Equilibrium Response of an Atmosphere–Mixed Layer Ocean Model to Different Radiative Forcing Agents: Global and Zonal Mean Response

By M. Yoshimori, A. Broccoli. 2008

145 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/6a5ace6a1d2007ba4edcdf0af9061ceeebebcf69

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. M. Zelinka
2. K. Armour
3. G. Roe
4. D. Hartmann
5. C. Bitz
6. Tobias Bischoff
7. Gabriele C. Hegerl
8. A. Friedman

In Global and Planetary Change

1. M. Zelinka
2. D. Hartmann
3. G. Roe
4. K. Armour
5. Tobias Bischoff
6. C. Bitz
7. Gabriele C. Hegerl
8. A. Friedman

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): “Yoshimori and Broccoli (2008) have recently emphasized how aerosol cooling, concentrated in the Northern Hemisphere, shifts the ITCZ southward.”
• Time-Varying Climate Sensitivity from Regional Feedbacks (2012, background): “(2010) have proposed an alternative interpretation of Teff in terms of a timedependent ‘‘efficacy of ocean heat uptake’’ that arises due to its geographic structure, analogous to the distinct efficacies of different radiative forcing agents (Hansen et al. 1997, 2005; Yoshimori and Broccoli 2008).”
• The effect of volcanic eruptions on global precipitation (2013, background): “Since volcanic forcing causes a greater reduction in temperature in the summer hemisphere relative to the winter one, the ITCZ should not migrate as far poleward as it normally would [Schneider et al., 2009; Yoshimori and Broccoli, 2008; G. Stenchikov, personal communication, 2012].”
• Climate Feedbacks and Their Implications for Poleward Energy Flux Changes in a Warming Climate (2011, background): “This point was emphasized by Fletcher et al. (2009) in the response of atmospheric circulation to snow albedo feedback on NH land as well as by Chiang and Bitz (2005), Yoshimori and Broccoli (2008), Kang et al. (2008), and Kang et al. (2009) in the movement of the ITCZ due to extratopical forcings.”
• Extratropical Cooling, Interhemispheric Thermal Gradients, and Tropical Climate Change (2012, result): “Subsequent studies by Yoshimori & Broccoli (2008, 2009) lent support to this view: They showed in AGCM–slab ocean simulations with imposed twentieth-century external radiative forcings that the interhemispheric gradient in radiative forcing was a better predictor for the tropical Hadley cell…”
• Energetic Constraints on the Position of the Intertropical Convergence Zone (2013, background): “…variations caused by the Atlantic meridional overturning circulation, can lead to shifts of the ITCZ, generally away from a cooling and toward a warming hemisphere (e.g., Vellinga and Wood 2002; Chiang et al. 2003; Chiang and Bitz 2005; Broccoli et al. 2006; Yoshimori and Broccoli 2008).”