Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correction
Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) is a technique to measure trace gas amounts in the lower troposphere from ground-based scattered sunlight observations. MAX-DOAS observations are especially suitable for validation of tropospheric trace gas observations from satellit...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2010-10-01
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| Series: | Atmospheric Measurement Techniques |
| Online Access: | http://www.atmos-meas-tech.net/3/1287/2010/amt-3-1287-2010.pdf |
| _version_ | 1819176210799788032 |
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| author | P. F. Levelt P. Wang P. Stammes A. J. M. Piters T. Vlemmix |
| author_facet | P. F. Levelt P. Wang P. Stammes A. J. M. Piters T. Vlemmix |
| author_sort | P. F. Levelt |
| collection | DOAJ |
| description | Multi-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) is a technique to measure trace gas amounts in the lower troposphere from ground-based scattered sunlight observations. MAX-DOAS observations are especially suitable for validation of tropospheric trace gas observations from satellite, since they have a representative range of several kilometers, both in the horizontal and in the vertical dimension. <br><br> A two-step retrieval scheme is presented here, to derive aerosol corrected tropospheric NO<sub>2</sub> columns from MAX-DOAS observations. In a first step, boundary layer aerosols, characterized in terms of aerosol optical thickness (AOT), are estimated from relative intensity observations, which are defined as the ratio of the sky radiance at elevation α and the sky radiance in the zenith. Relative intensity measurements have the advantage of a strong dependence on boundary layer AOT and almost no dependence on boundary layer height. In a second step, tropospheric NO<sub>2</sub> columns are derived from differential slant columns, based on AOT-dependent air mass factors. <br><br> This two-step retrieval scheme was applied to cloud free periods in a twelve month data set of observations in De Bilt, The Netherlands. In a comparison with AERONET (Cabauw site) a mean difference in AOT (AERONET minus MAX-DOAS) of −0.01±0.08 was found, and a correlation of 0.85. Tropospheric-NO<sub>2</sub> columns were compared with OMI-satellite tropospheric NO<sub>2</sub>. For ground-based observations restricted to uncertainties below 10%, no significant difference was found, and a correlation of 0.88. |
| first_indexed | 2024-12-22T21:07:09Z |
| format | Article |
| id | doaj.art-0a885e03ec98418eb2b403c7cdec2183 |
| institution | Directory Open Access Journal |
| issn | 1867-1381 1867-8548 |
| language | English |
| last_indexed | 2024-12-22T21:07:09Z |
| publishDate | 2010-10-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Measurement Techniques |
| spelling | doaj.art-0a885e03ec98418eb2b403c7cdec21832022-12-21T18:12:38ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482010-10-01351287130510.5194/amt-3-1287-2010Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correctionP. F. LeveltP. WangP. StammesA. J. M. PitersT. VlemmixMulti-Axis Differential Optical Absorption Spectroscopy (MAX-DOAS) is a technique to measure trace gas amounts in the lower troposphere from ground-based scattered sunlight observations. MAX-DOAS observations are especially suitable for validation of tropospheric trace gas observations from satellite, since they have a representative range of several kilometers, both in the horizontal and in the vertical dimension. <br><br> A two-step retrieval scheme is presented here, to derive aerosol corrected tropospheric NO<sub>2</sub> columns from MAX-DOAS observations. In a first step, boundary layer aerosols, characterized in terms of aerosol optical thickness (AOT), are estimated from relative intensity observations, which are defined as the ratio of the sky radiance at elevation α and the sky radiance in the zenith. Relative intensity measurements have the advantage of a strong dependence on boundary layer AOT and almost no dependence on boundary layer height. In a second step, tropospheric NO<sub>2</sub> columns are derived from differential slant columns, based on AOT-dependent air mass factors. <br><br> This two-step retrieval scheme was applied to cloud free periods in a twelve month data set of observations in De Bilt, The Netherlands. In a comparison with AERONET (Cabauw site) a mean difference in AOT (AERONET minus MAX-DOAS) of −0.01±0.08 was found, and a correlation of 0.85. Tropospheric-NO<sub>2</sub> columns were compared with OMI-satellite tropospheric NO<sub>2</sub>. For ground-based observations restricted to uncertainties below 10%, no significant difference was found, and a correlation of 0.88.http://www.atmos-meas-tech.net/3/1287/2010/amt-3-1287-2010.pdf |
| spellingShingle | P. F. Levelt P. Wang P. Stammes A. J. M. Piters T. Vlemmix Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correction Atmospheric Measurement Techniques |
| title | Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correction |
| title_full | Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correction |
| title_fullStr | Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correction |
| title_full_unstemmed | Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correction |
| title_short | Retrieval of tropospheric NO<sub>2</sub> using the MAX-DOAS method combined with relative intensity measurements for aerosol correction |
| title_sort | retrieval of tropospheric no sub 2 sub using the max doas method combined with relative intensity measurements for aerosol correction |
| url | http://www.atmos-meas-tech.net/3/1287/2010/amt-3-1287-2010.pdf |
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