Lightning and convection parameterisations ─ uncertainties in global modelling

The simulation of convection, lightning and consequent NO<sub>x</sub> emissions with global atmospheric chemistry models is associated with large uncertainties since these processes are heavily parameterised. Each parameterisation by itself has deficiencies and the combination of these s...

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Main Authors: J. Lelieveld, P. Jöckel, H. Tost
Format: Article
Language:English
Published: Copernicus Publications 2007-09-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/7/4553/2007/acp-7-4553-2007.pdf
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spelling doaj-edd1438f59f44b4490fb5cb8429acaef2020-11-24T21:33:17ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242007-09-0171745534568Lightning and convection parameterisations ─ uncertainties in global modellingJ. LelieveldP. JöckelH. TostThe simulation of convection, lightning and consequent NO<sub>x</sub> emissions with global atmospheric chemistry models is associated with large uncertainties since these processes are heavily parameterised. Each parameterisation by itself has deficiencies and the combination of these substantially increases the uncertainties compared to the individual parameterisations. In this study several combinations of state-of-the-art convection and lightning parameterisations are used in simulations with the global atmospheric chemistry general circulation model ECHAM5/MESSy, and are evaluated against lightning observations. A wide range in the spatial and temporal variability of the simulated flash densities is found, attributed to both types of parameterisations. Some combinations perform well, whereas others are hardly applicable. In addition to resolution dependent rescaling parameters, each combination of lightning and convection schemes requires individual scaling to reproduce the observed flash frequencies. The resulting NO<sub>x</sub> profiles are inter-compared, however definite conclusions about the most realistic profiles can currently not be drawn. http://www.atmos-chem-phys.net/7/4553/2007/acp-7-4553-2007.pdf
collection DOAJ
language English
format Article
sources DOAJ
author J. Lelieveld
P. Jöckel
H. Tost
spellingShingle J. Lelieveld
P. Jöckel
H. Tost
Lightning and convection parameterisations ─ uncertainties in global modelling
Atmospheric Chemistry and Physics
author_facet J. Lelieveld
P. Jöckel
H. Tost
author_sort J. Lelieveld
title Lightning and convection parameterisations ─ uncertainties in global modelling
title_short Lightning and convection parameterisations ─ uncertainties in global modelling
title_full Lightning and convection parameterisations ─ uncertainties in global modelling
title_fullStr Lightning and convection parameterisations ─ uncertainties in global modelling
title_full_unstemmed Lightning and convection parameterisations ─ uncertainties in global modelling
title_sort lightning and convection parameterisations ─ uncertainties in global modelling
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2007-09-01
description The simulation of convection, lightning and consequent NO<sub>x</sub> emissions with global atmospheric chemistry models is associated with large uncertainties since these processes are heavily parameterised. Each parameterisation by itself has deficiencies and the combination of these substantially increases the uncertainties compared to the individual parameterisations. In this study several combinations of state-of-the-art convection and lightning parameterisations are used in simulations with the global atmospheric chemistry general circulation model ECHAM5/MESSy, and are evaluated against lightning observations. A wide range in the spatial and temporal variability of the simulated flash densities is found, attributed to both types of parameterisations. Some combinations perform well, whereas others are hardly applicable. In addition to resolution dependent rescaling parameters, each combination of lightning and convection schemes requires individual scaling to reproduce the observed flash frequencies. The resulting NO<sub>x</sub> profiles are inter-compared, however definite conclusions about the most realistic profiles can currently not be drawn.
url http://www.atmos-chem-phys.net/7/4553/2007/acp-7-4553-2007.pdf
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AT pjockel lightningandconvectionparameterisationsuncertaintiesinglobalmodelling
AT htost lightningandconvectionparameterisationsuncertaintiesinglobalmodelling
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