Session Large-Scale Atmospheric Dynamics and Climate: Jet Streams, Storm Tracks, Stationary Waves, and Monsoons


Description:

The large-scale atmospheric circulation redistributes heat, moisture, and atmospheric tracers around the globe, playing a key role in shaping regional climate and climate change. The large-scale circulation is in turn shaped by the interactions of large-scale dynamics with the global energy budget and hydrological cycle and with smaller scale processes such as mesoscale motions and cloud processes. Disentangling the many processes that shape the large-scale circulation and its response to climate change requires a combination of conceptual understanding, hierarchical modeling, and observations. 

 

We welcome observational, modeling, and theoretical studies on the dynamics of large-scale atmospheric circulations such as the jet streams, storm tracks (including blocking and atmospheric rivers), stationary waves, monsoons, and tropical overturning circulations. Contributions on the response of these circulations to climate change are particularly encouraged


Papers:
Dynamical importance of the trade wind inversion in suppressing the southeast Pacific ITCZ
Alex Omar Gonzalez, WHOI, Woods Hole, MA; and I. Ganguly, M. Osterloh, G. Cesana, and C. A. DeMott

Coupling between Hadley Circulation Strength Variability and Wind-stress-driven Ocean Circulation is Hemisphere Dependent
Mahdi Hasan, North Carolina State Univ., Raleigh, NC; and S. Larson, K. McMonigal, W. A. Robinson, and A. Aiyyer

Storm Track Response to Uniform Global Warming Downstream of an Idealized Sea Surface Temperature Front
Sebastian Schemm, ETH, Zurich, ZH, Switzerland; ETH, Zurich, Switzerland

The Role of Topography in Shaping Southeast US Winter Precipitation
Benjamin O Johnson, Princeton University, Princeton, NJ; and T. L. Delworth

Insights on the North American Monsoon from Climate Simulations with Altered Topography
Benjamin O Johnson, Princeton University, Princeton, NJ; and T. L. Delworth

Seasonal Prediction of Wintertime North Pacific Blocking: What Are We Capturing and Missing?
Mingyu Park, NOAA/GFDL, Princeton, NJ; Princeton University, Princeton, NJ; and N. Johnson

Accurate Column Moist Static Energy Budget in GISS ModelE3
Kuniaki Inoue, CCSR, New York, NY; NASA Goddard Institute for Space Studies, New York, NY; and M. Kelley, A. Fridlind, M. Biasutti, and G. S. Elsaesser

Uniform Warming of Sea Surface Temperatures explain Blocking Reduction in Warming Simulations, but Pattern Changes are Important too
Veeshan T Narinesingh, Princeton University, Princeton, NJ; and H. Guo, S. Garner, and Y. Ming

Atmospheric blocking characteristics in two storm-resolving GCMs
Edgar Dolores Tesillos, Institute of Geography, Oeschger Centre for Climate Change Research, Bern, BE, Switzerland; and O. Martius

Nonlinearity of Atmospheric Circulation response to increased CO2
Darryn W. Waugh, Johns Hopkins University, Baltimore, MD; and X. Zhang, C. Orbe, I. Mitevski, and L. M. Polvani

Calendar Year Climatology of Northern Hemisphere Tropopause-level Jets
Libby Orr, University of Wisconsin - Madison, Madison, WI; and J. E. Martin

Classification of Tropics based on the Spatio-temporal Dynamics of the Intertropical Convergence Zone from a Complex Networks Perspective
Gaurav Chopra, Indian Institute of Technology Madras, Chennai, Tamil Nadu, India; Indian Institute of Technology Madras, Chennai, Tamil Nadu, India; and V. R. Unni, P. Venkateshan, S. M. Vallejo-Bernal, N. Marwan, J. Kurths, and R. I. Sujith

Exploring Stratospheric Mixing using Lagrangian Coherent Structures
Jezabel Curbelo, Universitat Politècnica de Catalunya, Barcelona, Spain; and M. Linz

The influence of SST on Walker circulation strength
Margaret L. Duffy, NCAR, Boulder, CO; and L. Back and P. A. O'Gorman

Submission Deadline: Thursday, 31 August 2023