NO₂ climatology in the northern subtropical region: diurnal, seasonal and interannual variability

M. Gil (1) , M. Yela (1) , L. N. Gunn (2) , A. Richter (3) , I. Alonso (1) , M. P. Chipperfield (2) , E. Cuevas (4) , J. Iglesias (1) , M. Navarro (1) , O. Puentedura (1) , S. Rodríguez (1)

1 Area de Investigación e Instrumentación Atmosférica
2 Institute for Atmospheric Science [Leeds]
3 IUP - Institute of Environmental Physics [Bremen]
4 Centro de Investigación Atmosférica de Izana

Daily NO₂ vertical column density (VCD) has been routinely measured by zenith sky spectroscopy at the subtropical station of Izaña (28° N, 16° W) since 1993 in the framework of the Network for the Detection of Atmospheric Composition Change (NDACC). Based on 14 years of data the first low latitudes NO₂ VCD climatology has been established and the main characteristics from short scales of one day to inter-annual variability are presented. Instrumental descriptions and different source of errors are described in detail. The observed diurnal cycle follows that expected by gas-phase NOx chemistry, as can be shown by the good agreement with a vertically integrated chemical box model, and is modulated by solar radiation. The seasonal evolution departs from the phase of the hours of daylight, showing the signature of upper stratospheric temperature changes. From the data record no significant long-term trends in NO₂ VCD can be inferred. Comparison of the ground-based data sets with nadir looking satellite spectrometers shows excellent agreement for SCIAMACHY with differences between both datasets of 1.1%. GOME displays unrealistic features with largest discrepancies during summer. The ground-based data are compared with long-term output of the SLIMCAT 3-D chemical transport model (CTM). The basic model, forced by ECMWF (ERA-40) analyses, captures the observed NO₂ annual cycle but significantly underestimates the spring/summer maximum. In a model run which uses assimilation of satellite CH₄ profiles to constrain the model long-lived tracers the agreement is significantly improved. This improvement in modelled column NO₂ is due to better modelled NOy profiles and points to transport errors in the ECMWF ERA-40 reanalyses.

Domaines: Océan, Atmosphère

M. Gil, M. Yela, L. N. Gunn, A. Richter, I. Alonso, et al.. NO₂ climatology in the northern subtropical region: diurnal, seasonal and interannual variability. Atmospheric Chemistry and Physics Discussions, 2007, 7 (5), pp.15067-15103. ⟨hal-00303960⟩