TY - JOUR
T1 - The chemistry-climate model ECHAM6.3-HAM2.3-MOZ1.0
AU - Schultz, Martin G.
AU - Stadtler, Scarlet
AU - Schröder, Sabine
AU - Taraborrelli, Domenico
AU - Franco, Bruno
AU - Krefting, Jonathan
AU - Henrot, Alexandra
AU - Ferrachat, Sylvaine
AU - Lohmann, Ulrike
AU - Neubauer, David
AU - Siegenthaler-Le Drian, Colombe
AU - Wahl, Sebastian
AU - Kokkola, Harri
AU - Kühn, Thomas
AU - Rast, Sebastian
AU - Schmidt, Hauke
AU - Stier, Philip
AU - Kinnison, Doug
AU - Tyndall, Geoffrey S.
AU - Orlando, John J.
AU - Wespes, Catherine
N1 - Publisher Copyright:
© 2018 Author(s).
PY - 2018/5/4
Y1 - 2018/5/4
N2 - The chemistry-climate model ECHAM-HAMMOZ contains a detailed representation of tropospheric and stratospheric reactive chemistry and state-of-the-art parameterizations of aerosols using either a modal scheme (M7) or a bin scheme (SALSA). This article describes and evaluates the model version ECHAM6.3-HAM2.3-MOZ1.0 with a focus on the tropospheric gas-phase chemistry. A 10-year model simulation was performed to test the stability of the model and provide data for its evaluation. The comparison to observations concentrates on the year 2008 and includes total column observations of ozone and CO from IASI and OMI, Aura MLS observations of temperature, HNO3, ClO, and O3 for the evaluation of polar stratospheric processes, an ozonesonde climatology, surface ozone observations from the TOAR database, and surface CO data from the Global Atmosphere Watch network. Global budgets of ozone, OH, NOx, aerosols, clouds, and radiation are analyzed and compared to the literature. ECHAM-HAMMOZ performs well in many aspects. However, in the base simulation, lightning NOx emissions are very low, and the impact of the heterogeneous reaction of HNO3 on dust and sea salt aerosol is too strong. Sensitivity simulations with increased lightning NOx or modified heterogeneous chemistry deteriorate the comparison with observations and yield excessively large ozone budget terms and too much OH. We hypothesize that this is an impact of potential issues with tropical convection in the ECHAM model.
AB - The chemistry-climate model ECHAM-HAMMOZ contains a detailed representation of tropospheric and stratospheric reactive chemistry and state-of-the-art parameterizations of aerosols using either a modal scheme (M7) or a bin scheme (SALSA). This article describes and evaluates the model version ECHAM6.3-HAM2.3-MOZ1.0 with a focus on the tropospheric gas-phase chemistry. A 10-year model simulation was performed to test the stability of the model and provide data for its evaluation. The comparison to observations concentrates on the year 2008 and includes total column observations of ozone and CO from IASI and OMI, Aura MLS observations of temperature, HNO3, ClO, and O3 for the evaluation of polar stratospheric processes, an ozonesonde climatology, surface ozone observations from the TOAR database, and surface CO data from the Global Atmosphere Watch network. Global budgets of ozone, OH, NOx, aerosols, clouds, and radiation are analyzed and compared to the literature. ECHAM-HAMMOZ performs well in many aspects. However, in the base simulation, lightning NOx emissions are very low, and the impact of the heterogeneous reaction of HNO3 on dust and sea salt aerosol is too strong. Sensitivity simulations with increased lightning NOx or modified heterogeneous chemistry deteriorate the comparison with observations and yield excessively large ozone budget terms and too much OH. We hypothesize that this is an impact of potential issues with tropical convection in the ECHAM model.
UR - https://www.scopus.com/pages/publications/85046833399
U2 - 10.5194/gmd-11-1695-2018
DO - 10.5194/gmd-11-1695-2018
M3 - Article
AN - SCOPUS:85046833399
SN - 1991-959X
VL - 11
SP - 1695
EP - 1723
JO - Geoscientific Model Development
JF - Geoscientific Model Development
IS - 5
ER -