[1] Brasseur G, Orlando J, Tyndall G S. Atmospheric Chemistry and Global Change[M].Oxford: Oxford University Press,1999. [2] Brasseur G P, Solomon S. Aeronomy of the Middle Atmosphere(2nd ed)[M]. Dordrecht:Reidel D Publishing Co,1986. [3] Solomon S. Progress towards a quantitative understanding of Antractic ozone depletion[J].Nature, 1990,347:347-354. [4] Solomon S, Burkholder J B, Ravishankara A R,et al. On the ozone depletion and global warming potential of CH3I[J].Journal of Geophysical Research, 1994,99:20 929-20 935. [5] Solomon S, Garcia R R, Ravishankara A R. On the role of iodine in ozone depletion[J].Journal of Geophysical Research,1994, 99:20 491-20 499. [6] Newman P A, Kawa S R, Nash E R. On the size of the Antarctic ozone hole?[J].Geophysical Research Letters,2004,31: L12814. [7] Weatherhead E C, Andersen S B. The search for signs of recovery of the ozone layer[J].Nature,2006,441: 39-45. [8] Yang X, Huang R X,Wang D X. Decadal changes of wind stress over the southern Ocean associated with Antarctic Ozone depletion[J].Journal of Climate,2007,20(14): 3 395-3 410. [9] Zhou Xiuji, Luo Chao, Li Weiliang, et al.Ozone content change in China region and ozone valley over Tibetan plateau[J].Chinese Science Bulletin,1995,40(15):1 396-1 398.[周秀骥,罗超,李维亮,等.中国地区臭氧总量变化与青藏高原低值中心[J].科学通报,1995,40(15):1 396-1 396.] [10] Bian Jianchun, Wang Gengchen, Chen Hongbin, et al.Ozone mini-hole occurring over the Tibetan plateau in December 2003[J].Chinese Science Bulletin, 2006, 51(7):885-888.[卞建春,王庚辰,陈洪滨,等. 2003年12月青藏高原上空出现微型臭氧洞[J].科学通报,2006,51(5):606-609.] [11] Liu Yu,Li Weiliang,Zhou Xiuji, et al.Mechanism of formation of the ozone valley over the Tibetan plateau in summer transport and chemical process of ozone[J].Advances in Atmospheric Sciences,2003,20(1):103-109.[刘煜,李维亮, 周秀骥,等.青藏高原夏季臭氧低谷形成的机理——臭氧输送和化学过程[J].大气科学进展,2003,20(1):103-109.] [12] Liu Yu,Li Weiliang .Deepening of ozone valley over Tibetan plateau and its possible influences[J].Acta Meteorologica Sinica, 2001,59(1): 97-106.[刘煜,李维亮.青藏高原臭氧低谷的加深及其可能的影响[J].气象学报,2001,59(1): 97-106.] [13] Crutzen P J. Ozone production rate in an oxygen-hydrogen-nitrogen oxide atmosphere[J].Journal of Geophysical Research, 1975,76:7 311-7 327. [14] Johnston H S. Reduction of stratospheric ozone by nitrogen oxide catalysts from supersonic transport exhaust[J].Science, 1971, 173:517-522. [15] Johnston H S, Kinnison D S, Wuebbles D J. Impact of aircraft and surface emission of nitrogen oxides on tropospheric warming[J].Nature,1992,355:69-71. [16] Schumann U. Air traffic and the environment-background, tendencies and Potential Atmospheric effect[J].Lecture Notes in Engineering, 1990, 60:170. [17] Schumann U. On the effect of emissions from aircraft engines on the state of the atmosphere[J].Annales Geophysicae, 1994,12:365-384. [18] Schumann U. AERONEX-The impact of NOx emissions from aircraft upon the atmosphere at flight altitudes 8-15km[R]. Final report tot CEC, CEC contract EV5V-CT91-0044, Brussels: Office for Publications of the European Commission, 1995:471. [19] Beck J P, Reeves C E. The effect of air traffic emission on tropospheric ozone in the northern hemisphere[J].Atmospheric Environment, 1992, 26A:17-29. [20] Schumann U , Wurzel D. Impact of Emissions from Aircraft and Spacecraft upon the Atmosphere[M]. DLR-Mitteilung,1994. [21] Brasseur G P,Muller J F,Granier C. Atmospheric impact of NOx emissions by subsonic aircraft: A three-dimensional model study[J].Journal of Geophysical Research,1996,101:1 423-1 428. [22] Ehhalt D H, Rohrer F, Wahner A. Sources and distribution of NOx in the upper troposphere at northern mid-latitudes[J]. Journal of Geophysical Research, 1992, 97:3 725-3 738. [23] Fuglestvedt J S, Jonson J E, Isaksen I S A. Effects of reductions in stratospheric ozone on tropospheric chemistry through changes in photolysis rates[J].Tellus,1994,46:172-192. [24] Stevenson D S, Collins W J, Johnson C E, et al. The impact of aircraft nitrogen oxide emissions on tropospheric ozone studied with 3 D lagrangian model including fully diurnal chemistry[J].Atmospheric Environment,1997,31:1 837-1 850. [25] Wauben W M F, Velthoven P F, Kelder H. A 3D chemistry transport model study of changes in atmospheric ozone due to aircraft NOx emissions[J].Atmospheric Environment,1997,31:1 819-1 836. [26] Dameris M, Grewe V, Kohler I,et al. Impact of aircraft NOx emissions on tropospheric and stratospheric ozone,Part II: 3-D model result[J].Atmospheric Environment,1998,32:3 185-3 199. [27] Liu Yu, Isaksen I S A, Sundet J K, et al. Impact of aircraft NOx emission on NOx and ozone over China[J].Advances in Atmospheric Sciences,2003,20(4):365-574. [28] Junge C E, Manson J E. Stratospheric aerosol studies[J].Journal of Geophysical Research,1961, 66: 2 163-2 182. [29] Worsnop D M. Mass accommodation coefficient measurements for, HNO, HCl and N2O5 on water, ice and aqueous sulfuric acid droplet surfaces[M].Polar ozone workshop.National Aeronautics and Space Administration,Snowmass,May,1988. [30] Mozurkewich M, Calvert J G. Reaction probabilities of on N2O5 aqueous aerosols[J]. Journal of Geophysical Research, 1988, 93: 15 889-15 896. [31] Tolbert M A, Rossi M J, Golden D M. Heterogeneous interactions of chlorine nitrate, hydrogen chlorine, and nitric acid with sulfuric acid surfaces at stratospheric temperature[J].Geophysical Research Letters,1988, 15:847-850. [32] Fried A, Henry B E, Calvert J G. The reaction probability of N2O5 with sulfuric acid aerosols at stratospheric temperatures and compositions[J].Journal of Geophysical Research,1994, 99: 3 517-3 532. [33] Hofmann D J, Solomon S. Ozone destruction through heterogeneous chemistry following the eruption of El Chichon[J]. Journal of Geophysical Research, 1989, 94: 5 029-5 041. [34] Rodriguez J M, Malcolm K W K, Nien D S. Role of heterogeneous conversion of N2O5 on sulfuric aerosols in global ozone losses[J]. Nature,1991, 352: 134-137. [35] Granier C, Brasseur G. Impact of heterogeneous chemistry on model predictions of ozone changes[J].Journal of Geophysical Research,1992, 97: 18 015-18 033. [36] WMO. Scientific assessment of ozone depletion: 1991[R].Geneva,1992. [37] Bojkov R D. The international ozone assessment[J].WMO Bulletin,1995, 44: 42-50. [38] Prather M J. Catastrophic loss of stratospheric ozone in dense volcanic clouds[J].Journal of Geophysical Research,1992, 97: 10 187-10 191. [39] McCormick M P, Veiga R E. SAGEⅡ measurement of early Pinatubo aerosols[J].Geophysical Research Letters,1992, 19: 155-158. [40] Yang P, Brasseur G. The Nonlinear Response of Stratospheric Ozone to NOx and ClOx Perturbations[J].Geophysical Research Letters,2001, 28: 717-720. [41] Hanson D R, Mauersberger K. Laboratory studies of the nitric acid trihydrate: Implications for the south polar stratosphere[J].Geophysical Research Letters,1988, 15: 855-858. [42] Hanson D R, Ravishankara A R. The reaction probability of ClNON2 and N2O5 on polar stratospheric cloud materials[J]. Journal of Geophysical Research,1991, 96: 5 081-5 090. [43] Theresa H, Stacy Walters, Guy Brasseur,et al. Description of SOCRATES─A chemical dynamical radiative two-Dimensional model[R].NCAR Technical Note, NCAR/TN-400+EDD,1998. [44] Potter B, Holton E, James R. The role of monsoon convection in the dehydration of the lower tropical stratosphere[J].Journal of the Atmospheric Sciences,1995, 52 (8): 1 034-1 050. [45] Wang Geli ,Yang Peicai. On the nonlinear response of lower stratospheric ozone to NOx and ClOx perturbations for different CH4 sources[J].Advances in Atmospheric Sciences,2006,23(5):750-757. |