Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic Sea

This paper describes the near-surface transport properties and Lagrangian statistics in the Adriatic semi-enclosed basin using synthetic drifters. Lagrangian transport models were used to simulate synthetic trajectories from the mean flow fields obtained by the Massachusetts Institute of Technology...

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Main Author: Saeed Hariri
Format: Article
Language:English
Published: MDPI AG 2020-09-01
Series:Journal of Marine Science and Engineering
Subjects:
Online Access:https://www.mdpi.com/2077-1312/8/9/681
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spelling doaj-14c380f7573a45ebb6cea81902a87ecc2021-04-02T14:00:35ZengMDPI AGJournal of Marine Science and Engineering2077-13122020-09-01868168110.3390/jmse8090681Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic SeaSaeed Hariri0Ifremer, Department of Coastal Environment Dynamics (DYNECO), 29280 Plouzané, FranceThis paper describes the near-surface transport properties and Lagrangian statistics in the Adriatic semi-enclosed basin using synthetic drifters. Lagrangian transport models were used to simulate synthetic trajectories from the mean flow fields obtained by the Massachusetts Institute of Technology general circulation model (MITgcm), implemented in the Adriatic from October 2006 until December 2008. In particular, the surface circulation properties in two contrasting years (2007 had a mild winter and cold fall, while 2008 had a normal winter and hot summer) are compared here. In addition, the Lagrangian statistics for the entire Adriatic Basin after removing the Eulerian mean circulation for numerical particles were calculated. The results indicate that the numerical particles were slower in this simulation when compared with the real drifters. This is because of the reduced energetic flow field generated by the MIT general circulation model during the selected years. The numerical results showed that the balanced effects of the wind-driven recirculation in the northernmost area(which would be a sea response to the Bora wind field) and the Po River discharge cause the residence times to be similar during the two selected years (182 and 185 days in 2007 and 2008, respectively). Furthermore, the mean angular momentum, diffusivity, and Lagrangian velocity covariance values are smaller than in the real drifter observations, while the maximum Lagrangian integral time scale is the same.https://www.mdpi.com/2077-1312/8/9/681Lagrangian statisticsAdriatic OGCMBora wind fieldresidence timesynthetic trajectoriesdrifter observations
collection DOAJ
language English
format Article
sources DOAJ
author Saeed Hariri
spellingShingle Saeed Hariri
Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic Sea
Journal of Marine Science and Engineering
Lagrangian statistics
Adriatic OGCM
Bora wind field
residence time
synthetic trajectories
drifter observations
author_facet Saeed Hariri
author_sort Saeed Hariri
title Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic Sea
title_short Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic Sea
title_full Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic Sea
title_fullStr Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic Sea
title_full_unstemmed Near-Surface Transport Properties and Lagrangian Statistics during Two Contrasting Years in the Adriatic Sea
title_sort near-surface transport properties and lagrangian statistics during two contrasting years in the adriatic sea
publisher MDPI AG
series Journal of Marine Science and Engineering
issn 2077-1312
publishDate 2020-09-01
description This paper describes the near-surface transport properties and Lagrangian statistics in the Adriatic semi-enclosed basin using synthetic drifters. Lagrangian transport models were used to simulate synthetic trajectories from the mean flow fields obtained by the Massachusetts Institute of Technology general circulation model (MITgcm), implemented in the Adriatic from October 2006 until December 2008. In particular, the surface circulation properties in two contrasting years (2007 had a mild winter and cold fall, while 2008 had a normal winter and hot summer) are compared here. In addition, the Lagrangian statistics for the entire Adriatic Basin after removing the Eulerian mean circulation for numerical particles were calculated. The results indicate that the numerical particles were slower in this simulation when compared with the real drifters. This is because of the reduced energetic flow field generated by the MIT general circulation model during the selected years. The numerical results showed that the balanced effects of the wind-driven recirculation in the northernmost area(which would be a sea response to the Bora wind field) and the Po River discharge cause the residence times to be similar during the two selected years (182 and 185 days in 2007 and 2008, respectively). Furthermore, the mean angular momentum, diffusivity, and Lagrangian velocity covariance values are smaller than in the real drifter observations, while the maximum Lagrangian integral time scale is the same.
topic Lagrangian statistics
Adriatic OGCM
Bora wind field
residence time
synthetic trajectories
drifter observations
url https://www.mdpi.com/2077-1312/8/9/681
work_keys_str_mv AT saeedhariri nearsurfacetransportpropertiesandlagrangianstatisticsduringtwocontrastingyearsintheadriaticsea
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