The dynamic range of poleward energy transport in an atmospheric general circulation model

By R. Caballero, P. Langen. 2005

134 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/6d6ecfe53d827a2de89d3c89536b997b984b0378

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. Tapio Schneider
2. D. Frierson
3. Jian Lu
4. Gang Chen
5. Tobias Bischoff
6. P. Zurita‐Gotor
7. I. Held
8. P. Langen

In Global and Planetary Change

1. Tapio Schneider
2. D. Frierson
3. Jian Lu
4. Gang Chen
5. Tobias Bischoff
6. P. Zurita‐Gotor
7. I. Held
8. P. Langen

In Oceanography

1. D. Frierson
2. Tapio Schneider
3. Tobias Bischoff
4. Jian Lu
5. Gang Chen
6. I. Held
7. P. O’Gorman
8. Kerry A. Emanuel

Citations in the corpus

• Subtropical Arctic Ocean temperatures during the Palaeocene/Eocene thermal maximum (2006, unknown): “Similarly, atmospheric general circulation models do not support strong enough positive feedbacks in atmospheric heat transport 30 .”
• Energetic Constraints on the Position of the Intertropical Convergence Zone (2013, methodology): “For the eddy flux of specific humidity q (or latent energy Lyq), we use a scaling in terms of the meridional gradient of specific humidity along (dry) isentropes near the surface hy0q0i} ye›yqju (Caballero and Langen 2005; O’Gorman and Schneider 2008; Pierrehumbert 2002; Caballero andHanley 2012).”
• Width of the Hadley cell in simple and comprehensive general circulation models (2007, methodology): “[11] The full GCM simulations in this paper are the same simulations originally used to study poleward heat transports in the study of Caballero and Langen [2005] .”
• Polar amplification of surface warming on an aquaplanet in “ghost forcing” experiments without sea ice feedbacks (2005, background): “Caballero and Langen (2005) have, however, demonstrated that the heat transport may saturate in warmer, low-gradient climates.”
• A Gray-Radiation Aquaplanet Moist GCM. Part II: Energy Transports in Altered Climates (2007, background): “A robust poleward shift of the midlatitude storm track with increased temperature/moisture content has been seen in global warming simulations (Yin 2005), and with a full GCM over idealized boundary conditions (Cabellero and Langen 2005).”