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Meridional heat transport at the onset of winter stratospheric warmingA continuous vertical flow of energy toward high altitude was verified. This process produced a dynamic instability of the stratospheric polar vortex. A meridional heat transport ws primed toward the north, which generated a warming trend.
Document ID
19820003824
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Conte, M. (NASA Headquarters Washington, DC United States)
Date Acquired
September 4, 2013
Publication Date
September 1, 1981
Subject Category
Geophysics
Report/Patent Number
NASA-TM-76614
Accession Number
82N11697
Funding Number(s)
CONTRACT_GRANT: NASW-3541
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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