Sea Ice Dynamics Induced by External Stochastic Fluctuations

The influence of stochastic fluctuations in the atmosphere and in the ocean caused by different occasional phenomena (noises) on dynamic processes of sea ice growth with a mushy layer is studied. It is shown that atmospheric temperature variances substantially increase the sea ice thickness, whereas...

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Bibliographic Details
Published in:Pure and Applied Geophysics
Main Authors: Alexandrov, D. V., Bashkirtseva, I. A., Malygin, A. P., Ryashko, L. B.
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
FALSE BOTTOM
MUSHY LAYER
NONLINEAR DYNAMICS
SEA ICE
STOCHASTIC FLUCTUATIONS
DISPERSION VARIATION
ON DYNAMICS
SEA ICE DYNAMICS
SEA ICE GROWTH
SEA-ICE THICKNESS
STOCHASTIC FLUCTUATION
DYNAMICS
STOCHASTIC SYSTEMS
AIR TEMPERATURE
ICE THICKNESS
STOCHASTICITY
TEMPERATURE EFFECT
TURBULENT FLOW
Sea ice
Online Access:http://elar.urfu.ru/handle/10995/27378
http://www.scopus.com/inward/record.url?partnerID=8YFLogxK&scp=84887559702
https://doi.org/10.1007/s00024-013-0664-z
Description
Summary:The influence of stochastic fluctuations in the atmosphere and in the ocean caused by different occasional phenomena (noises) on dynamic processes of sea ice growth with a mushy layer is studied. It is shown that atmospheric temperature variances substantially increase the sea ice thickness, whereas dispersion variations of turbulent flows in the ocean to a great extent decrease the ice content produced by false bottom evolution. © 2013 Springer Basel.

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