Atmospheric nitrogen oxides (NO and NO 2 ) at Dome C, East Antarctica, during the OPALE campaign
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Howard K. Roscoe | Michel Legrand | Markus M. Frey | Martin D. King | M. Frey | H. Roscoe | M. Legrand | M. King | J. Savarino | Suzanne Preunkert | Joel Savarino | Alexandre Kukui | S. Preunkert | A. Kukui
[1] James D. Lee,et al. Summertime NO x measurements during the CHABLIS campaign: can source and sink estimates unravel observed diurnal cycles? , 2009 .
[2] Arnold F. Moene,et al. The principles of surface flux physics: theory, practice and description of the ECPACK library , 2004 .
[3] J. Lee-Taylor,et al. Extinction of UV‐visible radiation in wet midlatitude (maritime) snow: Implications for increased NOx emission , 2005 .
[4] C. Genthon,et al. The surface layer observed by a high-resolution sodar at DOME C, Antarctica , 2014 .
[5] A. Jones,et al. Modelling photochemical NOX production and nitrate loss in the upper snowpack of Antarctica , 2002 .
[6] J. C. Kaimal,et al. Atmospheric boundary layer flows , 1994 .
[7] J. Lee-Taylor,et al. The importance of considering depth-resolved photochemistry in snow: a radiative-transfer study of NO2 and OH production in Ny-Ålesund (Svalbard) snowpacks , 2010, Journal of Glaciology.
[8] M. Frey,et al. Oxygen isotope mass balance of atmospheric nitrate at Dome C, East Antarctica, during the OPALE campaign , 2015 .
[9] H. Lenschow. Micrometeorological techniques for measuring biosphere-atmosphere trace gas exchange , 1995 .
[10] M. Frey,et al. Large mixing ratios of atmospheric nitrous acid (HONO) at Concordia (East Antarctic Plateau) in summer: a strong source from surface snow? , 2014 .
[11] Jennie L. Thomas,et al. The influence of snow grain size and impurities on the vertical profiles of actinic flux and associated NO x emissions on the Antarctic and Greenland ice sheets , 2012 .
[12] Christopher W. Fairall,et al. Boundary-layer dynamics and its influence on atmospheric chemistry at Summit, Greenland , 2007 .
[13] Bernhard Mayer,et al. Atmospheric Chemistry and Physics Technical Note: the Libradtran Software Package for Radiative Transfer Calculations – Description and Examples of Use , 2022 .
[14] J. Dibb,et al. Photochemical production of gas phase NO x from ice crystal NO3 , 2000 .
[15] M. Frey,et al. Contrasting atmospheric boundary layer chemistry of methylhydroperoxide (CH 3 OOH) and hydrogen peroxide (H 2 O 2 ) above polar snow , 2009 .
[16] C. Genthon,et al. Characterization of the boundary layer at Dome C (East Antarctica) during the OPALE summer campaign , 2014 .
[17] Mark Z. Jacobson,et al. Fundamentals of atmospheric modeling , 1998 .
[18] D. Lenschow,et al. Observations of summertime NO fluxes and boundary-layer height at the South Pole during ISCAT 2000 using scalar similarity , 2004 .
[19] M. Johnson,et al. Isotopic effects of nitrate photochemistry in snow: a field study at Dome C, Antarctica , 2014 .
[20] P. Shepson,et al. Is the Arctic Surface Layer a Source and Sink of NOx in Winter/Spring? , 2000 .
[21] W. Neff,et al. A study of boundary layer behavior associated with high NO concentrations at the South Pole using a minisodar, tethered balloon, and sonic anemometer , 2008 .
[22] M. Frey,et al. The diurnal variability of atmospheric nitrogen oxides (NO and NO 2 ) above the Antarctic Plateau driven by atmospheric stability and snow emissions , 2012 .
[23] R. Stull. An Introduction to Boundary Layer Meteorology , 1988 .
[24] B. Jourdain,et al. Year‐round record of surface ozone at coastal (Dumont d'Urville) and inland (Concordia) sites in East Antarctica , 2009 .
[25] M. Frey,et al. Snow optical properties at Dome C (Concordia), Antarctica; implications for snow emissions and snow chemistry of reactive nitrogen , 2011 .
[26] C. Anastasio,et al. Quantum Yields of Hydroxyl Radical and Nitrogen Dioxide from the Photolysis of Nitrate on Ice , 2003 .
[27] Xiong Liu,et al. A new interpretation of total column BrO during Arctic spring , 2010 .
[28] M. Frey,et al. Air–snow transfer of nitrate on the East Antarctic Plateau – Part 1: Isotopic evidence for a photolytically driven dynamic equilibrium in summer , 2012 .
[29] S. Oltmans,et al. Evidence for photochemical production of ozone at the South Pole surface , 2001 .
[30] D. Lenschow,et al. South Pole NOx Chemistry: an assessment of factors controlling variability and absolute levels , 2004 .
[31] Philip S. Anderson,et al. Measurements of NOx emissions from the Antarctic snowpack , 2001 .
[32] F. Hendrick,et al. Characterisation of vertical BrO distribution during events of enhanced tropospheric BrO in Antarctica, from combined remote and in-situ measurements , 2014 .
[33] Nicolas Theys,et al. Global observations of tropospheric BrO columns using GOME-2 satellite data , 2010 .
[34] S. Argentini,et al. Contrasts between the summertime surface energy balance and boundary layer structure at Dome C and Halley stations, Antarctica , 2006 .
[35] W. Simpson,et al. Radiation-transfer modeling of snow-pack photochemical processes during ALERT 2000 , 2002 .
[36] M. Frey,et al. Photolysis imprint in the nitrate stable isotope signal in snow and atmosphere of East Antarctica and implications for reactive nitrogen cycling , 2009 .
[37] A. Jones,et al. An analysis of the oxidation potential of the South Pole boundary layer and the influence of stratospheric ozone depletion , 2003 .
[38] D. Blake,et al. Results from the ANTCI 2005 Antarctic Plateau Airborne Study , 2010 .
[39] M. Johnson,et al. Laboratory study of nitrate photolysis in Antarctic snow. I. Observed quantum yield, domain of photolysis, and secondary chemistry. , 2014, The Journal of chemical physics.
[40] M. Frey,et al. Atmospheric hydroperoxides in West Antarctica: Links to stratospheric ozone and atmospheric oxidation capacity , 2005 .
[41] R. Honrath,et al. Observations of rapid photochemical destruction of ozone in snowpack interstitial air , 2001 .
[42] Y. Wanga,et al. Assessing the photochemical impact of snow NO x emissions over Antarctica during ANTCI 2003 , 2007 .
[43] S. Madronich,et al. Calculation of actinic fluxes with a coupled atmosphere-snow radiative transfer model , 2002 .
[44] G. Ancellet,et al. Oxidant Production over Antarctic Land and its Export (OPALE) project: An overview of the 2010–2011 summer campaign , 2012 .
[45] Philip S. Anderson,et al. Boundary layer physics over snow and ice , 2007 .
[46] J. Dibb,et al. Release of NOx from sunlight‐irradiated midlatitude snow , 2000 .
[47] I. Gorodetskaya,et al. Validation of a limited area model over Dome C, Antarctic Plateau, during winter , 2008 .
[48] Yuhang Wang,et al. Assessing the photochemical impact of snow NOx emissions over Antarctica during ANTCI 2003 , 2007 .
[49] M. Frey,et al. Measurements of OH and RO 2 radicals at Dome C, East Antarctica , 2014 .
[50] L. Kramer,et al. Evaluation of Boundary Layer Depth Estimates at Summit Station, Greenland , 2013 .
[51] K. Steffen,et al. Vertical fluxes of NOx, HONO, and HNO3 above the snowpack at Summit, Greenland , 2002 .
[52] D. Blake,et al. A reassessment of Antarctic plateau reactive nitrogen based on ANTCI 2003 airborne and ground based measurements , 2008 .