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2. The Importance of the Montreal Protocol in Mitigating the Potential Intensity of Tropical Cyclones
3. Airmass Origin in the Arctic. Part I: Seasonality
4. CMIP5 Projections of Arctic Amplification, of the North American/North Atlantic Circulation, and of Their Relationship
5. Contrasting short and long term projections of the hydrological cycle in the Southern extratropics
6. Drivers of the Recent Tropical Expansion in the Southern Hemisphere: Changing SSTs or Ozone Depletion?
7. On the surface impact of Arctic stratospheric ozone extremes
8. The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM)
9. Biases in Southern Hemisphere climate trends induced by coarsely specifying the temporal resolution of stratospheric ozone
10. Delayed Southern Hemisphere Climate Change Induced by Stratospheric Ozone Recovery, as Projected by the CMIP5 Models
11. Distinguishing the impacts of ozone-depleting substances and well-mixed greenhouse gases on Arctic stratospheric ozone and temperature trends
12. Impact of the Tropopause Temperature on the Intensity of Tropical Cyclones: An Idealized Study Using a Mesoscale Model
13. Influence of projected Arctic sea ice loss on polar stratospheric ozone and circulation in spring
14. Is climate sensitivity related to dynamical sensitivity? A Southern Hemisphere perspective
15. Seasonal Ventilation of the Stratosphere: Robust Diagnostics from One-Way Flux Distributions
16. Separating the stratospheric and tropospheric pathways of El Niño–Southern Oscillation teleconnections
17. Southern Hemisphere Cloud–Dynamics Biases in CMIP5 Models and Their Implications for Climate Projections
18. The response midlatitude jets to increased CO2: Distinguishing the roles of sea surface temperature and direct radiative forcing
19. The Specified Chemistry Whole Atmosphere Community Climate Model (SC-WACCM)
20. The surface impacts of Arctic stratospheric ozone anomalies
21. Air-Mass Origin as a Diagnostic of Tropospheric Transport
22. Are Recent Arctic Ozone Losses Caused by Increasing Greenhouse Gases?
23.
Can Natural Variability Explain Observed Antarctic Sea Ice Trends?
New Modeling Evidence from CMIP5
24. Can natural variability explain observed Antarctic sea ice trends? New modeling evidence from CMIP5
25. Changes in the frequency and return level of high ozone pollution events over the eastern United States following emission controls
26. Climate Change from 1850 to 2005 Simulated in CESM1(WACCM)
27. Delayed Southern Hemisphere Climate Change Induced by Stratospheric Ozone Recovery, as Projected by the CMIP5 Models
28.
Lifetime Dependent Flux into the Lowermost Stratosphere for Idealized
Trace Gases of Surface Origin
29.
Modeling Evidence that Ozone Depletion Has Impacted Extreme
Precipitation in the Austral Summer
30.
On the Lack of Stratospheric Dynamical Variability in Low-Top
Versions of the CMIP5 Models
31. Response of the Midlatitude Jets, and of Their Variability, to Increased Greenhouse Gases in the CMIP5 Models
32. Stratospheric ozone depletion: a key driver of recent precipitation trends in South Eastern South America
33. The Antarctic Atmospheric Energy Budget. Part I: Climatology and Intraseasonal-to-Interannual Variability
34. The Antarctic Atmospheric Energy Budget. Part II: The Effect of Ozone Depletion and its Projected Recovery
35. The Importance of the Montreal Protocol in Protecting Earth’s Hydroclimate
36. The ozone hole indirect effect: Cloud-radiative anomalies accompanying the poleward shift of the eddy-driven jet in the Southern Hemisphere
37. The Ozone Hole Indirect Effect: Cloud-Radiative Anomalies Accompanying the Poleward Shift of the Eddy-Driven Jet in the Southern Hemisphere
38. The Response of Extratropical Cyclones in the Southern Hemisphere to Stratospheric Ozone Depletion in the 20th Century
39. Uncertainty in Climate Change Projections of the Hadley Circulation: The Role of Internal Variability
40. Understanding Hadley Cell Expansion versus Contraction: Insights from Simplified Models and Implications for Recent Observations
41. Abrupt Circulation Responses to Tropical Upper-Tropospheric Warming in a Relatively Simple Stratosphere-Resolving AGCM
42. Antarctic Climate Response to Stratospheric Ozone Depletion in a Fine Resolution Ocean Climate Model
43. Antarctic Ozone Depletion and Trends in Tropopause Rossby Wave Breaking
44. Assessing and Understanding the Impact of Stratospheric Dynamics and Variability on the Earth System
45. Comment on "Tropospheric temperature response to stratospheric ozone recovery in the 21st century" by Hu et al. (2011)
46. Flux Distributions as Robust Diagnostics of Stratosphere-Troposphere Exchange
47. Mitigation of 21st Century Antarctic Sea Ice Loss by Stratospheric Ozone Recovery
48.
The Signature of Ozone Depletion on Tropical Temperature Trends,
as Revealed by Their Seasonal Cycle in Model Integrations with Single
Forcings
49. Why Might Stratospheric Sudden Warmings Occur with Similar Frequency in El Niño and La Niña Winters?
50. Double Tropopause Formation in Idealized Baroclinic Life Cycles: The Key Role of an Initial Tropopause Inversion Layer
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