Direct Sun measurements of NO2 column abundances from Table Mountain, California: Intercomparison of low- and high-resolution spectrometers
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Jay R. Herman | G. H. Mount | Stanley P. Sander | Alexander Cede | J. Herman | S. Sander | T. Pongetti | A. Cede | G. Mount | E. Spinei | S. Wang | Thomas J. Pongetti | Elena Spinei | S. Wang
[1] J. Burrows,et al. Measurements of nitrogen dioxide total column amounts using a Brewer double spectrophotometer in direct Sun mode , 2006 .
[2] John P. Burrows,et al. MAX-DOAS measurements of atmospheric trace gases in Ny- ˚ Alesund - Radiative transfer studies and their application , 2004 .
[3] K. F. Boersma,et al. Near-real time retrieval of tropospheric NO 2 from OMI , 2006 .
[4] A. Elokhov,et al. Slant Column Measurements of O3 and NO2 During the NDSC Intercomparison of Zenith-Sky UV-Visible Spectrometers in June 1996 , 1999 .
[5] U. Platt,et al. Ground‐based measurements of halogen oxides at the Hudson Bay by active longpath DOAS and passive MAX‐DOAS , 2004 .
[6] Glen Jaross,et al. Validation of Ozone Monitoring Instrument level 1b data products , 2008 .
[7] V. K. Semenov,et al. Ground‐based validation of EOS‐Aura OMI NO2 vertical column data in the midlatitude mountain ranges of Tien Shan (Kyrgyzstan) and Alps (France) , 2008 .
[8] D. Fahey,et al. Reactive nitrogen and its correlation with ozone in the lower stratosphere and upper troposphere , 1993 .
[9] P. Crutzen. The influence of nitrogen oxides on the atmospheric ozone content , 1970 .
[10] 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 .
[11] J. Margolis,et al. OH column abundance over Table Mountain Facility, California: AM‐PM diurnal asymmetry , 2005 .
[12] S. Sander,et al. Atmospheric hydroxyl radical (OH) abundances from ground-based ultraviolet solar spectra: an improved retrieval method. , 2008, Applied optics.
[13] S. Inomata,et al. Doppler detection of hydroxyl column abundance in the middle atmosphere , 1995 .
[14] James F. Gleason,et al. Algorithm for NO/sub 2/ vertical column retrieval from the ozone monitoring instrument , 2006, IEEE Transactions on Geoscience and Remote Sensing.
[15] K. Jucks,et al. Validation of Aura Microwave Limb Sounder OH measurements with Fourier Transform Ultra‐Violet Spectrometer total OH column measurements at Table Mountain, California , 2008 .
[16] D. York. Least-squares fitting of a straight line. , 1966 .
[17] S. Wofsy,et al. Tropospheric chemistry: A global perspective , 1981 .
[18] K. Boersma,et al. Trends, seasonal variability and dominant NOx source derived from a ten year record of NO2 measured from space , 2008 .
[19] James F. Gleason,et al. Validation of OMI tropospheric NO2 column densities using direct‐Sun mode Brewer measurements at NASA Goddard Space Flight Center , 2008 .
[20] P. F. Levelt,et al. Near-real time retrieval of tropospheric NO from OMI , 2007 .
[21] Ulrich Platt,et al. Differential optical absorption spectroscopy , 2008 .
[22] Jerald W. Harder,et al. Temperature dependent NO2 cross sections at high spectral resolution , 1997 .
[23] J. Veefkind,et al. Validation of Ozone Monitoring Instrument nitrogen dioxide columns , 2008 .
[24] Dimitris Balis,et al. Validation of the Aura Ozone Monitoring Instrument total column ozone product , 2008 .
[25] V. Nemtchinov,et al. OH column abundance over Table Mountain Facility, California: Annual average 1997–2000 , 2002 .
[26] Bernd Jähne,et al. Retrieval and analysis of stratospheric NO2 from the Global Ozone Monitoring Experiment , 2004 .
[27] J. Kerr,et al. Nitrogen Dioxide Concentrations in the Atmosphere , 1973, Nature.
[28] L. Brown,et al. Temperature and Pressure Dependence of High-Resolution Air-Broadened Absorption Cross Sections of NO2 (415−525 nm) , 2004 .
[29] B. Cameron Reed,et al. Linear least‐squares fits with errors in both coordinates , 1989 .
[30] V. Nemtchinov,et al. High-Resolution Fourier-Transform Ultraviolet-Visible Spectrometer for the Measurement of Atmospheric Trace Species: Application to OH. , 2001, Applied optics.
[31] Paul S. Monks,et al. Comparison of OMI and ground‐based in situ and MAX‐DOAS measurements of tropospheric nitrogen dioxide in an urban area , 2008 .
[32] B. Cameron Reed,et al. Linear least‐squares fits with errors in both coordinates. II: Comments on parameter variances , 1992 .
[33] J. Seinfeld,et al. Atmospheric Chemistry and Physics: From Air Pollution to Climate Change , 1997 .
[34] Henk Eskes,et al. Estimates of lightning NO x production from GOME satellite observations , 2005 .
[35] Philip J. Rasch,et al. MOZART, a global chemical transport model for ozone and related chemical tracers: 1. Model description , 1998 .