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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1990
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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 |
_version_ |
1766151072861126656 |