Ozone profile retrievals from the Ozone Monitoring Instrument
Ozone profiles from the surface to about 60 km are retrieved from Ozone Monitoring Instrument (OMI) ultraviolet radiances using the optimal estimation technique. OMI provides daily ozone profiles for the entire sunlit portion of the earth at a horizontal resolution of 13 km×48 km for t...
| Main Authors: | , , , , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2010-03-01
|
| Series: | Atmospheric Chemistry and Physics |
| Online Access: | http://www.atmos-chem-phys.net/10/2521/2010/acp-10-2521-2010.pdf |
| _version_ | 1828496443748384768 |
|---|---|
| author | X. Liu P. K. Bhartia K. Chance R. J. D. Spurr T. P. Kurosu |
| author_facet | X. Liu P. K. Bhartia K. Chance R. J. D. Spurr T. P. Kurosu |
| author_sort | X. Liu |
| collection | DOAJ |
| description | Ozone profiles from the surface to about 60 km are retrieved from Ozone Monitoring Instrument (OMI) ultraviolet radiances using the optimal estimation technique. OMI provides daily ozone profiles for the entire sunlit portion of the earth at a horizontal resolution of 13 km×48 km for the nadir position. The retrieved profiles have sufficient accuracy in the troposphere to see ozone perturbations caused by convection, biomass burning and anthropogenic pollution, and to track their spatiotemporal transport. However, to achieve such accuracy it has been necessary to calibrate OMI radiances carefully (using two days of Aura/Microwave Limb Sounder data taken in the tropics). The retrieved profiles contain ~6–7 degrees of freedom for signal, with 5–7 in the stratosphere and 0–1.5 in the troposphere. Vertical resolution varies from 7–11 km in the stratosphere to 10–14 km in the troposphere. Retrieval precisions range from 1% in the middle stratosphere to 10% in the lower stratosphere and troposphere. Solution errors (i.e., root sum square of precisions and smoothing errors) vary from 1–6% in the middle stratosphere to 6–35% in the troposphere, and are dominated by smoothing errors. Total, stratospheric, and tropospheric ozone columns can be retrieved with solution errors typically in the few Dobson unit range at solar zenith angles less than 80°. |
| first_indexed | 2024-12-11T12:29:56Z |
| format | Article |
| id | doaj.art-fd7cf97b77424f3e99687903e87f0612 |
| institution | Directory Open Access Journal |
| issn | 1680-7316 1680-7324 |
| language | English |
| last_indexed | 2024-12-11T12:29:56Z |
| publishDate | 2010-03-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Atmospheric Chemistry and Physics |
| spelling | doaj.art-fd7cf97b77424f3e99687903e87f06122022-12-22T01:07:16ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242010-03-0110525212537Ozone profile retrievals from the Ozone Monitoring InstrumentX. LiuP. K. BhartiaK. ChanceR. J. D. SpurrT. P. KurosuOzone profiles from the surface to about 60 km are retrieved from Ozone Monitoring Instrument (OMI) ultraviolet radiances using the optimal estimation technique. OMI provides daily ozone profiles for the entire sunlit portion of the earth at a horizontal resolution of 13 km×48 km for the nadir position. The retrieved profiles have sufficient accuracy in the troposphere to see ozone perturbations caused by convection, biomass burning and anthropogenic pollution, and to track their spatiotemporal transport. However, to achieve such accuracy it has been necessary to calibrate OMI radiances carefully (using two days of Aura/Microwave Limb Sounder data taken in the tropics). The retrieved profiles contain ~6–7 degrees of freedom for signal, with 5–7 in the stratosphere and 0–1.5 in the troposphere. Vertical resolution varies from 7–11 km in the stratosphere to 10–14 km in the troposphere. Retrieval precisions range from 1% in the middle stratosphere to 10% in the lower stratosphere and troposphere. Solution errors (i.e., root sum square of precisions and smoothing errors) vary from 1–6% in the middle stratosphere to 6–35% in the troposphere, and are dominated by smoothing errors. Total, stratospheric, and tropospheric ozone columns can be retrieved with solution errors typically in the few Dobson unit range at solar zenith angles less than 80°.http://www.atmos-chem-phys.net/10/2521/2010/acp-10-2521-2010.pdf |
| spellingShingle | X. Liu P. K. Bhartia K. Chance R. J. D. Spurr T. P. Kurosu Ozone profile retrievals from the Ozone Monitoring Instrument Atmospheric Chemistry and Physics |
| title | Ozone profile retrievals from the Ozone Monitoring Instrument |
| title_full | Ozone profile retrievals from the Ozone Monitoring Instrument |
| title_fullStr | Ozone profile retrievals from the Ozone Monitoring Instrument |
| title_full_unstemmed | Ozone profile retrievals from the Ozone Monitoring Instrument |
| title_short | Ozone profile retrievals from the Ozone Monitoring Instrument |
| title_sort | ozone profile retrievals from the ozone monitoring instrument |
| url | http://www.atmos-chem-phys.net/10/2521/2010/acp-10-2521-2010.pdf |
| work_keys_str_mv | AT xliu ozoneprofileretrievalsfromtheozonemonitoringinstrument AT pkbhartia ozoneprofileretrievalsfromtheozonemonitoringinstrument AT kchance ozoneprofileretrievalsfromtheozonemonitoringinstrument AT rjdspurr ozoneprofileretrievalsfromtheozonemonitoringinstrument AT tpkurosu ozoneprofileretrievalsfromtheozonemonitoringinstrument |