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RV Walton Smith Cruise WS17305, 31 Oct-10 Nov 2017, Miami – Miami. MerMEED microstructure cruise report

RV Walton Smith Cruise WS17305, 31 Oct-10 Nov 2017, Miami – Miami. MerMEED microstructure cruise report
RV Walton Smith Cruise WS17305, 31 Oct-10 Nov 2017, Miami – Miami. MerMEED microstructure cruise report
The MerMEED (Mechanisms responsible for Mesoscale Eddy Energy Dissipation) project is a NERC funded project (NE/N001745/1, 2015–2018) to investigate the levels of dissipation associated with eddies at a western boundary, in order to identify the mechanisms responsible. Mesoscale eddies are ubiquitous in the worlds oceans, and can be found in the subtropical Atlantic travelling slowly westward (at 4–5 cm/s), with a radius of about 100 km. These eddies are formed through baroclinic instability or wind forcing across the Atlantic, but when they reach the western boundary (east coast of the USA), they disappear from the satellite altimetry record. This disappearance of eddies occurs throughout the worlds oceans at western boundaries, but from altimetry alone, it is not known whether they disappear because energy is transferred to other wave modes or the mean flow, or whether it is locally dissipated through eddy-topography interactions. This is the second cruise of the MerMEED project, with the previous being detailed in [Frajka-Williams, 2017]. The purpose of this cruise was to (1) make microstructure temperature and shear measurements in order to measure dissipation at the intersection of an anticyclonic eddy and the steep topography to the east of Abaco, Bahamas, and (2) deploy standard and microstructure Seagliders. Of these, the standard Seagliders were intended to remain in the area for 4 months. During the 10 day cruise, 112 profiles of microstructure data were collected using a tethered microstructure profiler, and a shipboard 75 kHz ADCP collected concurrent measurements of ocean currents. This cruise is the second of several planned cruises for the MerMEED project, and the data collected are intended to complement additional field operations, including moored instruments added to the RAPID array (thermistors and ADCPs on the WB1 mooring) and a second glider deployment in the spring of 2018.
50
National Oceanography Centre
Frajka-Williams, Eleanor
da86044e-0f68-4cc9-8f60-7fdbc4dc19cb
et al,
867c20e9-3220-49c5-b89e-aac82d31ba5e
Frajka-Williams, Eleanor
da86044e-0f68-4cc9-8f60-7fdbc4dc19cb
et al,
867c20e9-3220-49c5-b89e-aac82d31ba5e

Frajka-Williams, Eleanor and et al, (2018) RV Walton Smith Cruise WS17305, 31 Oct-10 Nov 2017, Miami – Miami. MerMEED microstructure cruise report Southampton, GB. National Oceanography Centre 80pp. (National Oceanography Centre Cruise Report, 50) ,

Record type: Monograph (Project Report)

Abstract

The MerMEED (Mechanisms responsible for Mesoscale Eddy Energy Dissipation) project is a NERC funded project (NE/N001745/1, 2015–2018) to investigate the levels of dissipation associated with eddies at a western boundary, in order to identify the mechanisms responsible. Mesoscale eddies are ubiquitous in the worlds oceans, and can be found in the subtropical Atlantic travelling slowly westward (at 4–5 cm/s), with a radius of about 100 km. These eddies are formed through baroclinic instability or wind forcing across the Atlantic, but when they reach the western boundary (east coast of the USA), they disappear from the satellite altimetry record. This disappearance of eddies occurs throughout the worlds oceans at western boundaries, but from altimetry alone, it is not known whether they disappear because energy is transferred to other wave modes or the mean flow, or whether it is locally dissipated through eddy-topography interactions. This is the second cruise of the MerMEED project, with the previous being detailed in [Frajka-Williams, 2017]. The purpose of this cruise was to (1) make microstructure temperature and shear measurements in order to measure dissipation at the intersection of an anticyclonic eddy and the steep topography to the east of Abaco, Bahamas, and (2) deploy standard and microstructure Seagliders. Of these, the standard Seagliders were intended to remain in the area for 4 months. During the 10 day cruise, 112 profiles of microstructure data were collected using a tethered microstructure profiler, and a shipboard 75 kHz ADCP collected concurrent measurements of ocean currents. This cruise is the second of several planned cruises for the MerMEED project, and the data collected are intended to complement additional field operations, including moored instruments added to the RAPID array (thermistors and ADCPs on the WB1 mooring) and a second glider deployment in the spring of 2018.

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Published date: January 2018

Identifiers

Local EPrints ID: 417559
URI: https://eprints.soton.ac.uk/id/eprint/417559
PURE UUID: e7f7dc89-d94e-476e-98c9-2998aa3d9a1b
ORCID for Eleanor Frajka-Williams: ORCID iD orcid.org/0000-0001-8773-7838

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Date deposited: 05 Feb 2018 17:30
Last modified: 05 Feb 2018 17:30

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