Decorrelation scales for Arctic Ocean hydrography – Part I: Amerasian Basin

Any use of observational data for data assimilation requires adequate information of their representativeness in space and time. This is particularly important for sparse, non-synoptic data, which comprise the bulk of oceanic in situ observations in the Arctic. To quantify spatial and temporal s...

Full description

Bibliographic Details
Main Authors: H. Sumata, F. Kauker, M. Karcher, B. Rabe, M.-L. Timmermans, A. Behrendt, R. Gerdes, U. Schauer, K. Shimada, K.-H. Cho, T. Kikuchi
Format: Article
Language:English
Published: Copernicus Publications 2018-03-01
Series:Ocean Science
Online Access:https://www.ocean-sci.net/14/161/2018/os-14-161-2018.pdf