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Early onset of significant local warming in low latitude countries

Environmental research letters, 2011-07, Vol.6 (3), p.34009-6

2011

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An observationally based energy balance for the Earth since 1950

Journal of Geophysical Research - Atmospheres, 2009-09, Vol.114 (D17), p.D17107-n/a

2009

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Diverse policy implications for future ozone and surface UV in a changing climate

Environmental research letters, 2016-06, Vol.11 (6), p.64017

2016

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Transport of ice into the stratosphere and the humidification of the stratosphere over the 21st century

Geophysical research letters, 2016-03, Vol.43 (5), p.2323-2329

2016

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CF3CF=CH2 and (Z)-CF3CF=CHF : temperature dependent OH rate coefficients and global warming potentials

Physical chemistry chemical physics : PCCP, 2008-02, Vol.10 (6), p.808-820

2008

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Radiative forcing by well-mixed greenhouse gases: Estimates from climate models in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4)

Journal of Geophysical Research - Atmospheres, 2006-07, Vol.111 (D14), p.D14317-n/a

2006

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Comparison of three vertically resolved ozone data sets: climatology, trends and radiative forcings

Atmospheric chemistry and physics, 2013-06, Vol.13 (11), p.5533-5550

2013

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Stratospheric ozone depletion due to nitrous oxide: influences of other gases

Philosophical transactions of the Royal Society of London. Series B. Biological sciences, 2012-05, Vol.367 (1593), p.1256-1264

2012

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Experimental and Theoretical Study of the Atmospheric Chemistry and Global Warming Potential of SO2F2

The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory, 2008-12, Vol.112 (49), p.12657-12666

2008

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Efficacy of Climate Forcings in PDRMIP Models

Journal of geophysical research. Atmospheres, 2019-12, Vol.124 (23), p.12824-12844

2019

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Identifying weekly cycles in meteorological variables: The importance of an appropriate statistical analysis

Journal of Geophysical Research: Atmospheres, 2012-07, Vol.117 (D13), p.1R-n/a

2012

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A comparison of model‐simulated trends in stratospheric temperatures

Quarterly journal of the Royal Meteorological Society, 2003-04, Vol.129 (590), p.1565-1588

2003

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Variations in ozone depletion potentials of very short-lived substances with season and emission region

Geophysical research letters, 2010-10, Vol.37 (19), p.n/a

2010

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On the role of nitrogen dioxide in the absorption of solar radiation

Journal of Geophysical Research, Washington, DC, 1999-05, Vol.104 (D10), p.12047-12058

1999

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The role of aerosol variations in anthropogenic ozone depletion at northern midlatitudes

Journal of Geophysical Research, Washington, DC, 1996-03, Vol.101 (D3), p.6713-6727

1996

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A vertically resolved, global, gap-free ozone database for assessing or constraining global climate model simulations

Earth system science data, 2013-02, Vol.5 (1), p.31-43

2013

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On the distribution and variability of ozone in the tropical upper troposphere: Implications for tropical deep convection and chemical-dynamical coupling

Geophysical research letters, 2005-12, Vol.32 (23), p.L23813-n/a

2005

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Evidence for a recurring eastern North America upper tropospheric ozone maximum during summer

Journal of Geophysical Research - Atmospheres, 2007-12, Vol.112 (D23), p.D23304-n/a

2007

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Stratospheric ozone destruction: The importance of bromine relative to chlorine

Journal of Geophysical Research, Washington, DC, 1999-10, Vol.104 (D19), p.23871-23880

1999

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Anthropogenic aerosol drives uncertainty in future climate mitigation efforts

Scientific reports, 2019-11, Vol.9 (1), p.16538-8, Article 16538

2019

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Decadal Attribution of Historic Temperature and Ocean Heat Content Change to Anthropogenic Emissions

Geophysical research letters, 2020-02, Vol.47 (3), p.n/a

2020

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Options to accelerate ozone recovery: ozone and climate benefits

Atmospheric chemistry and physics, 2010-08, Vol.10 (16), p.7697-7707

2010

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How Often Does It Rain?

Journal of climate, 2006-03, Vol.19 (6), p.916-934

2006

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Rate Coefficients for the Reactions of OH with CF3CH2CH3 (HFC-263fb), CF3CHFCH2F (HFC-245eb), and CHF2CHFCHF2 (HFC-245ea) between 238 and 375 K

The journal of physical chemistry. A, Molecules, spectroscopy, kinetics, environment, & general theory, 2006-06, Vol.110 (21), p.6724-6731

2006

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Climate forcing due to tropospheric and stratospheric ozone

Journal of Geophysical Research, Washington, DC, 1999-12, Vol.104 (D24), p.31239-31254

1999

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Early onset of significant local warming in low latitude countries

An observationally based energy balance for the Earth since 1950

Diverse policy implications for future ozone and surface UV in a changing climate

Transport of ice into the stratosphere and the humidification of the stratosphere over the 21st century

CF3CF=CH2 and (Z)-CF3CF=CHF : temperature dependent OH rate coefficients and global warming potentials

Radiative forcing by well-mixed greenhouse gases: Estimates from climate models in the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report (AR4)

Comparison of three vertically resolved ozone data sets: climatology, trends and radiative forcings

Stratospheric ozone depletion due to nitrous oxide: influences of other gases

Experimental and Theoretical Study of the Atmospheric Chemistry and Global Warming Potential of SO2F2

Efficacy of Climate Forcings in PDRMIP Models

Identifying weekly cycles in meteorological variables: The importance of an appropriate statistical analysis

A comparison of model‐simulated trends in stratospheric temperatures

Variations in ozone depletion potentials of very short-lived substances with season and emission region

On the role of nitrogen dioxide in the absorption of solar radiation

The role of aerosol variations in anthropogenic ozone depletion at northern midlatitudes

A vertically resolved, global, gap-free ozone database for assessing or constraining global climate model simulations

On the distribution and variability of ozone in the tropical upper troposphere: Implications for tropical deep convection and chemical-dynamical coupling

Evidence for a recurring eastern North America upper tropospheric ozone maximum during summer

Stratospheric ozone destruction: The importance of bromine relative to chlorine

Anthropogenic aerosol drives uncertainty in future climate mitigation efforts

Decadal Attribution of Historic Temperature and Ocean Heat Content Change to Anthropogenic Emissions

Options to accelerate ozone recovery: ozone and climate benefits

How Often Does It Rain?

Rate Coefficients for the Reactions of OH with CF3CH2CH3 (HFC-263fb), CF3CHFCH2F (HFC-245eb), and CHF2CHFCHF2 (HFC-245ea) between 238 and 375 K

Climate forcing due to tropospheric and stratospheric ozone

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