Abstract
Autoregressive models are fitted to 57 polar low trajectories sampled by satellite and weather maps from The Norwegian Sea neighbourhood at approximately Δt = 3 h intervals. The data tentatively suggest that no velocity model is significantly better than a Brownian. When a low has been observed, the predicted probability of a low encounter is estimated to be significant over an area with 800 km characteristic length and width.
DOI: https://doi.org/10.3402/tellusa.v39i4.11768 | Journal eISSN: 3035-9554
Language: English
Page range: 390 - 396
Submitted on: Jun 13, 1986
Accepted on: Jan 12, 1987
Published on: Jan 1, 1987
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1987 Karl J. Eidsvik, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.
