Stratospheric ozone in 3-D models : A simple chemistry and the cross-tropopause flux

By C. McLinden, S. Olsen, B. Hannegan, O. Wild, Michael J. Prather, J. Sundet. 2000

536 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/5d64a9952571687367be5fb298c4e0c667fe5de1

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. Robert J. D. Spurr
2. Randall V. Martin
3. J. Golaz
4. V. Larson
5. Kelly Chance
6. Xiong Liu
7. C. Sioris
8. T. Kurosu

In Global and Planetary Change

1. Robert J. D. Spurr
2. Randall V. Martin
3. J. Golaz
4. V. Larson
5. Kelly Chance
6. Xiong Liu
7. T. Kurosu
8. C. Sioris

Citations in the corpus

• Understanding Cloud and Convective Characteristics in Version 1 of the E3SM Atmosphere Model (2018, background): “…from evaporated raindrops to coarse mode, the representation of marine organic aerosols, and a linearized ozone chemistry (Linoz2) mechanism (Hsu & Prather, 2009; McLinden et al., 2000) for representing stratospheric ozone and its radiative effects in the stratosphere (Bader et al., 2014).”
• An intercomparison and evaluation of aircraft-derived and simulated CO from seven chemical transport models during the TRACE-P experiment (2003, methodology): “The model uses the ASAD package for gas-phase tropospheric chemistry [Carver et al., 1997], supplemented by a hydrocarbon oxidation scheme and a simplified treatment of stratospheric chemistry using the Linoz approach [McLinden et al., 2000].”
• A revised linear ozone photochemistry parameterization for use in transport and general circulation models: multi-annual simulations (2007, unknown): “This result is consistent with the original findings of CD86 and those of McLinden et al. (2000), who followed a similar approach to derive the LINOZ scheme.”
• Stratospheric variability and tropospheric ozone (2009, methodology): “We approach the problem with a simplified chemical model that is focused on simulating the stratosphere-troposphere exchange (STE) of ozone: a linearized ozone chemistry (Linoz version 1 [ McLinden et al., 2000 ]) combined with unique transport diagnostics that quantify the STE ozone flux as a funct”
• First Directly Retrieved Global Distribution of Tropospheric Column Ozone from GOME: Comparison with the GEOS-CHEM Model (2006, methodology): “The model uses the Synoz flux boundary condition [ McLinden et al. , 2000] to impose a downward ozone flux of 475 Tg O 3 yr (cid:2) 1 from the stratosphere.”