平流层下层N2O5和C10NO2的遥感研究

Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques Pub Date : 1988-08-01 DOI:10.1364/lors.1987.tua4

J. Brasunas, J. Herman, V. Kunde, W. Maguire, L. Herath, W. Shaffer, S. Massie, A. Goldman

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摘要

平流层臭氧浓度取决于辐射、化学和动力学的综合作用。化学的核心是氮、氯和氢的催化臭氧破坏循环。验证试图预测臭氧趋势的光化学模型需要同时测量臭氧、温度和参与臭氧破坏的微量物质

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Remote Sensing of N2O5 and C10NO2 in the Lower Stratosphere

The stratospheric ozone concentration depends on a combination of radiation, chemistry and dynamics. Central to the chemistry are the nitrogen, chlorine, and hydrogen cycles of catalytic ozone destruction. Verification of the photochemical models that attempt to predict ozone trends requires the simultaneous measurement of ozone, temperature, and the trace species which participate in the ozone destruction.1

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Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques

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