Yanayin sararin samaniya

Space climate
Sake gina aikin hasken rana sama da shekaru 11,400. Lokaci na aiki mai girma sama da shekaru 8,000 da suka gabata.  

yanayi sararin samaniya shine bambancin dogon lokaci a cikin aikin hasken rana a cikin heliosphere, gami da iskar hasken rana, filin magnetic na Interplanetary (IMF), da tasirin su a cikin yanayin kusa da Duniya, gami na Magnetosphere na Duniya da ionosphere, sama da ƙasa, yanayi, yanayi, da sauran tsarin da suka danganci. Nazarin kimiyya na yanayin sararin samaniya wani bangare ne na ilimin kimiyyar sararin samaniya, kimiyyar hasken rana, Helio-physics, da geophysics. Don haka yana da alaƙa da ilimin yanayi na ƙasa, kuma ana la'akari da tasirinsa a kan Yanayin Duniya a cikin kimiyyar yanayi.[1][2][3]

  1. Mursula, K.; Usoskin, I.G.; Maris, G. (January 2007). "Introduction to Space Climate" (PDF). Advances in Space Research. 40 (7): 885–887. Bibcode:2007AdSpR..40..885M. doi:10.1016/j.asr.2007.07.046. ISSN 0273-1177.
  2. González Hernández, I.; Komm, R.; Pevstsov, A.; Leibacher, J (2014). "Solar Origins of Space Weather and Space Climate: Preface". Solar Physics. 289 (2): 437–439. Bibcode:2014SoPh..289..437G. doi:10.1007/s11207-013-0454-x.
  3. Lockwood, M.; et al. (2017). "Space climate and space weather over the past 400 years: 1. The power input to the magnetosphere". J. Space Weather Space Climate. 7: A25. arXiv:1708.04904. Bibcode:2017JSWSC...7A..25L. doi:10.1051/swsc/2017019. S2CID 37433045.

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