DOAS measurements on HALO • Scientific Objectives • Technical
Transcription
DOAS measurements on HALO • Scientific Objectives • Technical
DOAS measurements on HALO K. Pfeilsticker, F. Weidner, M. Dorf, H. Bösch, T. Wagner, K.-P. Heue, A. Richter(2), M. Bruns, P. Wang, U. Platt et al., Institut für Umweltphysik (IUP) Universität Heidelberg (2) Institut für Umweltphysik (IUP) Universität Bremen • Scientific Objectives • Technical details of the actual DOAS instruments • Results of balloon borne measurements • Results of Airborne Multi AXis DOAS instrument • Status & Summary Institut für Umweltphysik University of Heidelberg Scientific Objectives DOAS (UV/Vis) profile measurements in the UT/LS and TTL may address 1. bromine oxide budget and photochemistry (Dorf et al., 2005) trend in total stratospheric bromine role of VSLS 2. iodine oxide budget and photochemistry (Bösch et al., 2003) sources (VSLS) and sinks (aerosols ?) of iodine oxides role in photochemistry 3. Skylight radiance and photolysis rates 4. Ozone loss in combined BrOx/HOx and BrOx/ClOx cycles Institut für Umweltphysik University of Heidelberg Technical Details Airborne DOAS Observation mode: • use (UV/Vis) scattered skylight near the horizon Scanning mini DOAS - Small, light instrument - Small power consumption Flew on several balloons but it is in principle easy to handle and install (2) +2°elevation (1) Zenith AMAXDOAS (with IUP Bremen) - Good Spectral resolution - Linear dispersion - 2-D CCD Chip => Stray light correction Flew on Falcon D-CMET (1) (2) (4) (3) (3) -2°elevation (4) Nadir 400 450 500 550 Wavelength [nm] Institut für Umweltphysik University of Heidelberg Technical Details Airborne DOAS Data evaluation: • DOAS procedure on measured spectra for targeted gases • post flight Radiative Transfer calculation of air mass factors using aircraft altitude data, solar ephemerids and atmospheric data (T, P, aerosol and cloud droplet density) • Mathematical inversion of measured differential slant column amounts into absolute concentrations Institut für Umweltphysik University of Heidelberg Results (1): Time-dependent O3 and NO2 mini-DOAS observations on LPMA/IASI at Teresina/Brazil on June 30, 2005. 45 Altitude [km] 40 72 65 53 47 41 30 29 30 33 12 O3 0 1.0 1.6 1.8 2.0 2.2 2.4 2.6 2.8 3.0 3.2 3.4 3.6 3.8 4.0 35 30 25 20 15 40 3 10 molec/cm 45 10 Altitude [km] 59 SZA[°] 37 33 NO2 Envisat/SCIAMACHY overpass #17412 #17441 9 35 30 25 20 15 10 11:00 12:00 3 10 molec/cm 13:00 14:00 Time[UT] 15:00 16:00 0 0.0 0.4 0.5 0.6 0.7 0.8 0.9 1.0 1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 (courtesy: Kritten et al., IUP-Heidelberg) Institut für Umweltphysik University of Heidelberg Results (2): NO2 and BrO profiling mini DOAS on LPMA/DOAS at Kiruna on March 24, 2004. HALO F.A. HALO F.A. (Weidner et al. 2005) Institut für Umweltphysik University of Heidelberg AMAXDOAS Detection of BL BrO • AMAXDOAS -BrO Falcon flight track from Iceland over Greenland and back • during last part of measurements close to but not above regions with large BrO concentrations • large BrO signals in nadir off-axis 88° direction ⇒ has BrO been lifted into the free troposphere? P. Wang, K.-P. Heue, M. Bruns, T. Wagner, and A. Richter Institut für Umweltphysik University of Heidelberg OClO Slant columns AMAXDOAS - GOME molec cm-2 76 14 x 10 5 OClO slant column 92° viewing angle 75 4 74 Latitude (°N) 73 3 72 2 71 70 1 69 0 68 Kiruna 67 20 21 22 23 Longitude (°E) 24 25 -1 Return flight OClO slant columns smaller than during first part of the flight due to different radiative transport and chemistry Different solar zenith angle Different solar azimuth OClO photolysis Go to / leave vortex Wang et al. 16th SA/PAC Symposium 5 June 2003, St. Gallen, Switzerland Institut für Umweltphysik University of Heidelberg Status & Summary Mini-DOAS measurements have been successfully performed on 8 balloon flights from high, mid and low latitudes (Weidner et al., 2005). AMAXDOAS measurements have been successfully performed on 29 Falcon flights between Greenland and the Seychelles on 20 boundary layer flights in the Po basin (Partenavia 68) Past/present studies addressed • Feasibility of the methods (Weidner, 2005; Heue, 2005; Bruns, 2004) • Validation of the limb method employed e.g. on ENVISAT/SCIAMACHY • Validation of SCIAMACHY tropospheric columns (Heue et al.,2005) • NO2 and cloud studies (Wang et al., 2005) • HCHO, SO2 and NO2 observed in boundary layer flights (Wang et al., 2005) Upcoming projects • Deployment on HALO !! Institut für Umweltphysik University of Heidelberg