Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea)

In this memorandum we focus on one of the most important environmental factors affecting the propagation and dissipation of internal waves: the presence of strong vertical shear in the mean currents. Using a numerical model for the turbulent surface mixed layer, we have investigated two aspects of i...

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Bibliographic Details
Main Authors: Henderson, Laurel, Piacsek, Steve
Format: Other/Unknown Material
Language:English
Published: NATO. SACLANTCEN 1990
Subjects:
Online Access:https://hdl.handle.net/20.500.12489/199
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spelling ftcentremre:oai:cmre.archive.knowledgearc.net:20.500.12489/199 2023-05-15T17:46:59+02:00 Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea) Henderson, Laurel Piacsek, Steve 1990/12 vi, 23 p. : ill. 9 fig. https://hdl.handle.net/20.500.12489/199 English eng NATO. SACLANTCEN 1719 SM-241 http://hdl.handle.net/20.500.12489/199 Norwegian Sea Internal waves Currents Air-Sea interaction TOPS (Thermal Ocean Prediction System) model Inertial shear Scientific Memorandum (SM) 1990 ftcentremre https://doi.org/20.500.12489/199 2022-03-27T09:37:55Z In this memorandum we focus on one of the most important environmental factors affecting the propagation and dissipation of internal waves: the presence of strong vertical shear in the mean currents. Using a numerical model for the turbulent surface mixed layer, we have investigated two aspects of inertial shear statistics: the interannual variations due to variability of the atmospheric forcing fluxes, and the sensitivity of the model predicted shear to the grid size employed in the prediction model. To study the interannual variation of shear, we performed a simulation for the month of May for 20 consecutive years from 1960-1979 at the site of weathership 'Mike' in the Norwegian Sea. To examine the dependence of the shear statistics on the vertical grid size, we performed the computations on grid sizes of 1 m, 2 m, 5 m, and a grid approximating the TOPS grid (for the top 100 m). The results show that there are strong interannual variations in the magnitude and predominant depth of inertial shear, with magnitudes varying by a factor of up to three, and the depth of maximum shear moving by 30 m or more. A dependence of the these quantities on the vertical grid size is also found, with the simulation results showing large inaccuracies for 6% greater than 5 m. Other/Unknown Material Norwegian Sea CMRE Open Library (NATO STO Centre for Maritime Research and Experimentation Norwegian Sea
institution Open Polar
collection CMRE Open Library (NATO STO Centre for Maritime Research and Experimentation
op_collection_id ftcentremre
language English
topic Norwegian Sea
Internal waves
Currents
Air-Sea interaction
TOPS (Thermal Ocean Prediction System) model
Inertial shear
spellingShingle Norwegian Sea
Internal waves
Currents
Air-Sea interaction
TOPS (Thermal Ocean Prediction System) model
Inertial shear
Henderson, Laurel
Piacsek, Steve
Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea)
topic_facet Norwegian Sea
Internal waves
Currents
Air-Sea interaction
TOPS (Thermal Ocean Prediction System) model
Inertial shear
description In this memorandum we focus on one of the most important environmental factors affecting the propagation and dissipation of internal waves: the presence of strong vertical shear in the mean currents. Using a numerical model for the turbulent surface mixed layer, we have investigated two aspects of inertial shear statistics: the interannual variations due to variability of the atmospheric forcing fluxes, and the sensitivity of the model predicted shear to the grid size employed in the prediction model. To study the interannual variation of shear, we performed a simulation for the month of May for 20 consecutive years from 1960-1979 at the site of weathership 'Mike' in the Norwegian Sea. To examine the dependence of the shear statistics on the vertical grid size, we performed the computations on grid sizes of 1 m, 2 m, 5 m, and a grid approximating the TOPS grid (for the top 100 m). The results show that there are strong interannual variations in the magnitude and predominant depth of inertial shear, with magnitudes varying by a factor of up to three, and the depth of maximum shear moving by 30 m or more. A dependence of the these quantities on the vertical grid size is also found, with the simulation results showing large inaccuracies for 6% greater than 5 m.
format Other/Unknown Material
author Henderson, Laurel
Piacsek, Steve
author_facet Henderson, Laurel
Piacsek, Steve
author_sort Henderson, Laurel
title Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea)
title_short Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea)
title_full Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea)
title_fullStr Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea)
title_full_unstemmed Model statistics of inertial shear from multi- year simulations at weathership 'Mike': currents, atmospheric forcing, internal waves, mixed layer, Norwegian Sea)
title_sort model statistics of inertial shear from multi- year simulations at weathership 'mike': currents, atmospheric forcing, internal waves, mixed layer, norwegian sea)
publisher NATO. SACLANTCEN
publishDate 1990
url https://hdl.handle.net/20.500.12489/199
geographic Norwegian Sea
geographic_facet Norwegian Sea
genre Norwegian Sea
genre_facet Norwegian Sea
op_relation 1719
SM-241
http://hdl.handle.net/20.500.12489/199
op_doi https://doi.org/20.500.12489/199
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