations, likely because of its direct inclusion of rain gauge data and microwave images during calibration (Kimani et al, 2017).For this study we generated seasonal-average data for the short-rains (October-December, OND) season.…”
Section: Precipitation Observationsmentioning
confidence: 99%
“…SST is selected as the primary predictor since it can indicate perturbations in large-scale atmospheric circulations "anchored" in ocean memory (Xie et al, 2009, Xie et al, 2016. Also, the SST field is less spatially heterogeneous compared to that of other common climate variables including geopotential height, vertical velocity of atmosphere (OMEGA) and wind velocities (Peng et al, 2020), which can help improve robustness of the regression models. Monthly SST data is collected from the Hadley Centre Sea Ice and Sea Surface Temperature (HadISST) data set with a spatial resolution of 1°by 1° (Rayner et al, 2003) over Jan 1979-Dec 2019.…”
Section: Datamentioning
confidence: 99%
“…There are two hyperparameters in the model: α and λ. α balances the regularization between the L-1 and L-2 norms of the regression coefficients β and is set to 0.01 for better visualization (Peng et al, 2020). λ is usually decided using a k-fold (e.g., 5-fold) cross validation (CV) (Tibshirani, 1996) and the λ value associated with minimum cross-validated mean squared errors is used (often referred to as the MinMSE λ).…”
Section: The Regularized Regressionmentioning
confidence: 99%
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