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Updated: Aug 15, 2026

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface
13:27

Exploring the Effects of Atmospheric Forcings on Evaporation: Experimental Integration of the Atmospheric Boundary Layer and Shallow Subsurface

Published on: June 8, 2015

熱帯と中緯度の下層層層圏間の輸送を定量化する

Volk1, Elkins, Fahey

  • 1C. M. Volk, G. S. Dutton, and J. M. Gilligan are with the Climate Monitoring and Diagnostics Laboratory (CMDL), National Oceanic and Atmospheric Administration (NOAA), Boulder, CO 80303, and the Cooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO 80309, USA. J. W. Elkins is with NOAA/CMDL, Boulder, CO 80303, USA. D. W. Fahey is with the NOAA Aeronomy Laboratory, Boulder, CO 80303, USA. R. J. Salawitch and J. J. Margitan are with the Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA. M. H. Proffitt is with the NOAA Aeronomy Laboratory, Boulder, CO 80303, and CIRES, University of Colorado, Boulder, CO 80309, USA. M. Loewenstein, J. R. Podolske, and K. R. Chan are with the NASA Ames Research Center, Moffett Field, CA 94035, USA. K. Minschwaner is with the Department of Physics, New Mexico Institute of Mining and Technology, Socorro, NM 87801, USA.

Science (New York, N.Y.)
|June 21, 1996
PubMed
まとめ

中緯度の空気は,想定よりもゆっくりと熱帯の平流圏に入り,中緯度のオゾンは工業用塩素に対してより敏感になります. この発見は,オゾン層の減少と超音速航空機の排出量に関する予測に影響を与えます.

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