Observations of large reductions in the NO/NOy ratio near the mid‐latitude tropopause and the role of heterogeneous chemistry
暂无分享,去创建一个
James E. Dye | Stephan R. Kawa | R. M. Stimpfle | David W. Fahey | Ross J. Salawitch | Haflidi H. Jonsson | Paul O. Wennberg | M. H. Proffitt | Ronald C. Cohen | Eric J. Hintsa | K. K. Kelly | D. Fahey | R. Cohen | K. Kelly | H. Jonsson | D. Baumgardner | E. Woodbridge | R. Salawitch | P. Wennberg | M. Loewenstein | J. Podolske | E. Keim | J. Wilson | E. Hintsa | J. Dye | M. Proffitt | S. Kawa | R. Stimpfle | R. Gao | K. R. Chan | Max Loewenstein | Darrel Baumgardner | J. R. Podolske | James C. Wilson | E. L. Woodbridge | E. R. Keim | L. A. Del Negro | R. S. Gao | L. D. Negro
[1] S. W. Bowen,et al. In situ observations in aircraft exhaust plumes in the lower stratosphere at midlatitudes , 1995 .
[2] S. Wofsy,et al. Removal of Stratospheric O3 by Radicals: In Situ Measurements of OH, HO2, NO, NO2, ClO, and BrO , 1994, Science.
[3] D. Fahey,et al. Estimates of total organic and inorganic chlorine in the lower stratosphere from in situ and flask measurements during AASE II , 1995 .
[4] R. Cohen,et al. In Situ Measurements of OH and HO_2 in the Upper Troposphere and Stratosphere , 1995 .
[5] D. Fahey,et al. Stratospheric Meteorological Conditions in the Arctic Polar Vortex, 1991 to 1992 , 1993, Science.
[6] S. Wofsy,et al. In situ measurements constraining the role of sulphate aerosols in mid-latitude ozone depletion , 1993, Nature.
[7] D. Fahey,et al. Reactive nitrogen and its correlation with ozone in the lower stratosphere and upper troposphere , 1993 .
[8] Mark R. Schoeberl,et al. NEw observations of the NOy/N2O correlation in the lower stratosphere , 1993 .
[9] D. Fahey,et al. Evaluating the role of NAT, NAD, and liquid H2SO4/H2O/HNO3 solutions in Antarctic polar stratospheric cloud aerosol: Observations and implications , 1997 .
[10] D. Fahey,et al. Photochemical partitioning of the reactive nitrogen and chlorine reservoirs in the high-latitude stratosphere , 1992 .
[11] S. W. Bowen,et al. The distribution of hydrogen, nitrogen, and chlorine radicals in the lower stratosphere: Implications for changes in O3 due to emission of NOy from supersonic aircraft , 1994 .
[12] D. R. Hanson,et al. Differences in the reactivity of type I polar stratospheric clouds depending on their phase , 1996 .
[13] B. Luo,et al. An analytic expression for the composition of aqueous HNO3‐H2SO4 stratospheric aerosols including gas phase removal of HNO3 , 1995 .
[14] D. R. Hanson,et al. Reactive Uptake of ClONO2 onto Sulfuric Acid Due to Reaction with HCl and H2O , 1994 .
[15] M. Patrick McCormick,et al. The poleward dispersal of Mount Pinatubo volcanic aerosol , 1993 .
[16] D. Fahey,et al. Are models of catalytic removal of O3 by HOx accurate? Constraints from in situ measurements of the OH to HO2 ratio , 1994 .
[17] S. Wofsy,et al. Emission Measurements of the Concorde Supersonic Aircraft in the Lower Stratosphere , 1995, Science.
[18] D. Fahey,et al. In situ measurements of total reactive nitrogen, total water, and aerosol in a polar stratospheric cloud in the Antarctic , 1989 .
[19] J. Foot. Aircraft measurements of the humidity in the lower stratosphere from 1977 to 1980 between 45°N and 65°N , 1984 .
[20] E. Weinstock,et al. Mechanisms controlling water vapor in the lower stratosphere: “A tale of two stratospheres” , 1995 .
[21] S. Solomon,et al. Ozone destruction through heterogeneous chemistry following the eruption of El Chichón , 1989 .