A stratospheric ozone profile data set for 1979–2005: Variability, trends, and comparisons with column ozone data

By William J. Randel, Fei Wu. 2007

284 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/ed78bdfb36720789e855672a8e625db5818acb0c

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Citations in the corpus

SOLAR INFLUENCES ON CLIMATE (2010, unknown): “Rind, P. Lonergan and D. Shindell (1999), Effects of solar cycle variability on the lower stratosphere and the troposphere.”
Stratospheric variability and tropospheric ozone (2009, methodology): “[2] Scientific efforts to understand the trends and variations in ozone observed over the past few decades have demonstrated the role of both photochemical and meteorological factors in driving stratospheric ozone change [e.g., Randel and Wu, 2007; Stolarski et al., 2006; Salawitch et al., 2005].”
A Robust Mechanism for Strengthening of the Brewer–Dobson Circulation in Response to Climate Change: Critical-Layer Control of Subtropical Wave Breaking (2011, background): “…appears to be consistent with the vertical profile of observed ozone trends from the Stratospheric Aerosol and Gas Experiment (SAGE) over 1979–2005 (Randel and Wu 2007), although it must be noted that the vertically integrated SAGE trends in the tropics are inconsistent with the column ozone…”
Simulation of secular trends in the middle atmosphere, 1950–2003 (2007, methodology): “06 data mapped with Salby’s [1982] asynoptic Fourier transform technique for 1–19 July 2002 (52!S to 83!N) and for 19 July to 8 August 2005 (83!S to 54!S).”
Dynamics, stratospheric ozone, and climate change (2008, background): “However, since 1979 the stratospheric ozone column in the tropics has declined by about 7–8 DU, or about 3% (Randel and Wu, 2007), a value which is consistent with the CMAM total ozone decline shown in Fig.”
Anthropogenic and Natural Radiative Forcing (2014, methodology): “WMO (2011) assessed the RF from 1979 to 2005 from observed ozone changes (Randel and Wu, 2007) and results from 16 models for the 1970s average to 2004.”
The dynamical core, physical parameterizations, and basic simulation characteristics of the atmospheric component AM3 of the GFDL global coupled model CM3 (2011, methodology): “Stratospheric ozone concentrations in AM2 were prescribed following Randel and Wu (1999).”