Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region
Subsurface temperature and sound speed profiles are generated from satellite SST observations and validated by hydrocast observations. Hydrographic data from the October 1992 Iceland Faeroe frontal survey is used for the calculation of Empirical Orthogonal Functions (EOFs). Statistical relationships...
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NATO. SACLANTCEN
1996
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ftcentremre:oai:cmre.archive.knowledgearc.net:20.500.12489/312 2023-05-15T14:59:50+02:00 Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region Warn-Varnas, Alex Essen, Heinz-Hermann Gezgin, E. 1996/01 24 p. : ill. 15 fig. https://hdl.handle.net/20.500.12489/312 English eng NATO. SACLANTCEN ADB209666 2023 SR-246 http://hdl.handle.net/20.500.12489/312 Sea surface temperature (SST) Empirical Orthogonal Function (EOF) technique Sound velocity in sea water Iceland-Faeroe Frontal Scientific Report (SR) 1996 ftcentremre https://doi.org/20.500.12489/312 2022-03-27T09:37:57Z Subsurface temperature and sound speed profiles are generated from satellite SST observations and validated by hydrocast observations. Hydrographic data from the October 1992 Iceland Faeroe frontal survey is used for the calculation of Empirical Orthogonal Functions (EOFs). Statistical relationships between the EOF amplitudes and SSTs are derived and used for the construction of synthetic temperature profiles and sound speed distributions in the ocean. Average Root-Mean Square (RMS) errors were computed for synthetic temperature profiles in typical water categories. Corrections to the processed satellite SST data were applied using surface drifter data and sensitivity tests. The survey data reflects the water mass structure in three distinct regions; Atlantic, Frontal and Arctic, for which characteristic TS curves are derived. The best agreement between the synthetically generated temperature profiles, from SST data, with CTD measurements occurs in the Arctic region where a tendency to follow the slope and magnitude versus depth exists. The Frontal region shows disagreements in the upper thermocline with agreement elsewhere. In the Atlantic region there is agreement only in the upper mixed layer. In the thermocline regime the slope exhibits a parallel offset relative to the data. The differences are attributed to the inherent errors of EOF reconstruction which peak in the thermocline and the scatter of EOF amplitudes versus SST measurements. The work demonstrates that it is possible to derive synthetic temperature and sound speed profiles in the ocean from SST observations of particular water mass configurations at certain times of the season. Other/Unknown Material Arctic Iceland CMRE Open Library (NATO STO Centre for Maritime Research and Experimentation Arctic |
institution |
Open Polar |
collection |
CMRE Open Library (NATO STO Centre for Maritime Research and Experimentation |
op_collection_id |
ftcentremre |
language |
English |
topic |
Sea surface temperature (SST) Empirical Orthogonal Function (EOF) technique Sound velocity in sea water Iceland-Faeroe Frontal |
spellingShingle |
Sea surface temperature (SST) Empirical Orthogonal Function (EOF) technique Sound velocity in sea water Iceland-Faeroe Frontal Warn-Varnas, Alex Essen, Heinz-Hermann Gezgin, E. Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region |
topic_facet |
Sea surface temperature (SST) Empirical Orthogonal Function (EOF) technique Sound velocity in sea water Iceland-Faeroe Frontal |
description |
Subsurface temperature and sound speed profiles are generated from satellite SST observations and validated by hydrocast observations. Hydrographic data from the October 1992 Iceland Faeroe frontal survey is used for the calculation of Empirical Orthogonal Functions (EOFs). Statistical relationships between the EOF amplitudes and SSTs are derived and used for the construction of synthetic temperature profiles and sound speed distributions in the ocean. Average Root-Mean Square (RMS) errors were computed for synthetic temperature profiles in typical water categories. Corrections to the processed satellite SST data were applied using surface drifter data and sensitivity tests. The survey data reflects the water mass structure in three distinct regions; Atlantic, Frontal and Arctic, for which characteristic TS curves are derived. The best agreement between the synthetically generated temperature profiles, from SST data, with CTD measurements occurs in the Arctic region where a tendency to follow the slope and magnitude versus depth exists. The Frontal region shows disagreements in the upper thermocline with agreement elsewhere. In the Atlantic region there is agreement only in the upper mixed layer. In the thermocline regime the slope exhibits a parallel offset relative to the data. The differences are attributed to the inherent errors of EOF reconstruction which peak in the thermocline and the scatter of EOF amplitudes versus SST measurements. The work demonstrates that it is possible to derive synthetic temperature and sound speed profiles in the ocean from SST observations of particular water mass configurations at certain times of the season. |
format |
Other/Unknown Material |
author |
Warn-Varnas, Alex Essen, Heinz-Hermann Gezgin, E. |
author_facet |
Warn-Varnas, Alex Essen, Heinz-Hermann Gezgin, E. |
author_sort |
Warn-Varnas, Alex |
title |
Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region |
title_short |
Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region |
title_full |
Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region |
title_fullStr |
Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region |
title_full_unstemmed |
Deduction fo synthetic temperature profiles from SST observations in the Iceland-Faeroe frontal region |
title_sort |
deduction fo synthetic temperature profiles from sst observations in the iceland-faeroe frontal region |
publisher |
NATO. SACLANTCEN |
publishDate |
1996 |
url |
https://hdl.handle.net/20.500.12489/312 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Iceland |
genre_facet |
Arctic Iceland |
op_relation |
ADB209666 2023 SR-246 http://hdl.handle.net/20.500.12489/312 |
op_doi |
https://doi.org/20.500.12489/312 |
_version_ |
1766331949916356608 |