Remote Sensing of N2O5 and C10NO2 in the Lower Stratosphere

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

doi:10.1364/LORS.1987.TuA4

Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques
Technical Digest Series (Optica Publishing Group, 1987),
paper TuA4
•https://doi.org/10.1364/LORS.1987.TuA4

Remote Sensing of N₂O₅ and C10NO₂ in the Lower Stratosphere

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

Laser and Optical Remote Sensing: Instrumentation and Techniques 1987

North Falmoth, Massachusetts United States
28 September–1 October 1987
ISBN:

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Optical Techniques For Earth System Science (TuA)

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J. Brasunas, J. Herman, V. Kunde, W. Maguire, L. Herath, W. Shaffer, S. Massie, and A. Goldman, "Remote Sensing of N2O5 and C10NO2 in the Lower Stratosphere," in Topical Meeting on Laser and Optical Remote Sensing: Instrumentation and Techniques, Technical Digest Series (Optica Publishing Group, 1987), paper TuA4.

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Abstract

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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