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...

Full description

Bibliographic Details
Main Authors: Agarwal, Sahil, Wettlaufer, John S.
Format: Text
Language:unknown
Published: arXiv 2016
Subjects:
Eie
Online Access:https://dx.doi.org/10.48550/arxiv.1608.08340
https://arxiv.org/abs/1608.08340