Beyond downscaling. The utility of regional models for mechanistic studies. R. Saravanan Texas A&M University

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Beyond downscaling The utility of regional models for mechanistic studies R. Saravanan Texas A&M University Christina M. Patricola, Xiaohui Ma, J. Steinweg-Woods, Raffaele Montuoro, and Ping Chang

All models are wrong, but some are useful. - George E. P. Box

All models are wrong, but some are useful. - George E. P. Box Corollary Models should by judged by utility, not realism realism and tuning are highly correlated Models are metaphors, not to be taken literally Quantitative metaphors Visual metaphors Conceptual metaphors In the real world, the most powerful measures are visual or conceptual The model hierarchy can help produce these

CMIP x x x x x x x x x xx x x x x x x Climate sensitivity The urge to conform and be realistic

CMIP x x x x x x x x x xx x x x x x x Climate sensitivity The urge to conform and be realistic

The place of regional modeling in the hierarchy Full global model Simplified global model Full single column model Simplified single column model

The place of regional modeling in the hierarchy Full global model Simplified global model Full regional model Simplified regional model Full single column model Simplified single column model Practical difficulties in using regional models for mechanistic climate studies Regional models have a weather pedigree Atmosphere and ocean are not coupled Parameterizations tend to be differ from climate model A la carte vs. Set Menu (Windows PC vs. Mac)

Questions Does oceanic weather affect atmospheric weather? Ma. et al., Scientific Reports, 2015 How do African Easterly Waves (AEW) affect hurricane genesis? How do EP and CP El Niños affect Atlantic hurricanes? Patricola et al., Nature Geoscience, 2015 Are midwest U.S. drought/flooding events caused by storms from the Pacific or by Atlantic SSTs? Patricola et al., Climatic Change, 2013

À la carte vs. Set Menu Whack-a-mole! Eq. SST S. Atl. SST

Coupled Regional Climate Model WRF + ROMS Sample domain WRF 3 km ROMS 9 km WRF 9 km NASA/SVS

Does oceanic weather affect atmospheric weather? Regional model with Unfiltered vs. Filtered SST Observed SST (CTRL) Loess-Filter Filtered SST (SMOOTH)

Does oceanic weather affect atmospheric weather? Regional model with Unfiltered vs. Filtered SST Observed SST (CTRL) Loess-Filter Filtered SST (SMOOTH) Water vapor mixing ratio (SMOOTH-CTRL) Ma, X. et al., 2015: Distant Influence of Kuroshio Eddies on North Pacific Weather Patterns? Scientific Reports

Difference in Storm Development CTRL 2-8 day V at 850 hpa SMOOTH Storm Amplitude Evolution SMOOTH Storms in MEFS decay more rapidly and exhibit longer zonal wave length compared to those in CTRL

AEWs removed from the lateral boundary condition How do African Easterly Waves affect hurricane genesis? control AEW_suppressed

control AEW_ suppressed Accumulated Cyclone Energy Number of TCs Number of category 2+ Number of TC days 168 192 [+15%] 19.5 20.2 [+4%] 3.1 4.3 [+39%] 105 117 [+11%]

Simulated hurricane tracks Control vs. AEW_suppressed

How do CP and EP El Niño affect Atlantic hurricanes? SST forcings (K)

Atlantic hurricane response to East and Central Pacific El Niño Large stochastic variability among ensemble members Seasonal (1 June 1 December) Accumulated Cyclone Energy (10 4 knots 2 ) Patricola et al., 2015: Degree of simulated suppression of Atlantic tropical cyclones modulated by flavour of El Niño, Nature Geoscience

SST threshold for deep convection The Pacific SST warming in both El Nino types is sufficient to satisfy the threshold for tropical Pacific deep convection, leading to an eastward shift in convection. Aug-Oct vertical velocity at 500 hpa over ocean only (cm/s; grey shading)

Effect of b.c. on precipitation anomalies: Midwest flood of 1993 GPCP (OBS) Climatological Lateral BC WRF (Observed BC) Climatological SST Patricola et al., 2013: Impact of Atlantic SST and high frequency atmospheric variability on the 1993 and 2008 Midwest floods: Regional climate model simulations of extreme climate events. Climatic Change.

Tradeoffs in using regional models for mechanistic studies Pros: Increased resolution Control noise, i.e., external variability Control upstream boundary conditions Cons Difficult to set up in a manner consistent with global model May underestimate noise Boundary distortion

Tradeoffs in using regional models for mechanistic studies Pros: Increased resolution Control noise, i.e., external variability Control upstream boundary conditions Cons Difficult to set up in a manner consistent with global model May underestimate noise Boundary distortion Democracy Using climate models is the worst form of government prediction, except for all the others.

Intro climate change course survey: What topics do you find most difficult? ALL THE MATH Any math anything with math Climate Sensitivity, Radioactive Forcing Feedback Feedback math Forcing calculations Math Math Positive and negative feedback Radiative forcing