O'Gorman, Paul - Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology (MIT)

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O'Gorman, Paul - Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology (MIT)

Moist Convection and the Thermal Stratification of the Extratropical Troposphere TAPIO SCHNEIDER AND PAUL A. O'GORMAN
Observational data for studies of the General Circulation Overall global coverage (both over land and ocean)
Water vapor and the hydrological cycle -60 -30 0 30 60
12.812: Problem set 1 1. Vertical coordinate systems: A range of different vertical coordinates are used in analysis
Energy of Midlatitude Transient Eddies in Idealized Simulations of Changed Climates PAUL A. O'GORMAN* AND TAPIO SCHNEIDER
Relative humidity changes in a warmer climate Steven C. Sherwood,1,2
The velocity-scalar cross spectrum of stretched spiral vortices P. A. O'Gormana)
12.812: Problem set 4 1. Available potential energy
Generated using V3.0 of the official AMS LATEX template The relative humidity in an isentropic advection-condensation model: Limited poleward
The Hydrological Cycle over a Wide Range of Climates Simulated with an Idealized GCM
12.312: Understand and run your own climate model Instructor: Paul O'Gorman
Weather-Layer Dynamics of Baroclinic Eddies and Multiple Jets in an Idealized General Circulation Model
Precipitation and its extremes in changed climates T. Schneider and P. A. O'Gorman
12.812: Problem set 2 1. Zonal asymmetry of the mean relative humidity field
Supporting Information O'Gorman and Schneider 10.1073/pnas.0907610106
Understanding the varied response of the extratropical storm tracks to climate change
IOP PUBLISHING ENVIRONMENTAL RESEARCH LETTERS Environ. Res. Lett. 5 (2010) 025207 (7pp) doi:10.1088/1748-9326/5/2/025207
A Climatology of Tropospheric Zonal-Mean Water Vapor Fields and Fluxes in Isentropic Coordinates
The physical basis for increases in precipitation extremes in simulations of 21st-century
The Effective Static Stability Experienced by Eddies in a Moist Atmosphere PAUL A. O'GORMAN
Supporting Information O'Gorman10.1073/pnas.1011547107
WATER VAPOR AND THE DYNAMICS OF CLIMATE CHANGES
Scaling of Precipitation Extremes over a Wide Range of Climates Simulated with an Idealized GCM
Recovery of atmospheric flow statistics in a general circulation model without nonlinear eddy-eddy interactions
Stochastic Models for the Kinematics of Moisture Transport and Condensation in Homogeneous Turbulent Flows
Appendices to "Effect of Schmidt number on the velocityscalar cospectrum in isotropic turbulence
12.812: The general circulation of the atmosphere and climate change Instructor: Paul O'Gorman
The general circulation: historical perspective During the past three centuries, the prevailing ideas about
Section 3: Mean state and variability of the atmosphere Develop intuition and familiarity with current state
Circulation (Peixoto and Oort, fig 7.1a)
(Peixoto and Oort, fig 13.3: Kinetic energy is order 150 J/kg)
12.812: Problem set 3 1. Contributions to the poleward energy flux
Surveys in Geophysics manuscript No. (will be inserted by the editor)
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE1169
Annular modes Thompson and Wallace, J. Climate, 2000
PUBLISHED ONLINE: 24 JULY 2011 | DOI: 10.1038/NCLIMATE1169 An energetic perspective on the regional response