首页 | 本学科首页   官方微博 | 高级检索  
   检索      


On the problem of a connection between ozone dynamics at high latitudes and magnetospheric processes
Institution:1. Max-Planck-Institut für Aeronomie, 3411 KatlenburgLindau, Germany;2. Arctic and Antarctic Research Institute, 38 Bering Street. St Petersburg, 199226, Russia;1. Korea Astronomy and Space Science Institute, 776, Daedeokdae-ro, Youseong-gu, Daejeon, Republic of Korea;2. University of Science and Technology, Daejeon, Republic of Korea;1. Key Laboratory of Digital Earth Science, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100094, China;2. International Research Center of Big Data for Sustainable Development Goals, Beijing 100094, China;3. Univerisity of Chinese Academy of Sciences, Beijing 100049, China;4. Instituto de Astrofísica de Canarias, Vía Láctea s/n, La Laguna, 38205 Tenerife, Spain;5. Departamento de Astrofísica, Universidad de La Laguna, La Laguna, 38206 Tenerife, Spain;1. Department of Civil Engineering, G H Raisoni Institute of Engineering and Technology, Nagpur 440016, India;2. Department of Civil Engineering, Visvesvaraya National Institute of Technology, Nagpur 440010, India
Abstract:Two data sets of ozone density measurements over a wide latitudinal range in the Arctic during summer and winter seasons arc presented. It is shown that geophysical effects manifest themselves in the O3 dynamics in the high latitude region under various circumstances. Therefore a type of total ozone content diurnal variation is a distinctive feature in the auroral oval as well as the polar cap and must be taken into account in any full model of ozone dynamics in the polar regions.
Keywords:
本文献已被 ScienceDirect 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号