Tropopause height and zonal wind response to global warming in the IPCC scenario integrations

By D. Lorenz, Eric DeWeaver. 2007

453 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/d5dec7a008fd6716e178afe38f6ffadf3168332f

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. T. G. Shepherd
2. William J. Randel
3. A. Butler
4. T. Birner
5. L. Polvani
6. Gang Chen
7. D. Frierson
8. M. Hegglin

In Global and Planetary Change

1. T. G. Shepherd
2. A. Butler
3. William J. Randel
4. T. Birner
5. L. Polvani
6. Gang Chen
7. D. Frierson
8. T. Woollings

Citations in the corpus

• Expansion of the Hadley Cell under Global Warming: Winter versus Summer (2012, unknown): “…the extratropical sources of change that are shown by a number of recent studies to affect the HC edge trend such as the rise of tropo-pause (Lorenz and DeWeaver 2007), increase of mid-latitude eddy phase speed (Chen et al. 2008; Lu et al. 2008), upper-level midlatitude baroclinicity (Rivi…”
• The Steady-State Atmospheric Circulation Response to Climate Change–like Thermal Forcings in a Simple General Circulation Model (2010, background): “Lorenz and DeWeaver (2007) considered the effect of anthropogenically induced changes in tropopause height on the extratropical circulation.”
• A Diagnosis of the Seasonally and Longitudinally Varying Midlatitude Circulation Response to Global Warming (2014, methodology): “This produces similar features to Lorenz and DeWeaver (2007)’s analysis of the CMIP3 models (see their Fig.”
• Response of the large‐scale structure of the atmosphere to global warming (2015, background): “(2010), and other plausible arguments may be made. Thus, Chen and Held (2007) and Chen et al.”
• Width of the Hadley cell in simple and comprehensive general circulation models (2007, background): “Such a scaling produces qualitatively similar results to those presented in Figure 2. It is additionally important to recognize that when comparing with such a simple scaling, other physical effects, such as changes in phase speed spectra (Chen and Held, submitted manuscript, 2007), tropopause heigh”
• Persistent Extratropical Regimes and Climate Extremes (2015, background): “This is seen in a hierarchy of models from dry dynamical cores [53, 54] through more realistic atmo-”
• Future climate change in the Southern Hemisphere: Competing effects of ozone and greenhouse gases (2011, result): “This contrasts with the results of Lorenz and DeWeaver [2007], who found a significant intermodel correlation between this region and changes in the 850 hPa zonal wind (a measure of the SAM).”
• THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE (2011, background): “Changes in ExTL tracer gradients may affect tropopause height, and changes in tropopause height may alter tropospheric circulations [ Lorenz and DeWeaver , 2007].”
• Ozone hole and Southern Hemisphere climate change (2009, unknown): “Idealized models have shown that lowering the tropopause pressure, e.g., owing to stratospheric cooling, robustly induces a poleward shift in midlatitude jet [ Polvani and Kushner , 2002; Lorenz and DeWeaver , 2007].”