A11P:
Atmospheric Circulations and Their Role in the Hydrological Cycle: Monsoons, Storm Tracks, and the ITCZ I


Session ID#: 10980

Session Description:
The transport of water vapor by atmospheric circulations determines the global spatiotemporal pattern of precipitation. Latent heat release during condensation of water vapor in turn feeds back on the strength of atmospheric circulations. This coupled problem needs to be addressed in order to understand what determines spatial patterns of precipitation, the strength of atmospheric circulations, and how these quantities change with climate change. We invite presentations focusing on the physical mechanisms linking atmospheric circulations and the hydrological cycle, where the phenomena of interest could be (but are not limited to) the Hadley and Walker circulations, monsoons, synoptic or stationary eddies, or the ITCZ.
Primary Convener:  Robert Jnglin Wills, University of Washington, Seattle, WA, United States; ETH Swiss Federal Institute of Technology Zurich, Zurich, Switzerland
Conveners:  Sarah M Kang, Ulsan National Institute of Science and Technology, Ulsan, Korea, Republic of (South), Isla Simpson, National Center for Atmospheric Research, Climate and Global Dynamics Laboratory, Boulder, CO, United States and Jian Lu, Pacific Northwest National Laboratory, Richland, WA, United States
Chairs:  Isla Simpson, National Center for Atmospheric Research, Climate and Global Dynamics Laboratory, Boulder, CO, United States, Angeline G Pendergrass, Cornell University, Earth and Atmospheric Sciences, Ithaca, NY, United States and Hansi Alice Singh, University of Washington Seattle Campus, Seattle, United States
OSPA Liaison:  Robert Jnglin Wills, University of Washington, Seattle, WA, United States

Cross-Listed:
  • GC - Global Environmental Change
Index Terms:

3305 Climate change and variability [ATMOSPHERIC PROCESSES]
3319 General circulation [ATMOSPHERIC PROCESSES]
3354 Precipitation [ATMOSPHERIC PROCESSES]
3373 Tropical dynamics [ATMOSPHERIC PROCESSES]

Abstracts Submitted to this Session:

Simona Bordoni, University of Trento, Trento, Italy and Jinqiang Chen, California Institute of Technology, Pasadena, CA, United States
Xavier J Levine, Yale University, New Haven, CT, United States and William R Boos, University of California Berkeley, Department of Earth and Planetary Science, Berkeley, CA, United States
Tiffany Shaw, The University of Chicago, Chicago, IL, United States; The University of Chicago, Department of the Geophysical Sciences, Chicago, United States and Aiko Voigt, Lamont-Doherty Earth Observatory, Columbia University, New York, United States
Sean Faulk, University of California Los Angeles, Los Angeles, CA, United States, Jonathan Mitchell, University of California Los Angeles, Department of Atmospheric & Oceanic Sciences; Department of Earth, Planetary & Space Sciences, Los Angeles, CA, United States and Simona Bordoni, University of Trento, Trento, Italy
Bryce E Harrop, Pacific Northwest National Laboratory, Atmospheric Sciences and Global Change Division, Richland, United States and Dennis L. Hartmann, University of Washington, Department of Atmospheric Sciences, Seattle, WA, United States
Da Yang, University of California Berkeley, Berkeley, United States
Norman G Loeb1, Hailan Wang2, Anning Cheng3, Seiji Kato4, John Fasullo5, Kuan-Man Xu1 and Richard P Allan6, (1)NASA Langley Research Center, Hampton, VA, United States, (2)Science Systems and Applications, Inc. Hampton, Hampton, VA, United States, (3)IMSG at NOAA/NWS/NCEP/EMC, College Park, MD, United States, (4)NASA Langley Research Ctr, Hampton, United States, (5)National Center for Atmospheric Research, Climate and Global Dynamics Laboratory, Boulder, CO, United States, (6)University of Reading, Reading, United Kingdom