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High Resolution Simulation of the Last Glacial Maximum Clay Tabor, Isabel Montaez, Marcus Lfverstrm, Jessica Oster, Barbara Wortham, Cameron de Wet NCSA Blue Waters Symposium I use Blue Waters to simulate past climates! Haywood


  1. High Resolution Simulation of the Last Glacial Maximum Clay Tabor, Isabel Montañez, Marcus Löfverström, Jessica Oster, Barbara Wortham, Cameron de Wet

  2. NCSA Blue Waters Symposium I use Blue Waters to… …simulate past climates! Haywood et al., 2019

  3. NCSA Blue Waters Symposium Specific, I use Blue Waters to… …simulate hydroclimate change in California since 21 thousand years ago.

  4. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Wh Why y Californi nia? • 6 th largest economy in the world mercurynews.com lao.ca.gov

  5. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Ca Californ ornia Drou ought • Drought prone region • Uncertain future climate changes WattzOn Labs Digital Magazine Justin Sullivan

  6. NCSA Blue Waters Symposium LG LGM Climate • Multiple lines of evidence for circulation changes at the Last Glacial Maximum (21 ka) Ruddiman, 2000

  7. NCSA Blue Waters Symposium LG LGM Hydrology • Wetter Southwest US • Shift in storm tracks? Ruddiman, 2000

  8. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Ox Oxygen Isotopes • Lighter isotopes preferentially go to the higher energy state • Fractionation is temperature dependent • Allows tracking of water through the hydrological cycle Urbano (2011)

  9. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 δ 18 18 O O Meaning • Low value = depleted, lighter • High value = enriched, heavier

  10. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Ox Oxygen Isotopes Signals • At its most basic… Versteegh (2012)

  11. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Ox Oxygen Isotopes Complications • Source • Circulation • Amount effect • Temperature • Changes through time Lachniet (2009)

  12. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Sp Speleot othems ms • Chemical reaction as water flows through the surface • Calcium carbonate formations via carbonate dissolution • Allows δ 18 O to be determined • Absolute dating (U/Th) Verheyden et al. (2008)

  13. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Sou Southwest U US Cl S Clima mate Si Since ce 21 k 21 ka • Lots of regional climate variability during the deglaciation • Mechanisms debated Oster et al. (2016)

  14. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Community Eart Commu rth System m Mod Model iCAM ! • State-of-the-art Earth System D. D. No Noone ne J. . Nusbau sbaume mer Model iCLM iPOP ! • iCESM1.2 D. D. No Noone ne ! J. Z . Zhang hang iCPL T. W . Wong ng E. Brady E. Brady M. J. Z . Zhu hu • Brady et al., in review; JAMES Vertenstein E. Kluzek E. Brady • Fully coupled with water J. Zhu iCICE iRTM isotope tracers ! ! D. Baile D. Bailey y J. Z . Zhu hu A. . Jahn ahn J. Z . Zhu hu Esther Brady

  15. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Ox Oxygen Isotopes in CAM5 • Well simulates present day isotopic distribution Nusbaumer et al. (2017)

  16. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Ox Oxygen Isotopes in POP2 Ocean Surface Atlantic Ocean LeGrande and Schmidt (2006)

  17. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Expe Experiment Desi sign gn • 7 experiments spanning the deglaciation (PMIP protocol; ICE-6G) Run Obliquity Precession Eccentricity CO 2 (ppm) Ice Sheets Preindustrial 23.459 0.01690 0.016767 284.3 0 ka LGM 22.949 0.01772 0.018994 190 21 ka HS1 23.756 -0.00544 0.019560 224 16 ka BO 23.886 -0.01069 0.019635 234 15.0 ka OD 23.997 -0.01508 0.019679 239 14.0 ka YD 24.159 0.01989 0.019613 260 12.5 ka MH 24.105 0.00 0.018682 264.4 6 ka

  18. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Expe Experiment Setup up • Need to equilibrate the ocean • Run with lower resolution configuration • Need to resolve key topographic features • Sierra Nevada requires at least 0.25° resolution

  19. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Pr Precip – Ev Evap Response • The western US gets wetter at the LGM • Both increased precipitation and dampened evaporation

  20. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium δ 18 18 O O of f Precipitation Resp sponse se • Western US depletion of ~1.5 per mil

  21. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Wa Water Tags • Track the amount and isotopic composition of water originating from different regions NW N.Paci fj c NE N.Paci fj c CW N.Paci fj c CE N.Paci fj c SW N.Paci fj c SE N.Paci fj c

  22. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Wi Winter Precipi pitation n Amoun unt: Ce Central West Nort orth Pacific • Contributes ~7% more to the total precipitation at the LGM • Likely related to shift in storm track • Manabe and Broccoli, 1985

  23. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Ed Eddy Kinetic Energy • Southward shift of the storm tracks at the LGM • Potentially explains the central Pacific moisture increase at the LGM

  24. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Winter Precipi Wi pitation n Amoun unt: Sou Southwest Nort North P Paci cific • Contributes ~4% more to the total precipitation at the LGM • Atmospheric river contribution? • Lora et al. 2017

  25. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Ne Next St Step: H : High R Resolution • Low resolution limited • Significant local variability Wikipedia

  26. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Ne Next St Step: H : High F Frequency cy • Data is lost when averaging over months or years • Need identification tools University of Wisconsin

  27. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Ke Key Challenges • Understanding hydroclimate change in Western US since 21 ka! • Requires high resolution with water isotope tracers and high frequency outputs to perform an “apples to apples” comparison with speleothem records woot.com

  28. NCSA Blue Waters Symposium UConn Physics Colloquium 2/23 Wh Why y it Matters? s? • Help inform proxies and models • Improve understanding of Western US hydroclimate and abrupt climate change Those who do not learn history are doomed to repeat it incorrectly forecast the future! Foster et al. (2014)

  29. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Wh Why y Blue ue Waters? s? • Paleoclimate simulations require a long time to equilibrate • The addition of water isotopes adds ~50% cost • To resolve Western US topography, you need 0.25° resolution

  30. UConn Physics Colloquium 2/23 NCSA Blue Waters Symposium Qu Question ons?

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