Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean Sea

In this paper, the impact of assimilating Temperature (T) and Salinity (S) profiles from Argo floats in the Mediterranean Sea is quantitatively investigated using the Observing System Simulation Experiments (OSSE) approach. The impact of varying the number of floats and their launch positions is con...

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Main Authors: A. Griffa, A. Molcard, F. Raicich, V. Rupolo
Format: Article
Language:English
Published: Copernicus Publications 2006-01-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/2/237/2006/os-2-237-2006.pdf
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spelling doaj-73e84293351e4c1a916ad3bf23adc1972020-11-25T02:28:47ZengCopernicus PublicationsOcean Science1812-07841812-07922006-01-0122237248Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean SeaA. GriffaA. GriffaA. MolcardF. RaicichV. RupoloIn this paper, the impact of assimilating Temperature (T) and Salinity (S) profiles from Argo floats in the Mediterranean Sea is quantitatively investigated using the Observing System Simulation Experiments (OSSE) approach. The impact of varying the number of floats and their launch positions is considered, using numerical simulations with a MOM model and a reduced-order multivariate Optimal Interpolation scheme (SOFA) for assimilation. Realistic float coverage and launch positions used during the first MFSTEP phase are considered, as well as "ideal" density coverage that can be envisioned for the future, corresponding to a double coverage with respect to MFSTEP and with floats released along the VOS tracks. The most effective float trajectories are identified, showing that frontal regions play a major role, and that it is crucial to maintain a sufficient coverage of them. In addition to this, a comparison is also performed between the results obtained from MEDARGO floats in ideal conditions and results from "ideal" profiles taken at fixed points along the VOS tracks, as for the XBT data. For consistency the coverage considered is double the actual XBT coverage during MFSTEP, resulting in a threefold increase in the number of profiles compared to the MEDARGO experiment. The maximum error reduction is of approximately 10%, suggesting that spatially coarser profiles from floats can be more efficient since they follow flow features.http://www.ocean-sci.net/2/237/2006/os-2-237-2006.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Griffa
A. Griffa
A. Molcard
F. Raicich
V. Rupolo
spellingShingle A. Griffa
A. Griffa
A. Molcard
F. Raicich
V. Rupolo
Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean Sea
Ocean Science
author_facet A. Griffa
A. Griffa
A. Molcard
F. Raicich
V. Rupolo
author_sort A. Griffa
title Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean Sea
title_short Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean Sea
title_full Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean Sea
title_fullStr Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean Sea
title_full_unstemmed Assessment of the impact of TS assimilation from ARGO floats in the Mediterranean Sea
title_sort assessment of the impact of ts assimilation from argo floats in the mediterranean sea
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2006-01-01
description In this paper, the impact of assimilating Temperature (T) and Salinity (S) profiles from Argo floats in the Mediterranean Sea is quantitatively investigated using the Observing System Simulation Experiments (OSSE) approach. The impact of varying the number of floats and their launch positions is considered, using numerical simulations with a MOM model and a reduced-order multivariate Optimal Interpolation scheme (SOFA) for assimilation. Realistic float coverage and launch positions used during the first MFSTEP phase are considered, as well as "ideal" density coverage that can be envisioned for the future, corresponding to a double coverage with respect to MFSTEP and with floats released along the VOS tracks. The most effective float trajectories are identified, showing that frontal regions play a major role, and that it is crucial to maintain a sufficient coverage of them. In addition to this, a comparison is also performed between the results obtained from MEDARGO floats in ideal conditions and results from "ideal" profiles taken at fixed points along the VOS tracks, as for the XBT data. For consistency the coverage considered is double the actual XBT coverage during MFSTEP, resulting in a threefold increase in the number of profiles compared to the MEDARGO experiment. The maximum error reduction is of approximately 10%, suggesting that spatially coarser profiles from floats can be more efficient since they follow flow features.
url http://www.ocean-sci.net/2/237/2006/os-2-237-2006.pdf
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