Abstract
Ozone is a key atmospheric substance for both chemistry and climate. Being a secondary species, its concentration is controlled by a number of different factors, such as precursors’ emission, sunlight and oxidizing agents. Its impact on atmospheric chemistry and radiative balance differs with altitude: in the lower troposphere ozone acts as a toxic pollutant, in the upper troposphere as a greenhouse gas (GHG) and finally in the stratosphere as a protection against harmful ultraviolet (UV) radiation. Ozone is in general a radiatively active gas for both solar (shortwave, SW) and terrestrial (longwave, LW) radiation [14], therefore it’s very important to acquire and understand its radiative impact for climate related studies.
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Acknowledgments
The author would like to acknowledge the contribution of D. Hurtmans, L. Clarisse and P.-F. Coheur [Université Libre de Bruxelles, Belgium (ULB)], C. Clerbaux (LATMOS/IPSL, UPMC Univ. Paris 06 Sorbonne Universités, UVSQ, CNRS, France and ULB), H. M. Worden (Atmospheric Chemistry Observations & Modeling Laboratory, NCAR, USA) and K. W. Bowman (Jet Propulsion Laboratory, USA).
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Doniki, S. (2019). Calculating the O3 Instantaneous Longwave Radiative Impact from Satellite Observations. In: Palocz-Andresen, M., Szalay, D., Gosztom, A., Sípos, L., Taligás, T. (eds) International Climate Protection. Springer, Cham. https://doi.org/10.1007/978-3-030-03816-8_8
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