An advanced method to estimate deep currents from profiling floats
An advanced method to estimate deep currents from profiling floats
Subsurface ocean currents can be estimated from the positions of drifting profiling floats that are being widely deployed for the international Argo program. The calculation of subsurface velocity depends on how the trajectory of the float while on the surface is treated. The following three aspects of the calculation of drift velocities are addressed: the accurate determination of surfacing and dive times, a new method for extrapolating surface and dive positions from the set of discrete Argos position fixes, and a discussion of the errors in the method. In the new method described herein, the mean drift velocity and the phase and amplitude of inertial motions are derived explicitly from a least squares fit to the set of Argos position fixes for each surface cycle separately. The new method differs from previous methods that include prior assumptions about the statistics of inertial motions. It is concluded that the endpoints of the subsurface trajectory can be estimated with accuracy better than 1.7 km (East Sea/Sea of Japan) and 0.8 km (Indian Ocean). All errors, combined with the error that results from geostrophic shear and extrapolation, should result in individual subsurface velocity estimates with uncertainty of the order of 0.2 cm s?1.
1294-1304
Park, J.J.
28bc393d-8ba6-4f68-9562-fba4969b5d4f
Kim, K.
b7199e71-15d6-4159-ac0a-c7f1261a5439
King, B.A.
d9d50671-3777-453b-9f85-c67a56a4d8b8
Riser, S.C.
c19420bf-bd49-47d3-b7b8-189c9e7b7fdf
2005
Park, J.J.
28bc393d-8ba6-4f68-9562-fba4969b5d4f
Kim, K.
b7199e71-15d6-4159-ac0a-c7f1261a5439
King, B.A.
d9d50671-3777-453b-9f85-c67a56a4d8b8
Riser, S.C.
c19420bf-bd49-47d3-b7b8-189c9e7b7fdf
Park, J.J., Kim, K., King, B.A. and Riser, S.C.
(2005)
An advanced method to estimate deep currents from profiling floats.
Journal of Atmospheric and Oceanic Technology, 22 (8), .
(doi:10.1175/JTECH1748.1).
Abstract
Subsurface ocean currents can be estimated from the positions of drifting profiling floats that are being widely deployed for the international Argo program. The calculation of subsurface velocity depends on how the trajectory of the float while on the surface is treated. The following three aspects of the calculation of drift velocities are addressed: the accurate determination of surfacing and dive times, a new method for extrapolating surface and dive positions from the set of discrete Argos position fixes, and a discussion of the errors in the method. In the new method described herein, the mean drift velocity and the phase and amplitude of inertial motions are derived explicitly from a least squares fit to the set of Argos position fixes for each surface cycle separately. The new method differs from previous methods that include prior assumptions about the statistics of inertial motions. It is concluded that the endpoints of the subsurface trajectory can be estimated with accuracy better than 1.7 km (East Sea/Sea of Japan) and 0.8 km (Indian Ocean). All errors, combined with the error that results from geostrophic shear and extrapolation, should result in individual subsurface velocity estimates with uncertainty of the order of 0.2 cm s?1.
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Published date: 2005
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Local EPrints ID: 17748
URI: http://eprints.soton.ac.uk/id/eprint/17748
ISSN: 0739-0572
PURE UUID: f29dc5cb-f804-4b8f-a7f4-54db2938fbdf
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Date deposited: 24 Oct 2005
Last modified: 15 Mar 2024 06:01
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Author:
J.J. Park
Author:
K. Kim
Author:
B.A. King
Author:
S.C. Riser
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