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Academic Journals
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From:Geoscientific Model Development (Vol. 15, Issue 5) Peer-ReviewedThis paper provides initial results from a multi-model ensemble analysis based on the volc-pinatubo-full experiment performed within the Model Intercomparison Project on the climatic response to Volcanic forcing (VolMIP)...
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From:Atmospheric Chemistry and Physics (Vol. 22, Issue 2) Peer-ReviewedUntil now our understanding of the 11-year solar cycle signal (SCS) in stratospheric ozone has been largely based on high-quality but sparse ozone profiles from the Stratospheric Aerosol and Gas Experiment (SAGE) II or...
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From:Earth System Science Data (Vol. 13, Issue 12) Peer-ReviewedHigh-quality stratospheric ozone profile data sets are a key requirement for accurate quantification and attribution of long-term ozone changes. Satellite instruments provide stratospheric ozone profile measurements over...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 20) Peer-ReviewedThe NCAR Whole Atmosphere Community Climate Model with thermosphere and ionosphere eXtension (WACCM-X) v2.1 has been extended to include the neutral and ion-molecule chemistry and dynamics of three metals (Mg, Na, and...
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From:Atmospheric Chemistry and Physics (Vol. 21, Issue 18) Peer-ReviewedSevere vortex-wide ozone loss in the Arctic would expose both ecosystems and several millions of people to unhealthy ultraviolet radiation. Adding to these worries, and extreme events as the harbingers of climate change,...
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From:Geoscientific Model Development (Vol. 12, Issue 10) Peer-Reviewed
We present a Lagrangian convective transport scheme developed for global chemistry and transport models, which considers the variable residence time that an air parcel spends in convection. This is particularly...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 6) Peer-ReviewedWe provide an overview of the REF-C1SD specified-dynamics experiment that was conducted as part of phase 1 of the Chemistry-Climate Model Initiative (CCMI). The REF-C1SD experiment, which consisted of mainly nudged...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 14) Peer-ReviewedVarious observation-based datasets have confirmed positive zonal mean column ozone trends at midlatitudes as a result of the successful implementation of the Montreal Protocol. However, there is still uncertainty about...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 1) Peer-Reviewed
Stratospheric ozone loss inside the Arctic polar vortex for the winters between 2004-2005 and 2012-2013 has been quantified using measurements from the space-borne Atmospheric Chemistry Experiment Fourier Transform...
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From:Atmospheric Chemistry and Physics (Vol. 20, Issue 21) Peer-ReviewedAccurate simulation of atmospheric circulation, particularly in the lower stratosphere, is challenging due to unresolved wave-mean flow interactions and limited high-resolution observations for validation....
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From:Atmospheric Chemistry and Physics (Vol. 18, Issue 20) Peer-Reviewed
Meteoric ablation produces layers of metal atoms in the mesosphere and lower thermosphere (MLT). It has been known for more than 30 years that the Ca atom layer is depleted by over 2 orders of magnitude compared with...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 6) Peer-ReviewedByline: Tao Yuan, Wuhu Feng, John M. C. Plane, Daniel R. Marsh To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
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From:Geoscientific Model Development (Vol. 11, Issue 8) Peer-Reviewed
This paper presents the first results of an age-of-air (AoA) inter-comparison of six global transport models. Following a protocol, three global circulation models and three chemistry transport models simulated five...
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From:Atmospheric Chemistry and Physics (Vol. 19, Issue 2) Peer-Reviewed
Despite the recently reported beginning of a recovery in global stratospheric ozone (O.sub.3 ), an unexpected O.sub.3 decline in the tropical mid-stratosphere (around 30-35 km altitude) was observed in...
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From:Atmospheric Chemistry and Physics (Vol. 18, Issue 24) Peer-Reviewed
The atmospheric methane (CH.sub.4) growth rate has varied considerably in recent decades. Unexplained renewed growth after 2006 followed 7 years of stagnation and coincided with an isotopic trend toward CH.sub.4 more...
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From:Geoscientific Model Development (Vol. 10, Issue 8) Peer-ReviewedThis paper documents the tropospheric chemical mechanism scheme used in the TOMCAT 3-D chemical transport model. The current scheme includes a more detailed representation of hydrocarbon chemistry than previously...