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Upper stratospheric ozone decrease events due to a positive feedback between ozone and the ozone dissociation rate

机译：由于臭氧和臭氧解离率之间的正反馈，上层平流层臭氧减少事件

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G. R. Sonnemann; P. Hartogh;
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1. Upper stratospheric ozone decrease events due to a positive feedback between ozone and the ozone dissociation rate [J] . G. R. Sonnemann, P. Hartogh Nonlinear processes in geophysics . 2010,第3期

机译：由于臭氧与臭氧解离速率之间的正反馈，导致平流层上方的臭氧减少事件
2. Stratospheric ozone intrusion events and their impacts on tropospheric ozone in the Southern Hemisphere [J] . Greenslade Jesse W., Alexander Simon P., Schofield Robyn, Atmospheric Chemistry and Physics Discussions . 2017,第17期

机译：平流层臭氧入侵事件及其对南半球对流层臭氧的影响
3. Stratospheric ozone intrusion events and their impacts on tropospheric ozone in the Southern Hemisphere [J] . Greenslade Jesse W., Alexander Simon P., Schofield Robyn, Atmospheric chemistry and physics . 2017,第17期

机译：平流层臭氧入侵事件及其对南半球对流层臭氧的影响
4. Examining the quasibiennial oscillation of total ozone and ozone concentrations at separate stratospheric levels according to data of TOMS satellite instrumentation [C] . O.E. Bazhenov, A.P. Makeev International symposium on atmospheric and ocean optics/atmospheric physics . 2014

机译：根据TOMS卫星仪器的数据，检查平流层水平上总臭氧和臭氧浓度的准双年度振荡
5. Dissociation Rates of Oxygen and Ozone Molecules in the Stratosphere and Mesosphere [D] . Muramatsu, Hisafumi -1

机译：平流层和中层中氧气和臭氧分子的解离速率
6. Improved Global Surface Temperature Simulation using Stratospheric Ozone Forcing with More Accurate Variability [O] . Fei Xie, Jianping Li, Cheng Sun, -1

机译：利用平流层臭氧强迫和更精确的变异性改进了全球表面温度模拟
7. Upper stratospheric ozone decrease events due to a positive feedback between ozone and the ozone dissociation rate [O] . Sonnemann, G., Hartogh, P. 2009

机译：由于臭氧与臭氧解离率之间的正反馈，上层平流层臭氧减少事件
8. Balloon Borne Soundings of Water Vapor, Ozone and Temperature in the Upper Tropospheric and Lower Stratosphere as Part of the Second SAGE III Ozone Loss and Validation Experiment (SOLVE-2) [R] . Voemel, Holger 2004

机译：作为第二次saGE III臭氧损失和验证实验（sOLVE-2）的一部分，对流层上层和下层平流层的水蒸气，臭氧和温度的气球探测

Upper stratospheric ozone decrease events due to a positive feedback between ozone and the ozone dissociation rate

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