The statistical properties of sea ice velocity fields
By arguing that the surface pressure field over the Arctic Ocean can be treated as an isotropic, stationary, homogeneous, Gaussian random field, Thorndike estimated a number of covariance functions from two years of data (1979 and 1980). Given the active interest in changes of general circulation qu...
Main Authors: | , |
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Format: | Text |
Language: | unknown |
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arXiv
2016
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Online Access: | https://dx.doi.org/10.48550/arxiv.1608.08340 https://arxiv.org/abs/1608.08340 |