Labrador Sea Water exported through Flemish Pass : Hydrographic trends and transport variability inducing processes
Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves.
Gespeichert in:
| Autor*in: |
Sanguineti, Linn [verfasserIn] |
|---|---|
| Körperschaften: |
Universität Bremen [Grad-verleihende Institution] |
| Hochschulschrift: |
Dissertation ; Universität Bremen ; 2017 |
| Format: |
E-Book |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
Bremen: 2017 |
|---|
| Formangabe: |
Hochschulschrift |
|---|
| Umfang: |
1 Online-Ressource (xi, 148 Seiten) ; Illustrationen |
|---|
| Weitere Ausgabe: |
Erscheint auch als Druck-Ausgabe Sanguineti, Linn: Labrador Sea Water exported through Flemish Pass - Bremen, 2017 |
|---|
| Links: |
|---|
| DOI / URN: |
urn:nbn:de:gbv:46-00106030-18 |
|---|
| Katalog-ID: |
895552647 |
|---|
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| 520 | |a Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. | ||
| 520 | |a This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. | ||
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17,O09 dnb 1138338451 DE-101 urn:nbn:de:gbv:46-00106030-18 urn (DE-627)895552647 (DE-576)9895552645 (DE-599)GBV895552647 (OCoLC)1000579391 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Sanguineti, Linn verfasserin aut Labrador Sea Water exported through Flemish Pass Hydrographic trends and transport variability inducing processes von Linn Sanguineti Bremen 2017 1 Online-Ressource (xi, 148 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2017 Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. 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17,O09 dnb 1138338451 DE-101 urn:nbn:de:gbv:46-00106030-18 urn (DE-627)895552647 (DE-576)9895552645 (DE-599)GBV895552647 (OCoLC)1000579391 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Sanguineti, Linn verfasserin aut Labrador Sea Water exported through Flemish Pass Hydrographic trends and transport variability inducing processes von Linn Sanguineti Bremen 2017 1 Online-Ressource (xi, 148 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2017 Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Sanguineti, Linn Labrador Sea Water exported through Flemish Pass Bremen, 2017 xi, 148 Seiten (DE-627)895552442 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 Resolving-System kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 2017-09-08 Resolving-System Volltext http://d-nb.info/1138338451/34 2017-09-08 Langzeitarchivierung Nationalbibliothek Volltext http://elib.suub.uni-bremen.de/edocs/00106030-1.pdf 2017-09-08 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 1711268518 x 09-09-17 21 01 0046 1707512132 ebook_2017_dissbremen Kostenloser Zugriff zza 15-08-17 22 01 0018 1711296317 SUBolrd xu 09-09-17 23 01 0830 171130946X olr-d x 09-09-17 30 01 0104 1711318639 z 09-09-17 40 01 0007 1711326658 xsn 09-09-17 60 01 0705 171134298X OLRD z 09-09-17 63 01 3401 1711358983 ORD x 09-09-17 65 01 0003 4168027457 GBV-ODiss Open Access z 17-07-22 70 01 0089 1711366056 zdo 09-09-17 105 01 0841 1711449857 z 09-09-17 110 01 3110 1711376213 x 09-09-17 132 01 0959 1711387908 OLR-DISS x 09-09-17 151 01 0546 3583680650 OLR-ODISS z 31-01-20 161 01 0960 1711408697 ORD x 09-09-17 293 01 3293 1711439053 ORD xf 09-09-17 370 01 4370 1711447269 x 09-09-17 2403 01 DE-LFER 3496787368 00 --%%-- --%%-- n --%%-- l01 24-07-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 21 00 DE-46 00 Universität Bremen 21 00 DE-46 00 Fachbereich 01: Physik/Elektrotechnik (FB 01) 21 00 DE-46 99 93 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2017_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2017-09-09:11:39:40 |
| allfields_unstemmed |
17,O09 dnb 1138338451 DE-101 urn:nbn:de:gbv:46-00106030-18 urn (DE-627)895552647 (DE-576)9895552645 (DE-599)GBV895552647 (OCoLC)1000579391 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Sanguineti, Linn verfasserin aut Labrador Sea Water exported through Flemish Pass Hydrographic trends and transport variability inducing processes von Linn Sanguineti Bremen 2017 1 Online-Ressource (xi, 148 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2017 Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Sanguineti, Linn Labrador Sea Water exported through Flemish Pass Bremen, 2017 xi, 148 Seiten (DE-627)895552442 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 Resolving-System kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 2017-09-08 Resolving-System Volltext http://d-nb.info/1138338451/34 2017-09-08 Langzeitarchivierung Nationalbibliothek Volltext http://elib.suub.uni-bremen.de/edocs/00106030-1.pdf 2017-09-08 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 1711268518 x 09-09-17 21 01 0046 1707512132 ebook_2017_dissbremen Kostenloser Zugriff zza 15-08-17 22 01 0018 1711296317 SUBolrd xu 09-09-17 23 01 0830 171130946X olr-d x 09-09-17 30 01 0104 1711318639 z 09-09-17 40 01 0007 1711326658 xsn 09-09-17 60 01 0705 171134298X OLRD z 09-09-17 63 01 3401 1711358983 ORD x 09-09-17 65 01 0003 4168027457 GBV-ODiss Open Access z 17-07-22 70 01 0089 1711366056 zdo 09-09-17 105 01 0841 1711449857 z 09-09-17 110 01 3110 1711376213 x 09-09-17 132 01 0959 1711387908 OLR-DISS x 09-09-17 151 01 0546 3583680650 OLR-ODISS z 31-01-20 161 01 0960 1711408697 ORD x 09-09-17 293 01 3293 1711439053 ORD xf 09-09-17 370 01 4370 1711447269 x 09-09-17 2403 01 DE-LFER 3496787368 00 --%%-- --%%-- n --%%-- l01 24-07-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 21 00 DE-46 00 Universität Bremen 21 00 DE-46 00 Fachbereich 01: Physik/Elektrotechnik (FB 01) 21 00 DE-46 99 93 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2017_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2017-09-09:11:39:40 |
| allfieldsGer |
17,O09 dnb 1138338451 DE-101 urn:nbn:de:gbv:46-00106030-18 urn (DE-627)895552647 (DE-576)9895552645 (DE-599)GBV895552647 (OCoLC)1000579391 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Sanguineti, Linn verfasserin aut Labrador Sea Water exported through Flemish Pass Hydrographic trends and transport variability inducing processes von Linn Sanguineti Bremen 2017 1 Online-Ressource (xi, 148 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2017 Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. Langzeitarchivierung gewährleistet pdager Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content Universität Bremen Grad-verleihende Institution (DE-588)2001386-3 (DE-627)101380429 (DE-576)191575038 dgg Bremen (DE-588)4008135-7 (DE-627)106369636 (DE-576)208874569 uvp Erscheint auch als Druck-Ausgabe Sanguineti, Linn Labrador Sea Water exported through Flemish Pass Bremen, 2017 xi, 148 Seiten (DE-627)895552442 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 Resolving-System kostenfrei Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 2017-09-08 Resolving-System Volltext http://d-nb.info/1138338451/34 2017-09-08 Langzeitarchivierung Nationalbibliothek Volltext http://elib.suub.uni-bremen.de/edocs/00106030-1.pdf 2017-09-08 Verlag kostenfrei Volltext GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2403 ISIL_DE-LFER BO 20 01 0084 1711268518 x 09-09-17 21 01 0046 1707512132 ebook_2017_dissbremen Kostenloser Zugriff zza 15-08-17 22 01 0018 1711296317 SUBolrd xu 09-09-17 23 01 0830 171130946X olr-d x 09-09-17 30 01 0104 1711318639 z 09-09-17 40 01 0007 1711326658 xsn 09-09-17 60 01 0705 171134298X OLRD z 09-09-17 63 01 3401 1711358983 ORD x 09-09-17 65 01 0003 4168027457 GBV-ODiss Open Access z 17-07-22 70 01 0089 1711366056 zdo 09-09-17 105 01 0841 1711449857 z 09-09-17 110 01 3110 1711376213 x 09-09-17 132 01 0959 1711387908 OLR-DISS x 09-09-17 151 01 0546 3583680650 OLR-ODISS z 31-01-20 161 01 0960 1711408697 ORD x 09-09-17 293 01 3293 1711439053 ORD xf 09-09-17 370 01 4370 1711447269 x 09-09-17 2403 01 DE-LFER 3496787368 00 --%%-- --%%-- n --%%-- l01 24-07-19 20 01 0084 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 21 01 0046 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 LF 22 01 0018 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 23 01 0830 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 30 01 0104 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 40 01 0007 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 60 01 0705 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 63 01 3401 E-Book http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 LF 65 01 0003 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 70 01 0089 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 105 01 0841 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 110 01 3110 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 132 01 0959 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 151 01 0546 Volltext http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 161 01 0960 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 293 01 3293 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 370 01 4370 http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 2403 01 DE-LFER http://nbn-resolving.de/urn:nbn:de:gbv:46-00106030-18 21 00 DE-46 00 Universität Bremen 21 00 DE-46 00 Fachbereich 01: Physik/Elektrotechnik (FB 01) 21 00 DE-46 99 93 60 01 0705 10 ho 20 01 0084 OLRD 110 01 3110 OLRD 370 01 4370 OLRD 21 01 0046 ebook_2017_dissbremen 22 01 0018 SUBolrd 23 01 0830 olr-d 60 01 0705 OLRD 63 01 3401 ORD 65 01 0003 GBV-ODiss 132 01 0959 OLR-DISS 151 01 0546 OLR-ODISS 161 01 0960 ORD 293 01 3293 ORD 23 01 0830 2017-09-09:11:39:40 |
| allfieldsSound |
17,O09 dnb 1138338451 DE-101 urn:nbn:de:gbv:46-00106030-18 urn (DE-627)895552647 (DE-576)9895552645 (DE-599)GBV895552647 (OCoLC)1000579391 DE-627 ger DE-627 rda eng XA-DE 550 DE-101 Sanguineti, Linn verfasserin aut Labrador Sea Water exported through Flemish Pass Hydrographic trends and transport variability inducing processes von Linn Sanguineti Bremen 2017 1 Online-Ressource (xi, 148 Seiten) Illustrationen Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Dissertation Universität Bremen 2017 Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. 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Labrador Sea Water exported through Flemish Pass Hydrographic trends and transport variability inducing processes |
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Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. |
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Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. |
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Oceanography, Flemish Pass, Labrador Sea Water, hydrographic variability, transport variability, topographic Rossby waves. This study investigates the deep flow through the 1200 m deep Flemish Pass, located at the western subpolar margin, constrained by the Grand Banks and the underwater plateau Flemish Cap. In addition to the Deep Western Boundary Current (DWBC) pathway offshore of Flemish Cap, Flemish Pass represents another southward export pathway for Labrador Sea Water (LSW), a main component of the climate modulating Atlantic Meridional Overturning Circulation. Hydrographic measurements show a significant warming of 0.3 degree/decade and a salinification of 0.03/decade of the Upper LSW in Flemish Pass between 1993 and 2013. Ship-based velocity measurements between 2009 and 2013 in Flemish Pass and in the DWBC east of Flemish Cap revealed a considerable southward transport of Upper LSW through Flemish Pass (15 - 27%). Mooring based transport time series revealed an average southward LSW transport of -1.9 Sv (-1.4 Sv) and a range of -3.5 Sv to 0.7 Sv (-5 Sv to 3 Sv) in Flemish Pass in 2012 - 2013 (2013 - 2014). The dominant LSW transport variability was observed on intra-seasonal time scales of 20 - 50 days and related to topographic Rossby waves trapped at the western slope of Flemish Pass. |
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Labrador Sea Water exported through Flemish Pass |
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