N: 90 S: -90 E: 180 W: -180
Description
The Aura Ozone Monitoring Instrument (OMI) Level-1B (L1B) Geo-located Earth View VIS Radiance, Global-Mode (OML1BRVG) Version-3 product contains geo-located Earth view spectral radiances from the VIS detector in the wavelength range of 349 to 504 nm conducted in the global measurement mode. In the standard global measurement mode, OMI observes 60 ground pixels (13 km x 24 km at nadir) across the swath (13 km x 48 km at nadir). Each file contains data from the day lit portion of an orbit (~60 minutes) and is roughly 200 MB in size. There are approximately 14 orbits per day. Once a month, in one orbit, OMI performs dark measurements, it does not perform radiance measurements. In addition, OMI performs spatial zoom measurements one day per month. For that day, this product also contains UV2 measurements that are rebinned from the spatial zoom-in measurements. In original spatial zoom mode the nadir ground pixel size is 13 x 12 km and measurements are available only for the UV2 and VIS wavelengths (306 to 432 nm). The shortname for this OMI Level-1B Product is OML1BRVG. The lead algorithm scientist for this product is Dr. Marcel Dobber from the Royal Netherlands Meteorological Institude (KNMI).
The OML1BRVG files are stored in the HDF4 based EOS Hierarchical Data Format (HDF-EOS). The radiances for the earth measurements (also referred as signal) and its precision are stored as a 16-bit mantissa and an 8-bit exponent. The signal can be computed using the equation: signal = mantissa x 10^exponent. For the precision, the same exponent is used as for the signal.
Product Summary
Citation
Citation is critically important for dataset documentation and discovery. This dataset is openly shared, without restriction, in accordance with the EOSDIS Data Use and Citation Guidance.
Copy Citation
Documents
READ-ME
PI DOCUMENTATION
ALGORITHM THEORETICAL BASIS DOCUMENT (ATBD)
Publications Citing This Dataset
| Title | Year Sort ascending | Author | Topic |
|---|---|---|---|
| Harmonized cloud datasets for the Ozone Monitoring Instrument (OMI) and TROPOspheric Monitoring Instrument (TROPOMI) using the O2O2 477 nm absorption ... | Yu, Huan, De Smedt, Isabelle, Theys, Nicolas, Sneep, Maarten, Veefkind, Pepijn, Van Roozendael, Michel | Solar Irradiance, Visible Radiance, Cloud Fraction, Cloud Top Pressure | |
| Updated OMI Glyoxal Column Measurements Using Collection 4 Level 1B | Kwon, HyeongAhn, Gonzalez Abad, Gonzalo, Chan Miller, Christopher, Hall, Kirsten R., Nowlan, Caroline R., OSullivan, Ewan, Wang, Huiqun, Chong, Heesung, Ayazpour, Zolal, Liu, Xiong, Chance, Kelly | Solar Irradiance, Visible Radiance, Cloud Fraction, Cloud Top Pressure | |
| Use of machine learning and principal component analysis to retrieve nitrogen dioxide (NO2) with hyperspectral imagers and reduce noise in spectral fitting | Joiner, Joanna, Marchenko, Sergey, Fasnacht, Zachary, Lamsal, Lok, Li, Can, Vasilkov, Alexander, Krotkov, Nickolay | ULTRAVIOLET RADIANCE, Nitrogen Dioxide, Visible Radiance | |
| Estimating spectral effects of absorbing aerosols on backscattered UV radiation | Jethva, Hiren, Haffner, David P., Bhartia, Pawan K., Torres, Omar | ULTRAVIOLET RADIANCE, Visible Radiance, Aerosol Extinction, Aerosol Optical Depth/Thickness | |
| Ozone Monitoring Instrument (OMI) collection 4: establishing a 17-year-long series of detrended level-1b data | Kleipool, Quintus, Rozemeijer, Nico, van Hoek, Mirna, Leloux, Jonatan, Loots, Erwin, Ludewig, Antje, van der Plas, Emiel, Adrichem, Daley, Harel, Raoul, Spronk, Simon, ter Linden, Mark, Jaross, Glen, Haffner, David, Veefkind, Pepijn, Levelt, Pieternel F. | ULTRAVIOLET RADIANCE, Solar Irradiance, Visible Radiance | |
| Detection of anomalies in the UVvis reflectances from the Ozone Monitoring Instrument | Gorkavyi, Nick, Fasnacht, Zachary, Haffner, David, Marchenko, Sergey, Joiner, Joanna, Vasilkov, Alexander | Visible Radiance, Sulfur Dioxide, ULTRAVIOLET RADIANCE | |
| Explicit and consistent aerosol correction for visible wavelength satellite cloud and nitrogen dioxide retrievals based on optical properties from a global ... | Vasilkov, Alexander, Krotkov, Nickolay, Yang, Eun-Su, Lamsal, Lok, Joiner, Joanna, Castellanos, Patricia, Fasnacht, Zachary, Spurr, Robert | Visible Radiance, Nitrogen Dioxide, Reflectance, Aerosol Extinction, Aerosol Optical Depth/Thickness | |
| Observations by Ground-Based MAX-DOAS of the Vertical Characters of Winter Pollution and the Influencing Factors of HONO Generation in Shanghai, China | Xu, Shiqi, Wang, Shanshan, Xia, Men, Lin, Hua, Xing, Chengzhi, Ji, Xiangguang, Su, Wenjing, Tan, Wei, Liu, Cheng, Hu, Qihou | Visible Radiance | |
| Calibration and Data Quality Assurance Technical Advancements for Quantitative Remote Sensing in the DRAGON 4 Project | Ma, Lingling, Zhao, Yongguang, Li, Chuanrong, Goryl, Philippe, Liu, Cheng, He, Jieying, Wang, Pucai, Bouvet, Marc, Zhao, Ran, Wang, Ning, Liu, Yaokai, Gao, Caixia, Dils, Bart, Zhang, Chengxin, Chan, Ka Lok, Wang, Xinhong | Visible Radiance | |
| Synergistic use of hyperspectral uv-visible omi and broadband meteorological imager MODIS data for a merged aerosol product | Go, Sujung, Kim, Jhoon, Park, Sang Seo, Kim, Mijin, Lim, Hyunkwang, Kim, Ji-Young, Lee, Dong-Won, Im, Jungho | Albedo, Anisotropy, Aerosol Extinction, Aerosol Optical Depth/Thickness, Solar Irradiance, Visible Radiance | |
| Validation of Aura-OMI QA4ECV NO2 climate data records with ground-based DOAS networks: the role of measurement and comparison uncertainties | Compernolle, Steven, Verhoelst, Tijl, Pinardi, Gaia, Granville, Jose, Hubert, Daan, Keppens, Arno, Niemeijer, Sander, Rino, Bruno, Bais, Alkis, Beirle, Steffen, Boersma, Folkert, Burrows, John P., De Smedt, Isabelle, Eskes, Henk, Goutail, Florence, Hendrick, Francois, Lorente, Alba, Pazmino, Andrea, Piters, Ankie, Peters, Enno, Pommereau, Jean-Pierre, Remmers, Julia, Richter, Andreas, van Geffen, Jos, Van Roozendael, Michel, Wagner, Thomas, Lambert, Jean-Christopher | Nitrogen Dioxide, Cloud Fraction, Cloud Top Pressure, Nitrogen Dioxide, Visible Radiance | |
| Discrete-wavelength DOAS NO2 slant column retrievals from OMI and TROPOMI | Ruiz Villena, Cristina, Anand, Jasdeep S., Leigh, Roland J., Monks, Paul S., Parfitt, Claire E., Vande Hey, Joshua D. | Visible Radiance | |
| Development and Application of HECORA Cloud Retrieval Algorithm Based On the O2-O2 477 nm Absorption Band | Wang, Shuntian, Liu, Cheng, Zhang, Wenqiang, Hao, Nan, Gimeno Garcia, Sebastian, Xing, Chengzhi, Zhang, Chengxin, Su, Wenjing, Liu, Jianguo | Cloud Fraction, Cloud Top Pressure, Visible Radiance | |
| Effects of spatiotemporal O4 column densities and temperature-dependent O4 absorption cross-section on an aerosol effective height retrieval algorithm using the O4 ... | Choi, Wonei, Lee, Hanlim, Kim, Jhoon, Ryu, Jae-Yong, Park, Sang Seo, Park, Junsung, Kang, Hyeongwoo | Cloud Fraction, Cloud Top Pressure, Solar Irradiance, Atmospheric Ozone, Reflectance, Aerosol Optical Depth/Thickness, Visible Radiance | |
| A Retrieval of Glyoxal from OMI over China: Investigation of the Effects of Tropospheric NO2 | Wang, Yapeng, Tao, Jinhua, Cheng, Liangxiao, Yu, Chao, Wang, Zifeng, Chen, Liangfu | Cloud Fraction, Cloud Top Pressure, Nitrogen Dioxide, Visible Radiance | |
| Ship-based MAX-DOAS measurements of tropospheric NO2, SO2, and HCHO distribution along the Yangtze River | Hong, Qianqian, Liu, Cheng, Chan, Ka Lok, Hu, Qihou, Xie, Zhouqing, Liu, Haoran, Si, Fuqi, Liu, Jianguo | Visible Radiance | |
| Tropospheric NO2, SO2, and HCHO over the East China Sea, using ship-based MAX-DOAS observations and comparison with OMI and OMPS satellite data | Tan, Wei, Liu, Cheng, Wang, Shanshan, Xing, Chengzhi, Su, Wenjing, Zhang, Chengxin, Xia, Congzi, Liu, Haoran, Cai, Zhaonan, Liu, Jianguo | Visible Radiance | |
| Aerosol-type retrieval and uncertainty quantification from OMI data | Kauppi, Anu, Kolmonen, Pekka, Laine, Marko, Tamminen, Johanna | Aerosol Optical Depth/Thickness, Solar Irradiance, Visible Radiance, Aerosol Extinction, Aerosol Optical Depth/Thickness, Aerosol Optical Depth/Thickness, Cloud Fraction, Cloud Top Pressure, Aerosol Extinction, Aerosol Optical Depth/Thickness, ULTRAVIOLET RADIANCE | |
| In-flight performance of the Ozone Monitoring Instrument | Schenkeveld, V. M. Erik, Jaross, Glen, Marchenko, Sergey, Haffner, David, Kleipool, Quintus L., Rozemeijer, Nico C., Veefkind, J. Pepijn, Levelt, Pieternel F. | Visible Radiance, ULTRAVIOLET RADIANCE, Solar Irradiance, Aerosol Optical Depth/Thickness, Atmospheric Ozone, Reflectance, Cloud Fraction, Cloud Top Pressure | |
| Characterization of ozone in the lower troposphere during the 2016 G20 conference in Hangzhou | Su, Wenjing, Liu, Cheng, Hu, Qihou, Fan, Guangqiang, Xie, Zhouqing, Huang, Xin, Zhang, Tianshu, Chen, Zhenyi, Dong, Yunsheng, Ji, Xiangguang, Liu, Haoran, Wang, Zhuang, Liu, Jianguo | Carbon And Hydrocarbon Compounds, Visible Radiance | |
| An improved retrieval of tropospheric NO2 from space over polluted regions using an Earth radiance reference | Anand, J. S., Monks, P. S., Leigh, R. J. | Cloud Fraction, Cloud Top Pressure, Solar Irradiance, Nitrogen Dioxide, Visible Radiance | |
| Observation of slant column NO2 using the super-zoom mode of AURA-OMI | Valin, L. C., Russell, A. R., Bucsela, E. J., Veefkind, J. P., Cohen, R. C. | Visible Radiance | |
| Data processing and in-flight calibration systems for OMI-EOS-Aura | van den Oord, G. H. J., Dobber, M., van de Vegte, J., van der Neut, I., Som de Cerff, W., Rozemeijer, N. C., Schenkelaars, V., ter Linden, M. | Solar Irradiance, Visible Radiance, ULTRAVIOLET RADIANCE | |
| Atmospheric products from the ozone monitoring instrument (OMI) | Ahmad, Suraiya P., Levelt, Pieternel F., Bhartia, Pawan K., Hilsenrath, Ernest, Leppelmeier, Gilbert W., Johnson, James E. | Atmospheric Ozone, Reflectance, Aerosol Optical Depth/Thickness, Visible Radiance, ULTRAVIOLET RADIANCE, Atmospheric Ozone, Reflectance, Nitrogen Dioxide, Atmospheric Ozone, Sulfur Dioxide, Bromine Monoxide, Aerosol Extinction, Aerosol Optical Depth/Thickness, Aerosol Optical Depth/Thickness, Cloud Fraction, Cloud Top Pressure, Chlorine Dioxide, Carbon And Hydrocarbon Compounds, Solar Irradiance |