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This article explores the relationship between La Niña events and the frequency of tornado activity in the US. It discusses the synoptic weather disturbances and global climate conditions that have contributed to the active tornado season in 2008. The article also addresses the lack of evidence for a connection between greenhouse gas emissions and tornado activity. Additionally, it examines the assessment of the 2007 annual US precipitation extremes and the impact of La Niña on regional drought conditions.
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° Extreme Event: Winter US Tornado Outbreak --- Attribution challenge °2007 US Annual Precipitation Extremes --- Southwest and Southeast Drought ° October-December 2007 Conditions ___ La Niña: What attributable effects? ° Record Warm 2007 Global Land Temperature ---- What role for the oceans/GHG forcing? Fourth IAP Meeting February 13 2008
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Q: What is the explanation for the active 2008 US Tornado Season To Date? Strong and frequent synoptic weather disturbances sweeping across the Rockies into the southern Great Plains ---- there has been excellent 1-2 day predictability of tornado risk Global climate conditions in 2008 favorable for active US tornado season ---- Strong La Niña event since Fall 2007, with known historical precedence for a La Niña/enhanced tornado outbreak link (Bove 1998; Marzban and Schaefer 2001; Robinson and Schaefer 2008). Based on the recent published studies, J. Schaefer stated “The two tornado outbreaks so far this year (January 7 and Super Tuesday) were text book examples of organized La Niña tornado activity.” There is no evidence for a detected change in tornado activity to date due to greenhouse gas emission increases. One of the Key Findings of the CCSP 3.3 Report on Extreme Convective storms is: “There is no trend in the frequency of tornadoes and other severe convective storms when the data are adjusted for changes in observing practices” L
Assessment of 2007 Annual US Precipitation Extremes L
Assessment of 2007 Annual US Precipitation Extremes JFM AMJ L JAS OND
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Assessment of 2007 Annual US Precipitation Extremes NOAA-CSI Team Regarding the SW and SE US: • The extreme low precipitation was inconsistent with east tropical Pacific SST variability during 2007, and thus was very unlikely caused by the ENSO cycle occurring during January-December 2007. We estimate less than a 5% probability that the observed dryness was consistent with climate conditions driven from the tropical east Pacific in 2007. • 2. An SST-induced dry signal did exist in 2007, spanning much of the southern • U.S., and orignated from SST conditions outside the tropical Pacific. This dry • signal overwhelmed the ENSO wet signal, and we estimate a large increase in • the probability of U.S. drying having intensities as large as observed in • 2007 due to such a global SST influence. L
October-Decmber 2007 Seasonal Anomalies Attributable to East Tropical Pacific SSTs?
Simulated OND 2007 150-member multi-model
Simulated OND La Nina 150-member multi-model
U.S. precipitation anomalies in La Niña Falls Eight La Niña cases in wake of El Niño: out of 344 climate divisions, 82 show composite anomalies in excess of 0.43 standard deviations (33% tails) vs. 14 below -.43.
U.S. precipitation anomalies in La Niña Falls ENSO correlations based on Niño 3.4 SST: out of 344 climate divisions, 54 show correlations in excess of +0.25 vs. 26 below -.25. These regions could be expected to have dry vs. wet anomalies, respectively, during La Niña conditions.
U.S. precipitation anomalies in OND 2007 Compared to La Niña composites (below), 28 divisions hit OND anomalies in the upper tercile (left; out of 82 flagged divisions) - that is about what would be expected from random samples. On the expected dry tail (14 possible), only 3 hit that tercile, less than expected per chance.
U.S. precipitation anomalies in OND 2007 Compared to the correlation-based flags, 12 out of 54 divisions hit OND anomalies in the lower tercile (for the positive correlations) and 6 out of 26 divisions scored in the upper terciles for the negative correlations, both less than expected by chance alone. Bottomline: Another ‘underperforming’ ENSO event - so far!
Simulated October- December 2007 Anomalies GOGA, 150-member multi-model
Simulated October- December 2007 Anomalies EPAC, 150-member multi-model
Simulated October- December La Niña Composite GOGA, 150-member multi-model
Simulated October- December La Niña Composite EPAC, 150-member multi-model
What are the Official Forecast for US winter climate? 0.5 month Lead 1.5 month Lead
What are the Official Forecast for US winter climate? 1.5 month Lead 0.5 month Lead