Mechanisms of decadal SST variability
Collaborators: Dennis Hartmann, David Battisti, Kyle Armour, Mike Wallace (University of Washington)
Unforced climate variability on decadal and longer time scales has garnered
much attention, both because of its potential predictability and because it often masks the influence of externally forced climate change. My work focuses on identifying patterns of sea-surface temperature (SST) variability that are associated with low-frequency variability in the Pacific and the Atlantic. I am interested in the mechanisms governing this variability, particularly the relative role of air-sea fluxes of heat and momentum on the dynamics of the subpolar ocean gyres and the impact of extratropical heat flux anomalies on the atmospheric circulation. The goal of this work is to develop a simple model for the response of the subpolar ocean gyres to atmospheric forcing and use it to make long-term regional climate projections.
Wills, R.C., T. Schneider, J.M. Wallace, D.S. Battisti, and D.L. Hartmann, 2018: Disentangling global warming, multidecadal variability, and El Niño in Pacific temperatures. Geophysical Research Letters, 45, doi:10.1002/2017GL076327. [PDF] [SI] [Official version] [Code] [Science Editor's Note] [PCC Research Highlight]
Wills, R.C., D.S. Battisti, D.L. Hartmann, and T. Schneider, 2017: Extracting modes of variability and change from climate model ensembles. Proceedings of the 7th International Workshop on Climate Informatics: CI 2017, V. Lyubchich, N.C. Oza, A. Rhines, and E. Szekely, Eds., NCAR Technical Note NCAR/TN-536+PROC, 25-28. [PDF] [Official version]
Wills, R.C.J., K.C. Armour, D.S. Battisti, and D.L. Hartmann, 2018: Ocean-atmosphere dynamical coupling fundamental to the Atlantic Multidecadal Oscillation. Submitted January 2018.
Wills, R.C.J., D.S. Battisti, D.L. Hartmann and T. Schneider: Constraining externally forced climate change from small ensembles and individual realizations, in preparation.
Zonal variation of P - E
Collaborators: Tapio Schneider (Caltech), Michael Byrne (ETH Zurich)
Atmospheric circulations transport water that is evaporated in one region and deposit it as precipitation in another. In the zonal mean, the Hadley cell and synoptic eddies transport water from the dry evaporative regions of the subtropics to regions of high precipitation in the Intertropical Convergence Zone and extratropical storm track. Variations about this zonal mean are responsible for, for example, the relative wetness of Southeast Asia and the eastern US and the relative dryness of central Asia. I am interested in how stationary eddy circulations lead to these spatial patterns in net precipitation through there influence on vertical motion in the lower troposphere and how changes in stationary-eddy circulations influence the response of the hydrological cycle to global warming.
Wills, R.C. and T. Schneider, 2015: Stationary eddies and the zonal asymmetry of net precipitation and ocean freshwater forcing. Journal of Climate, 28, 5115-5133. Corrigendum. Journal of Climate, 30, 8841-8842. [PDF] [Official version] [Corrigendum]
Wills, R.C. and T. Schneider, 2016: How stationary eddies shape changes in the hydrological cycle: Zonally asymmetric experiments in an idealized GCM. Journal of Climate, 29, 3161-3179. [PDF] [Official version]
Wills, R.C., M.P. Byrne, and T. Schneider, 2016: Thermodynamic and dynamic controls on changes in the zonally anomalous hydrological cycle. Geophysical Research Letters, 43, doi:10.1002/2016GL068418. [PDF] [SI] [Official version] [EOS Spotlight]
Wills, R., 2016: Stationary Eddies and Zonal Variations of the Global Hydrological Cycle in a
Changing Climate. Ph.D. Thesis, California Institute of Technology. (see chapters 2-4) [PDF]
Stationary eddy changes with warming
Collaborators: Tapio Schneider (Caltech), Xavier Levine (Yale)
Partly motivated by their importance for the zonal variation of P - E, I would like to know how the amplitude of stationary eddies changes with climate change. To begin to answer this question, I have sets of experiments in an idealized GCM, where stationary eddies are forced by a large-scale Gaussian mountain or an equatorial ocean heat flux convergence. The stationary eddies from these two sources respond differently to climate changes in this idealized model.
In the Gaussian mountain case, the response depends on the zonal wind hitting the mountain, the latent heating in the orographic flow, and the top-of-mountain surface pressure and thus can behave in a number of different ways depending on the latitude of the mountain.
In the equatorial heating case, stationary waves in midlatitudes are driven by a Walker circulation along the equator. The strength of this Walker circulation can be constrained with energetic arguments focused on the net column energy input and the gross moist stability, an effective static stability for tropical circulations.
Wills, R.C.J. and T. Schneider, 2018: Mechanisms setting the strength of orographic Rossby waves across a wide range of climates in a moist idealized GCM. Journal of Climate, Revised March 2018. [PDF]
Wills, R.C., X.J. Levine, and T. Schneider, 2017: Local energetic constraints on Walker circulation strength. Journal of the Atmospheric Sciences, 74, 1907-1922. [PDF] [Official version]
Wills, R.C., 2016: Stationary Eddies and Zonal Variations of the Global Hydrological Cycle in a
Changing Climate. Ph.D. Thesis, California Institute of Technology. (see chapters 5-6) [PDF]
Atmospheric influences on the ocean at the Last Glacial Maximum
Collaborators: James Rae (St Andrews), William Gray (St. Andrews), Ian Eisenman (SCRIPPS)
Stationary eddy circulations were substatially altered during the Last Glacial Maximum, when large continental-scale ice sheets covered North America and Europe, providing additional stationary-wave forcing. The surface winds, surface heat fluxes, and net precipitation associated with the stationary waves provide forcing to the Northern Hemisphere oceans. We would like to understand how stationary wave and ocean circulation differences simulated by models fit with sediment core based proxies of temperature, ocean convection, and surface nutrient availability. Changes in the ocean circulation associated with this stationary wave forcing could have implications for the release of CO2 from the deep ocean, an important driver of glacial cycles.
Wills, R.C.J., J.W.B. Rae, W.R. Gray, I. Eisenman, and D.S. Battisti: Wind shifts drive an intensified North Pacific ocean circulation at the Last Glacial Maximum, in preparation.
Rae, J.W.B., R.C. Wills, I. Eisenman, W. Gray, and B. Taylor: Overturning circulation, nutrient limitation, and warming in the Glacial North Pacific, in preparation.
Gray, W.R., J.W.B. Rae, R.C.J. Wills, A.E. Shevenell, G.L. Foster, C.H. Lear, and B. Taylor, 2018: Deglacial upwelling, productivity and CO2 outgassing in the North Pacific Ocean. Nature Geoscience, in press. [Official version] [News and Views]