Title of article :
Estimating the influence of lightning on upper tropospheric ozone using NLDN lightning data and CMAQ model
Author/Authors :
Wang، نويسنده , , Lihua and Newchurch، نويسنده , , M.J. and Pour-Biazar، نويسنده , , Arastoo and Kuang، نويسنده , , Shi and Khan، نويسنده , , Maudood and Liu، نويسنده , , Xiong and Koshak، نويسنده , , William T. Chance PhD، نويسنده , , Kelly، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2013
Pages :
10
From page :
219
To page :
228
Abstract :
Lightning is a particularly significant NOx source in the middle and upper troposphere where it affects tropospheric chemistry and ozone. Because the version-4 Community Multiscale Air Quality Modeling System (CMAQ) does not account for NOx emission from lightning, it underpredicts NOx above the mixed layer. In this study, the National Lightning Detection Network™ (NLDN) lightning data are applied to the CMAQ model to simulate the influence of lightning-produced NOx (LNOx) on upper tropospheric NOx and subsequent ozone concentration. Using reasonable values for salient parameters (detection efficiency ∼95%, cloud flash to ground flash ratio ∼3, LNOx production rate ∼500 mol N per flash), the NLDN ground flashes are converted into total lightning NOx amount and then vertically distributed on 39 CMAQ model layers according to a vertical-distribution profile of lightning N mass. This LNOx contributes 27% of the total NOx emission during 15 July ∼7 September 2006. This additional NOx reduces the low-bias of simulated tropospheric O3 columns with respect to OMI tropospheric O3 columns from 10 to 5%. Although the model prediction of ozone in upper troposphere improves by ∼20 ppbv due to lightning-produced NOx above the southeastern and eastern U.S.A., the improved ozone prediction is still ∼20–25 ppbv lower than ozonesonde measurements.
Keywords :
LNOx , lightning , CMAQ , ozone , NLDN , OMI , IONS06
Journal title :
Atmospheric Environment
Serial Year :
2013
Journal title :
Atmospheric Environment
Record number :
2240603
Link To Document :
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