A Gray-Radiation Aquaplanet Moist GCM. Part II: Energy Transports in Altered Climates

By D. Frierson, I. Held, P. Zurita‐Gotor. 2007

141 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/0a6f19e2eb8139855375decf11d66b77d9e4a4c6

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Gang Chen
2. Jian Lu
3. D. Frierson
4. G. Rivière
5. Tapio Schneider
6. M. Byrne
7. Tobias Bischoff

In Global and Planetary Change

1. Gang Chen
2. Jian Lu
3. D. Frierson
4. G. Rivière
5. Tapio Schneider
6. M. Byrne
7. Tobias Bischoff

In Oceanography

1. Jian Lu
2. Gang Chen
3. D. Frierson

Citations in the corpus

• The Tropical Response to Extratropical Thermal Forcing in an Idealized GCM: The Importance of Radiative Feedbacks and Convective Parameterization (2009, unknown): “As in Frierson et al. (2007), we take m to be the moist static energy just above the surface, which can be written as where T s is the surface temperature, q * s is the saturation specific humidity at the surface, h s is the surface relative humidity (fixed as 76%), and e * s is the saturation vapor…”
• The Dynamics of Idealized Convection Schemes and Their Effect on the Zonally Averaged Tropical Circulation (2007, methodology): “In Frierson et al. (2006, 2007), we used large-scale condensation (LSC) only as the convection scheme.”
• Width of the Hadley cell in simple and comprehensive general circulation models (2007, background): “Idealized moist simulations also show a poleward shift of the storm tracks with increased moisture content [ Frierson et al., 2006, 2007 ], but it is clear in these simulations that the subtropical jet can separate quite far GEOPHYSICAL RESEARCH LETTERS, VOL.”
• Phase Speed Spectra and the Latitude of Surface Westerlies: Interannual Variability and Global Warming Trend (2008, background): “…jet moves poleward with anomalous westerlies in the subtropics, analogous to the separation of the eddy-driven jet from the subtropical jet in idealized models, as the equator-to-pole temperature gradients or water vapor contents are altered (e.g., Son and Lee 2005; Frierson et al. 2006, 2007a).”