Open AccessTropospheric O 3 distribution over the Indian Ocean during spring 1995 evaluated with a chemistry‐climate model
Author(s) -
Laat A. T. J.,
Zachariasse M.,
Roelofs G. J.,
Velthoven P.,
Dickerson R. R.,
Rhoads K. P.,
Oltmans S. J.,
Lelieveld J.
Publication year - 1999
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/1999jd900176
Subject(s) - troposphere , intertropical convergence zone , climatology , atmospheric sciences , environmental science , diurnal temperature variation , climate model , convergence zone , meteorology , geology , climate change , oceanography , precipitation , geography
An analysis of tropospheric O 3 over the Indian Ocean during spring 1995 is presented based on O 3 soundings and results from the European Centre Hamburg (ECHAM) chemistry‐general circulation model. The ECHAM model is nudged toward actual meteorology using European Centre for Medium‐Range Weather Forecasts analyses, to enable a direct comparison between model results and in situ observations. The model reproduces observed CO levels in different air mass categories. The model also reproduces the general tendencies and the diurnal variation in the observed surface pressure, although the amplitude of the diurnal variation in the amplitude is underestimated. The model simulates the general O 3 tendencies as seen in the sonde observations. Tropospheric O 3 profiles were characterized by low surface concentrations (<10 ppbv), midtropospheric maxima (60–100 ppbv, at 700–250 hPa) and upper tropospheric minima (<20 ppbv, at 250–100 hPa). Large‐scale upper tropospheric O 3 minima were caused by connective transport of O 3 ‐depleted boundary layer air in the intertropical convergence zone (ITCZ). Similarly, an upper tropospheric O 3 minimum was caused by Cyclone Marlene south of the ITCZ. The midtropospheric O 3 maxima were caused by transport of polluted African air. The ECHAM model appears to overestimate surface O 3 levels and does not reproduce the diurnal variations very well. This could be related to unaccounted multiphase O 3 destruction mechanisms involving low level clouds and aerosols, and missing halogen chemistry.