Armin Kleinböhl, Holger Bremer, Miriam von König, Harry Küllmann,
and Klaus F. Künzi
Institute of Environmental Physics, University of Bremen, Bremen, Germany
Albert P. H. Goede
Space Research Organization of the Netherlands, Utrecht, The Netherlands,
now at: Royal Netherlands Meteorological Institute, De Bilt, The Netherlands
Edward V. Browell and William B. Grant
NASA Langley Research Center, Hampton, VA, USA
Geoffrey C. Toon
Jet Propulsion Laboratory, Pasadena, CA, USA
Thomas Blumenstock
Institute of Meteorology and Climate Research,
Forschungszentrum Karlsruhe and University of Karlsruhe, Karlsruhe, Germany
Bo Galle
Swedish Environmental Research Institute, Gothenburg, Sweden
Björn-Martin Sinnhuber and Stewart Davies
School of the Environment, University of Leeds, Leeds, UK
Abstract
Denitrification has been studied using measurements of stratospheric
HNO3 and N2O by the Airborne SUbmillimeter Radiometer ASUR, operated
on board the NASA DC-8 during THESEO 2000 / SOLVE. Lidar measurements taken
on board the same aircraft have been used to distinguish between temporary
uptake of HNO3 in polar stratospheric clouds (PSCs) and denitrification
events. To derive an NOy budget, ClNO3 data by balloon borne and
ground-based Fourier transform infrared measurements and a model estimate
of NOx + 2 N2O5 have been considered.
The HNO3 profiles of sporadic ASUR measurements without PSC coverage
in January suggest that denitrification had started in the vortex core
region by then. Vortexwide denitrification was found in mid-March 2000.
Corrected for diabatic descent using the N2O measurements, a vortex
averaged NOy deficit between 1.2 +- 0.9 ppb at about 16 km
altitude and 5.3 +- 2.7 ppb at about 20.5 km altitude was derived
compared to December 1999, based on an observed decrease in HNO3
between 2.2 and 3.5 ppb during this time period. A shift in the NOy
partitioning from HNO3 towards ClNO3 of about 0.4 to 0.7 ppb was observed
in mid-March compared to December, indicating that chlorine deactivation
was occurring.
Comparisons with the SLIMCAT 3D chemical transport model applying
denitrification schemes based on ice and nitric acid trihydrate particles
in equilibrium, respectively, reveal agreement within the error bars at higher
altitudes (~19 km) but show discrepancies at lower altitudes
(~16 km). It is suggested that more sophisticated denitrification
schemes are needed to generally describe denitrification processes.