Mobile MAX-DOAS observations of tropospheric trace gases

Abstract. From Multi-Axis- (MAX-) DOAS observations, information on tropospheric trace gases close to the surface and up to the free troposphere can be obtained. Usually MAX-DOAS observations are performed at fixed locations, which allows to retrieve the diurnal variation of tropospheric species at that location. Alternatively, MAX-DOAS observations can also be made on mobile platforms like cars, ships or aircrafts. Then, in addition to the vertical (and temporal) distribution, also the horizontal variation of tropospheric trace gases can be measured. Such information is important for the quantitative comparison with model simulations, study of transport processes, and for the validation of tropospheric trace gas products from satellite observations. However, for MAX-DOAS observations from mobile platforms, the standard analysis techniques for MAX-DOAS observations can usually not be applied, because the probed airmasses can change rapidly between successive measurements. In this study we introduce a new technique which overcomes these problems and allows the exploitation of the full information content of mobile MAX-DOAS observations. Our method can also be applied to MAX-DOAS observations made at fixed locations in order to improve the accuracy especially in cases of strong winds. We apply the new technique to MAX-DOAS observations made during an automobile trip from Brussels to Heidelberg.

[1]  Yan Zhang,et al.  Quantification of total emission of air pollutants from Beijing using mobile mini-DOAS , 2008 .

[2]  Stanley C. Solomon,et al.  On the interpretation of zenith sky absorption measurements , 1987 .

[3]  H. Tanimoto,et al.  Validation of OMI tropospheric NO 2 column data using MAX-DOAS measurements deep inside the North China Plain in June 2006 , 2008 .

[4]  R. L. Curier,et al.  The 2005 and 2006 DANDELIONS NO2 and aerosol intercomparison campaigns , 2008 .

[5]  H. Tanimoto,et al.  Validation of OMI tropospheric NO 2 column data using MAX-DOAS measurements deep inside the North China Plain in June 2006: Mount Tai Experiment 2006 , 2008 .

[6]  F. Hendrick,et al.  Retrieval of stratospheric and tropospheric BrO columns from multi-axis DOAS measurements at Reunion Island (21 S, 56 E) , 2007 .

[7]  Ulrich Platt,et al.  Improved air mass factor concepts for scattered radiation differential optical absorption spectroscopy of atmospheric species , 2000 .

[8]  Dietrich Althausen,et al.  Retrieval of Aerosol Profiles using Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) , 2003 .

[9]  Yugo Kanaya,et al.  Comparison of box-air-mass-factors and radiances for Multiple-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) geometries calculated from different UV/visible radiative transfer models , 2006, Atmospheric Chemistry and Physics.

[10]  John P. Burrows,et al.  Measurements of tropospheric NO 2 with an airborne multi-axis DOAS instrument , 2004 .

[11]  Ulrich Platt,et al.  Observations of BrO and its vertical distribution during surface ozone depletion at Alert , 2002 .

[12]  M. Buchwitz,et al.  SCIAMACHY: Mission Objectives and Measurement Modes , 1999 .

[13]  Johannes Orphal,et al.  Measurements of molecular absorption spectra with the SCIAMACHY pre-flight model: instrument characterization and reference data for atmospheric remote-sensing in the 230–2380 nm region , 2003 .

[14]  Stefan Kraus,et al.  DOASIS: a framework design for DOAS , 2006 .

[15]  Yan Zhang,et al.  Mobile mini-DOAS measurement of the outflow of NO 2 and HCHO from Mexico City , 2009 .

[16]  U. Platt,et al.  Ground‐based measurements of halogen oxides at the Hudson Bay by active longpath DOAS and passive MAX‐DOAS , 2004 .

[17]  J. Grainger,et al.  Anomalous Fraunhofer Line Profiles , 1962, Nature.

[18]  Ingemar Furenlid,et al.  Solar flux atlas from 296 to 1300 nm , 1985 .

[19]  John P. Burrows,et al.  MAX-DOAS measurements of atmospheric trace gases in Ny- ˚ Alesund - Radiative transfer studies and their application , 2004 .

[20]  J. Lambert,et al.  Retrieval of Tropospheric BrO and NO2 from UV-Visible Observations , 2004 .

[21]  U. Platt,et al.  MAX‐DOAS measurements of BrO and NO2 in the marine boundary layer , 2003 .

[22]  Stanley C. Solomon,et al.  On the evaluation of air mass factors for atmospheric near‐ultraviolet and visible absorption spectroscopy , 1993 .

[23]  J. Burrows,et al.  No 2 Profile Retrieval Using Amaxdoas Data Atmospheric Chemistry and Physics Discussions No 2 Profile Retrieval Using Airborne Multi Axis Uv-visible Skylight Absorption Measurements over Central Europe No 2 Profile Retrieval Using Amaxdoas Data , 2022 .

[24]  Ulrich Platt,et al.  Determination of aerosol properties from MAX-DOAS observations of the Ring effect , 2009 .

[25]  L. Molina,et al.  Mobile mini-DOAS measurement of the emission of NO 2 and HCHO from Mexico City , 2009 .

[26]  J. Veefkind,et al.  Validation of Ozone Monitoring Instrument nitrogen dioxide columns , 2008 .

[27]  Maria Tzortziou,et al.  NO2 column amounts from ground‐based Pandora and MFDOAS spectrometers using the direct‐sun DOAS technique: Intercomparisons and application to OMI validation , 2009 .

[28]  Ann Carine Vandaele,et al.  Measurements of the NO2 absorption cross-section from 42 000 cm−1 to 10 000 cm−1 (238–1000 nm) at 220 K and 294 K , 1998 .

[29]  James B. Burkholder,et al.  Absorption measurements of oxygen between 330 and 1140 nm , 1990 .

[30]  Ulrich Platt,et al.  Differential optical absorption spectroscopy , 2008 .

[31]  R. S. Hyde,et al.  Stratospheric NO2: 1. Observational method and behavior at mid‐latitude , 1979 .

[32]  U. Platt,et al.  Numerical analysis and estimation of the statistical error of differential optical absorption spectroscopy measurements with least-squares methods. , 1996, Applied optics.

[33]  John P. Burrows,et al.  Validation of SCIAMACHY tropospheric NO2-columns with AMAXDOAS measurements , 2004 .

[34]  Ulrich Platt,et al.  MAX‐DOAS O4 measurements: A new technique to derive information on atmospheric aerosols: 2. Modeling studies , 2006 .

[35]  Gang Li,et al.  The HITRAN 2008 molecular spectroscopic database , 2005 .

[36]  J. Burrows,et al.  Ground-based measurements of tropospheric and stratospheric bromine monoxide above Nairobi (1° S, 36° E) , 2007 .

[37]  T. Wagner,et al.  Enhanced tropospheric BrO over Antarctic sea ice in mid winter observed by MAX-DOAS on board the research vessel Polarstern , 2007 .

[38]  O. Ibrahim Applications on Ground-based Tropospheric Measurements using Multi-Axis Differential Optical Absorption Spectrosopy , 2009 .

[39]  John P. Burrows,et al.  MAX-DOAS measurements of formaldehyde in the Po-Valley , 2004 .

[40]  B. Dix,et al.  Airborne multi-axis DOAS measurements of atmospheric trace gases on CARIBIC long-distance flights , 2009 .

[41]  John P. Burrows,et al.  Airborne multi-axis DOAS measurements of tropospheric SO 2 plumes in the Po-valley , Italy , 2005 .

[42]  Ulrich Platt,et al.  MAX‐DOAS O4 measurements: A new technique to derive information on atmospheric aerosols—Principles and information content , 2004 .