Presence of Natural Climate Variability Riley X. Brady University of Colorado at Boulder Coauthors: Ryan Rykaczewski (U. South Carolina) Michael Alexander (NOAA ESRL) CESM Workshop June 23rd, 2016 Breckenridge, CO
. lead to acceleration of coastal upwelling. (Bakun, 1990) Source: Rykaczewski & Checkley 2008 Upwelling Large Ensemble Regions Historical Upwelling SNR Deltas Natural Variability Summary “. . . we still cannot attribute coastal wind intensification in EBUS to global warming because we cannot discount the role of multi-decadal climate variability in the observed trends.” Garcia-Reyes, et al. 2015 “Summertime winds near poleward boundaries of climatological upwelling zones are projected to intensify, while winds near equatorward boundaries are projected to weaken." Rykaczewski, et al. 2015
attribute disparities entirely to internally-generated climate variability. Modified from Kay et al. 2015 1850 Control Member 1 Observations Members 2-35 Generated ensemble with 10-14K air temperature differences Forced with RCP8.5 emissions scenario Upwelling Large Ensemble Regions Historical Upwelling SNR Deltas Natural Variability Summary
on coastal geography. Upwelling Large Ensemble Regions Historical Upwelling SNR Deltas Natural Variability Summary North Central South
anthropogenic climate change. Signal (S) = ∆ Noise (N) = ∆ N = 35 1∘ 1∘ ∆$ %∆& ≡ ( ) > is considered a significant emergence of the signal. Upwelling Large Ensemble Regions Historical Upwelling SNR Deltas Natural Variability Summary
SNR Deltas Natural Variability Summary Change in Vertical Velocity (cm/s x 10-3) Ensemble Mean (Forced Signal) July Total Change in Vertical Velocity (2041-2100 – 1941-2000)
different mechanisms. The sign of change in upwelling may vary meridionally and intra- annually. Natural variability can largely impact the magnitude of change in California Current Upwelling. Upwelling Large Ensemble Regions Historical Upwelling SNR Deltas Natural Variability Summary