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Observing and Modeling Currents on the Continental Slope: Assimilation of High Frequency Radar Currents and Hydrography Profiles : Volume 11, Issue 3 (04/06/2014)

By Sperrevik, A. K.

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Book Id: WPLBN0004020780
Format Type: PDF Article :
File Size: Pages 34
Reproduction Date: 2015

Title: Observing and Modeling Currents on the Continental Slope: Assimilation of High Frequency Radar Currents and Hydrography Profiles : Volume 11, Issue 3 (04/06/2014)  
Author: Sperrevik, A. K.
Volume: Vol. 11, Issue 3
Language: English
Subject: Science, Ocean, Science
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Historic
Publication Date:
2014
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

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Christensen, K. H., Röhrs, J., & Sperrevik, A. K. (2014). Observing and Modeling Currents on the Continental Slope: Assimilation of High Frequency Radar Currents and Hydrography Profiles : Volume 11, Issue 3 (04/06/2014). Retrieved from http://www.ebooklibrary.org/


Description
Description: Norwegian Meteorological Institute, Oslo, Norway. Assimilation of High Frequency (HF) radar current observations and CTD hydrography is performed with the 4D-Var analysis scheme implemented in the Regional Ocean Modeling System (ROMS). We consider both an idealized case, with a baroclinic slope current in a periodic channel, and a realistic case for the coast of Vesterålen in Northern Norway. In the realistic case the results of the data assimilation are compared with independent data from acoustic profilers and surface drifters. Best results are obtained when background error correlation scales are small (10 km or less) and when the data assimilation window is short, i.e. about one day. Furthermore, we find that the impact of assimilating HF radar currents is generally larger than the impact of CTD hydrography, which implies that the amount of hydrographic data is insufficient to constrain the solution. Combining the HF radar currents with a few hydrographic profiles gives significantly better results, which demonstrates the importance of complementing surface observations with observations of the vertical structure of the ocean.

Summary
Observing and modeling currents on the continental slope: assimilation of high frequency radar currents and hydrography profiles

Excerpt
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