The ozone monitoring instrument

By Pieternel F. Levelt, Gijsbertus H. J. van den Oord, M. Dobber, A. Mälkki, H. Visser, J. D. Vries, Piet Stammes, J.O.V. Lundell, Heikki Saari. IEEE Transactions on Geoscience and Remote Sensing, 2006

1,924 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/3f388e9dc2e804c3f5d1635dc98914d791c97013

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Citations in the corpus

Anthropogenic emissions of highly reactive volatile organic compounds in eastern Texas inferred from oversampling of satellite (OMI) measurements of HCHO columns (2014, methodology): “OMI is a UV/Vis nadir solar backscatter spectrometer launched in 2004 on the Aura satellite (Levelt et al 2006).”
Updated Smithsonian Astrophysical Observatory Ozone Monitoring Instrument (SAO OMI) formaldehyde retrieval (2015, methodology): “OMI (Levelt et al., 2006) was launched on 15 July 2004 onboard the NASA Earth Observing System (EOS) Aura platform into a Sun-synchronous polar orbit with an average altitude of 705 km and a period of 99 min, giving 14.”
Validation of Ozone Monitoring Instrument total ozone column measurements using Brewer and Dobson spectrophotometer ground‐based observations (2007, methodology): “Validation of Ozone Monitoring Instrument total ozone column measurements using Brewer and Dobson spectrophotometer ground- based observations D. Balis,1 M. Kroon,2 M. E. Koukouli,1 E. J. Brinksma,2 G. Labow,3 J. P. Veefkind,2 and R. D. McPeters3 Received 13 April 2007; revised 13 September 2007;…”
An advanced scattered moonlight model for Cerro Paranal (2013, methodology): “We then scaled it to the values from OMI (Levelt et al. 2006) at the three provided wavelengths for the region around Cerro Paranal.”
Recent reduction in NOx emissions over China: synthesis of satellite observations and emission inventories (2016, background): “TheOzoneMonitoring Instrument (OMI) is a UV–vis nadir-viewing satellite spectrometer (Levelt et al 2006) on board the Aura satellite (Celarier et al 2008) that was launched in 2004.”
Band residual difference algorithm for retrieval of SO/sub 2/ from the aura ozone monitoring instrument (OMI) (2006, methodology): “OMI measured N -value spectra difference inside and outside the Anatahan volcanic plume on April 7, 2005 (orbit 3871) overlapped with a scaled SO cross section [25] smoothed with the nominal OMI UV-2 slit function (triangular, FWHM = 0:45 nm [18]).”
Space‐based constraints on the production of nitric oxide by lightning (2007, background): “[40] We have analyzed space-based observations of tropospheric NO2 columns from SCIAMACHY over 2003– 2005, tropospheric O3 columns from OMI and MLS over 2004–2005, and upper tropospheric HNO3 from ACE-FTS over 2004–2006 to provide top-down constraints on lightning NOx emissions.”
Overview of the EOS aura mission (2006, background): “Aura MLS continues the successful effort of UARS MLS [16] using advanced technology to provide new measurements.”
Optimized regional and interannual variability of lightning in a global chemical transport model constrained by LIS/OTD satellite data (2012, neutral): “…developed by Ziemke et al. [2006], who subtracted coincident measurements of stratospheric ozone made by the Microwave Limb Sounder (MLS) [ Waters et al. , 2006] from total column ozone measurements made by the Ozone Monitoring Instrument (OMI) [ Levelt et al. , 2006], both on the Aura satellite.”
The global lightning-induced nitrogen oxides source (2007, methodology): “, 1999), and OMI (Levelt et al., 2006); GOME-2 on METOP was launched recently, see Table 5.”
Retrieval of large volcanic SO2 columns from the Aura Ozone Monitoring Instrument: Comparison and limitations (2007, background): “Dutch-Finnish Ozone Monitoring Instrument (OMI) [Levelt et al., 2006], launched on the EOS/Aura platform in July 2004, is continuing and expanding these records that are invaluable to both atmospheric scientists and volcanologists [Krotkov et al.”
A fast and sensitive new satellite SO2 retrieval algorithm based on principal component analysis: Application to the ozone monitoring instrument (2013, background): “Among them is the Ozone Monitoring Instrument (OMI), a Dutch-Finnish sensor flying on NASA’s Aura spacecraft that provides daily global coverage at high spatial resolution (13 24 km2 at nadir) [Levelt et al., 2006].”
The Earth observing system microwave limb sounder (EOS MLS) on the aura Satellite (2006, neutral): “The ~1 s difference between the ends of the THz and GHz scans is to reduce power transients when mirrors move quickly during retrace. ta ng en t h t ( km ) time (seconds from arbitrary zero) THz GHz TABLE VI DETAILS OF THE NOMINAL GHZ AND THZ LIMB SCANS GHz scan THz scan tangent height range (km) MI”
Unprecedented Arctic ozone loss in 2011 (2011, methodology): “Total column ozone is measured by the Dutch-Finnish Ozone Monitoring Instrument (OMI”