Pathways of the Greenland Sea warming
|
|
- Tyler Woods
- 5 years ago
- Views:
Transcription
1 GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L10608, doi: /2007gl029974, 2007 Pathways of the Greenland Sea warming Waldemar Walczowski 1 and Jan Piechura 1 Received 12 March 2007; revised 23 April 2007; accepted 1 May 2007; published 30 May [1] Progressive warming of the West Spitsbergen Current (WSC) has been observed since During summer 2006 temperature and salinity of the core of Atlantic Water (AW) reached the highest ever observed by the Institute of Oceanology Polish Academy of Sciences (IOPAS) values. The structure of the WSC, the heat content and the extent of AW in the Fram Strait (FS) region has also changed. Temperature changes resulted from the upstream warming of the Norwegian-Atlantic Current (NwAC); the structure of the WSC and its heat content were modified by the northward advection of large mesoscale eddies observed within the western branch of the WSC in summer These changes may have large impacts on the Arctic Ocean (AO) climate and ecosystem. Citation: Walczowski, W., and J. Piechura (2007), Pathways of the Greenland Sea warming, Geophys. Res. Lett., 34, L10608, doi: /2007gl Introduction [2] Two branches of the NwAC, slope and offshore, carry warm, salty AW northward through the Norwegian Sea [Orvik and Niiler, 2002] (Figure 1). The eastern branch, called the Norwegian Atlantic Slope Current (NwASC), is a nearly barotropic flow related to the Norwegian shelf break. This current continues northward over the Barents Sea slope and along the West Spitsbergen shelf break as the WSC. The WSC carries only part (about 60%) of the AW transported by the NwASC; the other part, after passing northern Norway, branches eastward into the Barents Sea. Skagseth et al. [2004] claimed that the large-scale variability of the NwASC is a coherent mode extending from the shelf edge west of Ireland to the Fram Strait. They also describe this system as the main conduit of heat and salt between the North Atlantic Ocean and the Artic Ocean. [3] Considering northward transport of the AW, the WSC has been traditionally described as this barotropic flow along the Barents Sea and the West Spitsbergen shelf-break. The existence of a second, mostly baroclinic, western branch over the Mohns and Knipovich Ridges was postulated earlier [Walczowski et al., 2005], but its role in AW poleward transport was not considered. The western branch, which could be a continuation of the little known NwAC offshore branch, is an along-frontal baroclinic jet steered by the bottom topography of the Mohns and Knipovich Ridges. The dynamics of this flow are characterized by high variability and mesoscale activity, and eddies in the Arctic Front (AF) have been observed by IOPAS each summer. The part of AW carried by the western branch crosses the AF and joins Greenland Sea Gyre [Piechura and Walczowski, 1995], 1 Institute of Oceanology, Polish Academy of Sciences, Sopot, Poland. Copyright 2007 by the American Geophysical Union /07/2007GL while the other fraction recirculates westward between 76 and 78 N. The bottom configuration causes the poleward flowing branches of the WSC to converge in the region of western Spitsbergen, at latitude of about 78 N. Continuing north, the current diverges again into three paths. The Svalbard and Yermak branches flow into to the AO through the FS (Figure 1), while the offshore branch recirculates westward and then southward [Manley, 1995]. The Svalbard Branch is fed by the along-slope core of the WSC, and recirculation is maintained by the western branch of the WSC. The postulated origin of the central, Yermak Branch, by the splitting of the Svalbard Branch due to bottom topography is not clear. Current investigations indicate that this central WSC branch may influence both, transport through the FS, and AW recirculation. [4] Since summer 2004, substantial increases have been observed in the temperature, salinity and heat transport of the WSC [Walczowski and Piechura, 2006; Beszczynska- Möller et al., 2007]. Holliday et al. [2007] found that the anomaly observed in had been formed in 1998 in the eastern subpolar gyre. Hakkinen and Rhines [2004] and Hátún et al. [2005] showed that the intensification of northward flow of warm, saline subtropical water was caused by changes in the subpolar gyre and increasing entrainment of AW into subarctic circulation. Increasing AW temperature, salinity, and heat transport by the NwASC was reported by Orvik and Skagseth [2005]. The time needed for the warm anomaly to travel from the Svinoy Section (63 N) to FS (79 N) was estimated at 18 months [Polyakov et al., 2005], which indicates that the mean speed of anomaly propagation was 3.8 cm/s. A similar value is derived using results from the Svinoy Section published by Orvik and Skagseth [2005] and IOPAS data for section N along the N parallel, which indicate a time lag of 18 to 21 months between the temperature increase in the Svinoy Section and the N section. This differs from the mean signal propagation speed from the Rockall Trough (57 N) to the Fram Strait, which was estimated based on information in the work of Holliday et al. [2007] at about 1.6 cm/s. 2. Data and Methods [5] The data used in the study were collected by IOPAS during cruises to the Nordic Seas. A detailed description of the data set and methods can be found in the work of Walczowski and Piechura [2006]. In this paper we also present data collected along N parallel during r/v Oceania cruises in summers and two CTD sections obtained by the Institute of Marine Research in Bergen. All anomalies were calculated in reference to the mean from the summers of Baroclinic calculations were applied to describe the structure of the currents. Although this method does not yield exact values of total L of5
2 Figure 1. Sketch of the AW currents in the Nordic Seas. fluxes, it represents the long-time averaged flows associated with water mass advection and variability. The temperature of and the heat stored in the AW layer were analyzed. Interannual variability of the heat flux to the atmosphere and seasonality of AW temperature was not considered. 3. Results [6] AW propagation pathways are represented by the mean baroclinic flow kinetic energy for the summers of (Figure 2). The western branch of the WSC, manifested as a strong flow over the underwater ridges, continues northward from the southwestern part of the study area. The eastern branch (core) of the WSC, in the southeastern part of study area is less visible, mostly due to the barotropic nature of the flow in this region and sparse covering by measurements. The core is more distinct over the shelf-break, north of the 74 N parallel. The distribution of mean currents also indicates that the western branch divides at the latitude of 73 N into two streams: one that flows northward over the ridges, and a second that joins the WSC core. Due to bottom topography, all the streams converge west of Spitsbergen at latitude of about 78 N. Very similar pathways were inferred by Jakobsen et al. [2003] from Lagrangian drifters. [7] Substantial summer-to-summer differences are noted in both flow magnitudes and patterns. In some years the western branch was relatively strong (2001), while in others eastern branch was dominating (2002). The summers of 2005 and 2006 were particularly characterized by an intensification of the northward flow. Since 2004, there have been signs of higher AW temperature and salinity propagation to the north towards the Fram Strait. Never-recorded by IOPAS, high AW salinity and temperature values in the WSC core west of Spitsbergen were observed in the summer of Unusually large and warm anticyclonic eddies in the western branch of the WSC carried a large amount of heat northward [Walczowski and Piechura, 2006] (Figure 3a). They further suggested that these structures would transport a large amount of heat into the AO through the Fram Strait. Indeed, in summer 2006 ice conditions in the region of northeastern Spitsbergen were unusual; in areas where AW remained at the surface, the sea ice edge was shifted towards the north and east. The winter of was curiously warm in Svalbard possibly due to the inflow of AW into the fjords and the release of heat into the atmosphere. The temperature of AW column recorded by a mooring situated in the Kongsfjorden [Cottier et al., 2005] increased from the end of January 2006 until March 2006 (F. R. Cottier, personal communication, 2006). This could be an effect of the communication of the heat anomaly observed in summer 2005 at 76 N (Figure 3a). The movement from latitude of 76 N to latitude of Kongsfjorden (79 N) within a six-month period indicates a mean propagation speed of about 2.1 cm/s. [8] The temperature of the AW core west of Spitsbergen was even higher in summer 2006 than it was in 2005, and heat anomalies shifted from the WSC western branch to the central part and over the Spitsbergen shelf break (Figure 3b). Because of this, warm AW extended over the shelf and penetrated the fjords. Horizontal distributions and water mass properties suggest that the heat anomaly observed in summer 2006 south of FS was the same as that observed in 2005 in the western branch at N. The hydrographic properties of the water in both places were very similar, and the mean anomaly propagation speed was 1.9 cm/s, a value similar to that estimated by Furevik at cm/s [Furevik, 2000]. [9] The mean northward propagation of the AW warming is clearly visible in the position of the summer isotherms. At 100 m the isotherm of 5 C (Figure 4) moved to the north Figure 2. Mean kinetic energy (cm 2 /s 2 ) of baroclinic currents at 100 dbar in the summers of of5
3 Figure 3. Heat content anomaly (10 9 J/m 2 ) of the AW layer in the summers of (a) 2005 and (b) more than 2 of latitude per year from 2004 to This corresponds to a summer-to-summer mean propagation velocity of the temperature signal of 0.8 cm/s. The horizontal temperature and baroclinic current distributions suggest that in 2004 warm AW entered the investigated area carried by the NwASC and was advected eastward to the Barents Sea and northward along the slope (Figure 4a). In 2005 the northward propagation of the AW warm signal intensified mostly due to large anticyclonic eddies in the western branch (Figure 4b). The AW layer heat anomaly observed in 2005 in the southwestern part continued northeastward, joined the core of the WSC, and then moved northward along the slope. Also in summer 2006 intensive AW inflow into investigated area along the western branch was observed (Figure 4c). The warmer fraction of the inflowing water turned northeastward between 72 and 73 N and continued northward along the slope. 4. Discussion and Conclusions [10] The data presented indicate that the temperature and heat content rise of the WSC is not only caused by the Figure 4. Distribution of temperature and baroclinic currents at 100 dbar in summers (a) 2004, (b) 2005, and (c) The 2 C and 5 C isolines are in bold. 3of5
4 Figure 5. Section along N parallel, between latitudes 04 E 15 E. (a)temperature at 200 dbar, summers (b) Hovmoeller plot of the heat content (GJ/m 2 ) of AW layer in summers Bottom topography has been marked. NwASC. The western branch of Atlantic inflow might also influence WSC temporal variability. The propagation of changes by the slope current system (NwASC, WSC core) is fast at about 3.8 cm/s, which is due to the coherent structure of these barotropic currents. Presented results indicate that the propagation of the anomaly by the western branch of the WSC may be two-fold slower, about cm/s. A northward shift of the 5 C isotherm towards the Fram Strait was slower due to cooling of the AW layer during its northward advection and observed summer-tosummer mean velocity was 0.8 cm/s. [11] The differing velocities of signal propagation among the various downstream branches that converge in Fram Strait will clearly impact the mean characteristics and dynamics of AW entering the AO. For example, Orvik and Skagseth [2005] showed that the mean NwASC temperature in the Svinoy Section increased in beginning of 2002 and then stabilized in If the overall signal transmission time between Svinoy Section and Fram Strait is 18 months, as postulated by Polyakov et al. [2005], then the mean AW temperature in Fram Strait should have stabilized in 2004, but this did not occur. Rising temperature and heat content of the AW layer at N parallel occurred in stages (Figure 5). In 2004 temperature has raised along whole section. In 2005 the core temperature decreased a bit while entire western part still continues warming. Finally, in 2006 warm anomaly moved from the western part over the slope, shifting the core over the shelfbreak. The mean AW temperature and heat content increase observed in 2005 and 2006 was carried by the western, highly baroclinic branch, which is slower than the barotropic current. Intensity of baroclinic currents and mesoscale activity along the AF depend of the front strength. Weakening and strengthening of the AF is correlated with increasing and decreasing of the NAO index [Schlichtholz and Goszczko, 2006]. [12] The specific pathways of AW in the southern part of the Nordic Seas, but especially the activity of the western branch of WSC, might also be very important for transport into the AO through the Fram Strait. Converging bottom topography at 78 N modifies pattern of AW circulation and inflow into AO. The core of AW supplied by the NwASC, after passing 78 N parallel follows Spitsbergen slope as the Svalbard Branch. Westward AW recirculation is maintained mostly by the western branch continuing over the AF. The present results indicate that the western branch of WSC entering the Greenland Sea over the ridges might also turn northeastward and next move northward along the slope. This path, which is parallel to the core flow, might pass the 78 N bottom narrowing and flow into the AO as the central, Yermak Branch (Figure 1); upstream propagation pathways might have a decisive impact on the southwestward recirculation or northward inflow of AW into the AO. [13] Similar to Holliday et al. [2007], the authors concluded that the unusually warm inflow into the Arctic Ocean will continue; however, the IOPAS upstream data further suggest that the local maximum of WSC warming has already occurred or should do so before summer 2007: in the southern part of the study area, the highest AW temperature in the summer of 2006 was already lower than 4of5
5 that in Since the increased heat inflow into the AO was mostly due to the higher AW temperature [Beszczynska- Möller et al., 2007], and upstream data show temperature decreasing already in 2006, we anticipate that in 2007 heat inflow into the AO will decrease. These short-term predictions were constructed based on the hydrographical situation in summer 2006 in the area between Norway and the Fram Strait. In contrast, the time series for locations far upstream that were presented by Holliday et al. [2007] suggest a renewed warming of AW inflow in subsequent years. [14] The International Polar Year (IPY) activity has begun in Intensive investigations of the AO and the subpolar seas will be conducted with icebreakers, moorings, drifting stations, automatic drifters, satellite observations, and other means. In this paper we have described the structure of the flow and the hydrographic situation upstream from the Fram Strait in the summer of 2006 and suggest that these conditions will influence the AO during the IPY. [15] Acknowledgments. We are grateful to the entire crew of the r/v Oceania who participated in the work at sea. Thanks are due to Kjell Arne Mork and the Institute of Marine Research, Bergen, for providing some hydrographic data. This research was supported by a grant from the European Union Fifth Framework Programme project ASOF-N (Arctic-Subarctic Ocean Flux Array for European Climate: North), contract EVK2-CT , and Sixth Framework Programme DAMOCLES (Developing Arctic Modelling and Observing Capabilities for Long-term Environment Studies), contract GOCE. References Beszczynska-Möller, A., U. Schauer, and E. Fahrbach (2007), Variations of the Atlantic inflow and related heat flux through Fram Strait in the last decade, CLIVAR Exch., 12(1), 7 8. Cottier, F. R., V. Tverberg, M. Inall, H. Svendsen, and C. Griffiths (2005), Water mass modification in an Arctic fjord through cross-shelf exchange: The seasonal hydrography of Kongsfjorden, Svalbard, J. Geophys. Res., 110, C12005, doi: /2004jc Furevik, T. (2000), On anomalous sea surface temperatures in the Nordic Seas, J. Clim., 13, Hakkinen, S., and P. B. Rhines (2004), Decline of subpolar North Atlantic circulation during the 1990s, Science, 304, Hátún, H., A. B. Sandø, H. Drange, B. Hansen, and H. Valdimarsson (2005), Influence of the Atlantic subpolar gyre on the thermohaline circulation, Science, 309, Holliday, N. P., S. Hughes, A. Lavín, K. A. Mork, G. Nolan, W. Walczowski, and A. Beszczynska-Möller (2007), The end of a trend? The progression of unusually warm and saline water from the eastern North Atlantic into the Arctic Ocean, CLIVAR Exch., 12(1), Jakobsen, P., M. Ribergaard, D. Quadfasel, T. Schrnith, and C. Hughes (2003), Near-surface circulation in the northern North Atlantic as inferred from Lagrangian drifters: Variability from the mesoscale to interannual, J. Geophys. Res., 108(C8), 3251, doi: /2002jc Manley, T. O. (1995), Branching of Atlantic Water within the Greenland- Spitsbergen Passage: An estimate of recirculation, J. Geophys. Res., 100, 20,627 20,634. Orvik, K. A., and P. Niiler (2002), Major pathways of Atlantic water in the northern North Atlantic and Nordic Seas toward Arctic, Geophys. Res. Lett., 29(19), 1896, doi: /2002gl Orvik, K. A., and Ø. Skagseth (2005), Heat flux variations in the eastern Norwegian Atlantic Current toward the Arctic from moored instruments, , Geophys. Res. Lett., 32, L14610, doi: / 2005GL Piechura, J., and W. Walczowski (1995), The Arctic Front: Structure and dynamics, Oceanologia, 37(1), Polyakov, I. V., et al. (2005), One more step toward a warmer Arctic, Geophys. Res. Lett., 32, L17605, doi: /2005gl Schlichtholz, P., and I. Goszczko (2006), Interannual variability of the Atlantic water layer in the West Spitsbergen Current at 76.5 N in summer , Deep-Sea Res., Part I, 53, Skagseth, Ø., K. Orvik, and T. Furevik (2004), Coherent variability of the Norwegian Atlantic Slope Current derived from TOPEX//ERS altimeter data, Geophys. Res. Lett., 31, L14304, doi: /2004gl Walczowski, W., and J. Piechura (2006), New evidence of warming propagating toward the Arctic Ocean, Geophys. Res. Lett., 33, L12601, doi: /2006gl Walczowski, W., J. Piechura, R. Osinski, and P. Wieczorek (2005), The West Spitsbergen Current volume and heat transport from synoptic observations in summer, Deep-Sea Res., Part I, 52, J. Piechura and W. Walczowski, Institute of Oceanology, Polish Academy of Sciences, Powstancow Warszawy 55, Sopot, Poland. (walczows@iopan.gda.pl) 5of5
Cruise Report R/V Oceania, AREX 2007
Powstańców Warszawy 55, PL - 81-712 Sopot, P.O. Box 68 March 15, 2008 Cruise Report R/V Oceania, AREX 2007 Ship: R/V Oceania Cruise: AREX 2007 Dates: 19.06.2007 05.08.2007 Port Calls: Gdansk (Poland) Longyearbyen
More informationCruise Report R.V. Oceania, AREX2004
Powstaców Warszawy, PL - 81-71 Sopot, P.O. Box 68 November 16. 4 Cruise Report R.V. Oceania, AREX4 Ship: Cruise: R.V. Oceania Arex4 Dates: 8.6.4 19.7.4 Port Calls: Sopot (Poland) Longyearbyen (Spitsbergen)
More informationCruise Report. RV Oceania, AREX2011. Institute of Oceanology Polish Academy of Sciences. the Norwegian, Greenland and Barents Seas
w Warszawy 55, 81-712 Sopot, Poland, P.O. Box 68 10 December, 2011 Cruise Report RV Oceania, AREX2011 Institution Ship Name Cruise Name Institute of Oceanology Polish Academy of Sciences RV Oceania AREX2011
More informationThe deepening of the Atlantic water in the Lofoten Basin of the Norwegian Sea, demonstrated by using an active reduced gravity model
GEOPHYSICAL RESEARCH LETTERS, VOL. 31, L01306, doi:10.1029/2003gl018687, 2004 The deepening of the Atlantic water in the Lofoten Basin of the Norwegian Sea, demonstrated by using an active reduced gravity
More informationHeat flux variations in the eastern Norwegian Atlantic Current toward the Arctic from moored instruments,
GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L14610, doi:10.1029/2005gl023487, 2005 Heat flux variations in the eastern Norwegian Atlantic Current toward the Arctic from moored instruments, 1995 2005 Kjell Arild
More informationICES Journal of Marine Science
ICES Journal of Marine Science ICES Journal of Marine Science (2012), 69(5), 852 863. doi:10.1093/icesjms/fss056 Variability in Atlantic water temperature and transport at the entrance to the Arctic Ocean,
More informationProd:Type:COM ARTICLE IN PRESS. The West Spitsbergen Current volume and heat transport from synoptic observations in summer
B2v8:06a=w ðdec 200Þ:c XML:ver::0: DSRI : 20 Prod:Type:COM pp:8ðcol:fig::4;6;;þ ED:Sushma PAGN:Dini SCAN:Dominic Deep-Sea Research I ] (]]]]) ]]] ]]] www.elsevier.com/locate/dsr The West Spitsbergen Current
More informationProblems with estimation and interpretation of oceanic heat transport conceptual remarks for the case of Fram Strait in the Arctic Ocean
Ocean Sci., 5, 487 494, 2009 Author(s) 2009. This work is distributed under the Creative Commons Attribution 3.0 License. Ocean Science Problems with estimation and interpretation of oceanic heat transport
More informationAtlantic Water inflow north of Svalbard; new insights from recent years
Atlantic Water inflow north of Svalbard; new insights from recent years Arild Sundfjord, Norwegian Polar Institute, Tromsø Partners: Norwegian Polar Institute, Institute of Marine Research, Universty of
More informationForcing of oceanic heat anomalies by air sea interactions in the Nordic Seas area
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116,, doi:10.1029/2009jc005944, 2011 Forcing of oceanic heat anomalies by air sea interactions in the Nordic Seas area P. Schlichtholz 1 and M. N. Houssais 2 Received
More informationA Synthesis of Results from the Norwegian ESSAS (N-ESSAS) Project
A Synthesis of Results from the Norwegian ESSAS (N-ESSAS) Project Ken Drinkwater Institute of Marine Research Bergen, Norway ken.drinkwater@imr.no ESSAS has several formally recognized national research
More informationOn the recent time history and forcing of the inflow of Atlantic Water to the Arctic Mediterranean
On the recent time history and forcing of the inflow of Atlantic Water to the Arctic Mediterranean Jan Even Ø. Nilsen (1), Hjálmar Hátún (2), Anne Britt Sandø (1), Ingo Bethke (1,3), Olivier Laurantin
More informationVariability of the surface circulation of the Nordic Seas during the 1990s
ICES Marine Science Symposia 219: 367-370. Variability of the surface circulation of the Nordic Seas during the 1990s Philip K. Jakobsen, Mads H. Ribergaard, Detlef Quadfasel, and Torben Schmith The surface
More informationChanges in the properties and distribution of the intermediate and deep waters in the Fram Strait
Changes in the properties and distribution of the intermediate and deep waters in the Fram Strait Helene R. Langehaug 1,2 and Eva Falck 3 1 Nansen Environmental and Remote Sensing Center, Bergen, Norway.
More informationOn Modeling the Oceanic Heat Fluxes from the North Pacific / Atlantic into the Arctic Ocean
On Modeling the Oceanic Heat Fluxes from the North Pacific / Atlantic into the Arctic Ocean Wieslaw Maslowski Naval Postgraduate School Collaborators: Jaclyn Clement Kinney Terry McNamara, John Whelan
More informationNational Oceanography Centre. Research & Consultancy Report No. 36
National Oceanography Centre Research & Consultancy Report No. 36 State of the eastern North Atlantic subpolar gyre: The Extended Ellett Line Programme Annual Report No. 1 N P Holliday 1, S Cunningham
More informationWater masses and circulation pathways through the Iceland Basin during Vivaldi 1996
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109,, doi:10.1029/2003jc002067, 2004 Water masses and circulation pathways through the Iceland Basin during Vivaldi 1996 R. T. Pollard, J. F. Read, and N. P. Holliday
More informationSkagseth et al ASOF-book
Skagseth et al. - 1 - ASOF-book Volume and heat transports to the Arctic Ocean via the Norwegian and Barents Seas. by Øystein Skagseth a,c, Tore Furevik b,c, Randi Ingvaldsen a,c, Harald Loeng a,c, Kjell
More informationVolume and heat transports to the Arctic Ocean via the Norwegian and Barents Seas.
Volume and heat transports to the Arctic Ocean via the Norwegian and Barents Seas. Øystein Skagseth a,c, Tore Furevik b,c, Randi Ingvaldsen a,c, Harald Loeng a,c,kjell Arne Mork a,c, Kjell Arild Orvik
More informationMonitoring the Norwegian Atlantic slope current using a single moored current meter
Monitoring the Norwegian Atlantic slope current using a single moored current meter Kjell Arild Orvik a and Øystein Skagseth a, b a Geophysical Institute, University of Bergen, Allegaten 70, N-5007, Bergen,
More informationWintertime warming of an Arctic shelf in response to large-scale atmospheric circulation
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L10607, doi:10.1029/2007gl029948, 2007 Wintertime warming of an Arctic shelf in response to large-scale atmospheric circulation F. R.
More informationUpper Ocean Circulation
Upper Ocean Circulation C. Chen General Physical Oceanography MAR 555 School for Marine Sciences and Technology Umass-Dartmouth 1 MAR555 Lecture 4: The Upper Oceanic Circulation The Oceanic Circulation
More informationObservations of water masses and circulation with focus on the Eurasian Basin of the Arctic Ocean from the 1990s to the late 2000s
https://helda.helsinki.fi Observations of water masses and circulation with focus on the Eurasian Basin of the Arctic Ocean from the 1990s to the late 2000s Rudels, B. 2013 Rudels, B, Schauer, U, Bjork,
More informationRelation between the wind stress curl in the North Atlantic and the Atlantic inflow to the Nordic Seas
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113,, doi:10.1029/2007jc004236, 2008 Relation between the wind stress curl in the North Atlantic and the Atlantic inflow to the Nordic Seas A. B. Sandø 1,2 and T.
More informationUpper ocean heat content in the Nordic seas
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114,, doi:10.1029/2007jc004674, 2009 Upper ocean heat content in the Nordic seas Daniela Di Iorio 1 and Caitlin Sloan 1 Received 4 December 2007; revised 12 January
More informationf r o m a H i g h - R e s o l u t i o n I c e - O c e a n M o d e l
Circulation and Variability in the Western Arctic Ocean f r o m a H i g h - R e s o l u t i o n I c e - O c e a n M o d e l Jeffrey S. Dixon 1, Wieslaw Maslowski 1, Jaclyn Clement 1, Waldemar Walczowski
More informationTemperature and salinity fluctuations in the Norwegian Sea in relation to wind
ICES Annual Science Conference 1999 Theme session L: Nordic Seas Exchanges ICES C.M. 19991L:03 Temperature and salinity fluctuations in the Norwegian Sea in relation to wind by Kjell Arne Mork and Lars
More informationArctic oceanography; the path of North Atlantic Deep Water
Chapter 7 Arctic oceanography; the path of North Atlantic Deep Water The importance of the Southern Ocean for the formation of the water masses of the world ocean poses the question whether similar conditions
More informationGeneral AW Circulation Schemes
General AW Circulation Schemes Aagaard, 1989 - topographically steered boundary current along slopes and ridges - interior flow weak, dominated by eddies (based on current meters) Rudels et al, 1994 -
More informationIsopycnal Analysis of Near-surface Waters in the Norwegian-Barents Sea Region. by Tom Rossby, Vladimir Ozhigin, Victor Ivshin, and Sheldon Bacon
INTERNATIONAL COUNCIL FOR THE EXPLORATION OF THE SEA ICES CM 2006/C:14 Use of isopycnal water mass to distinguish between variability due to the heaving of, and property change on density surfaces. Isopycnal
More informationPUBLICATIONS. Journal of Geophysical Research: Oceans
PUBLICATIONS Journal of Geophysical Research: Oceans RESEARCH ARTICLE Key Points: Two summer 2012 shipboard surveys document the evolution of the East Greenland Current (EGC) system from Fram Strait to
More informationVariability in the Slope Water and its relation to the Gulf Stream path
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L03606, doi:10.1029/2007gl032183, 2008 Variability in the Slope Water and its relation to the Gulf Stream path B. Peña-Molino 1 and T.
More informationNOTES AND CORRESPONDENCE
SEPTEMBER 2008 N O T E S A N D C O R R E S P O N D E N C E 2097 NOTES AND CORRESPONDENCE On the Temporally Varying Northward Penetration of Mediterranean Overflow Water and Eastward Penetration of Labrador
More informationCirculation in the South China Sea in summer of 1998
Circulation in the South China Sea in summer of 1998 LIU Yonggang, YUAN Yaochu, SU Jilan & JIANG Jingzhong Second Institute of Oceanography, State Oceanic Administration (SOA), Hangzhou 310012, China;
More informationRecent warming and changes of circulation in the North Atlantic - simulated with eddy-permitting & eddy-resolving models
Recent warming and changes of circulation in the North Atlantic - simulated with eddy-permitting & eddy-resolving models Robert Marsh, Beverly de Cuevas, Andrew Coward & Simon Josey (+ contributions by
More informationA possible mechanism for the strong weakening of the North Atlantic subpolar gyre in the mid-1990s
GEOPHYSICAL RESEARCH LETTERS, VOL. 36, L15602, doi:10.1029/2009gl039166, 2009 A possible mechanism for the strong weakening of the North Atlantic subpolar gyre in the mid-1990s Katja Lohmann, 1,2,3 Helge
More informationTemporal switching between sources of the Denmark Strait overflow water
II. Regional ocean climate ICES Marine Science Symposia, 219: 319-325. 23 Temporal switching between sources of the Denmark Strait overflow water Bert Rudels, Patrick Eriksson, Erik Buch, Gereon Budéus,
More informationModeling Arctic Intermediate Water: The effects of Neptune parameterization and horizontal resolution
Article Advances in Polar Science doi: 10.3724/SP.J.1085.2013.00098 June 2013 Vol. 24 No. 2: 98-105 Modeling Arctic Intermediate Water: The effects of Neptune parameterization and horizontal resolution
More informationSCIENTIFIC COUNCIL MEETING JUNE Atlantic Subpolar Gyre Warming Impacts on Greenland Offshore Waters? M. Stein
NOT TO BE CITED WITHOUT PRIOR REFERENCE TO THE AUTHOR(S) Northwest Atlantic Fisheries Organization Serial No. N5072 NAFO SCR Doc. 05/1 SCIENTIFIC COUNCIL MEETING JUNE 2005 Atlantic Subpolar Gyre Warming
More informationThe seasonal and interannual variability of circulation in the eastern and western Okhotsk Sea and its impact on plankton biomass
The seasonal and interannual variability of circulation in the eastern and western Okhotsk Sea and its impact on plankton biomass Andrey G. Andreev, Sergey V. Prants, Maxim V. Budyansky and Michael Yu.
More informationLET NOT THAT ICE MELT IN SVALBARD S. RAJAN, INCOIS NEELU SINGH, NCAOR
LET NOT THAT ICE MELT IN SVALBARD S. RAJAN, INCOIS NEELU SINGH, NCAOR 1. Arctic (surface air) temperatures are rising twice as fast as the temperatures in the rest of the world (Amplification). The Arctic
More informationRegional Sea Ice Outlook for Greenland Sea and Barents Sea - based on data until the end of May 2013
Regional Sea Ice Outlook for Greenland Sea and Barents Sea - based on data until the end of May 2013 Sebastian Gerland 1*, Max König 1, Angelika H.H. Renner 1, Gunnar Spreen 1, Nick Hughes 2, and Olga
More informationMechanisms for the variability of dense water pathways in the Nordic Seas
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 114,, doi:10.1029/2008jc004916, 2009 Mechanisms for the variability of dense water pathways in the Nordic Seas Rolf H. Käse, 1 Nuno Serra, 1 Armin Köhl, 1 and Detlef
More informationOcean Mixing and Climate Change
Ocean Mixing and Climate Change Factors inducing seawater mixing Different densities Wind stirring Internal waves breaking Tidal Bottom topography Biogenic Mixing (??) In general, any motion favoring turbulent
More informationEddy-induced meridional heat transport in the ocean
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L20601, doi:10.1029/2008gl035490, 2008 Eddy-induced meridional heat transport in the ocean Denis L. Volkov, 1 Tong Lee, 1 and Lee-Lueng Fu 1 Received 28 July 2008;
More informationObserved rate of loss of Arctic ice extent is faster than IPCC AR4 predictions
When will Summer Arctic Sea Ice Disappear? Wieslaw Maslowski Naval Postgraduate School Collaborators: Jaclyn Clement Kinney, Andrew Miller, Terry McNamara, John Whelan - Naval Postgraduate School Jay Zwally
More informationThe Planetary Circulation System
12 The Planetary Circulation System Learning Goals After studying this chapter, students should be able to: 1. describe and account for the global patterns of pressure, wind patterns and ocean currents
More informationAPPENDIX B PHYSICAL BASELINE STUDY: NORTHEAST BAFFIN BAY 1
APPENDIX B PHYSICAL BASELINE STUDY: NORTHEAST BAFFIN BAY 1 1 By David B. Fissel, Mar Martínez de Saavedra Álvarez, and Randy C. Kerr, ASL Environmental Sciences Inc. (Feb. 2012) West Greenland Seismic
More informationIrminger Water variability in the West Greenland Current
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L17601, doi:10.1029/2007gl030419, 2007 Irminger Water variability in the West Greenland Current Paul G. Myers, 1 Nilgun Kulan, 1 and Mads
More informationExchange of mass, heat and carbon across the Barents Sea Opening
Exchange of mass, heat and carbon across the Barents Sea Opening Peter M. Haugan University Courses on Svalbard, Longyearbyen, Norway, and Geophysical Institute, University of Bergen, Norway January 13,
More informationLecture 4:the observed mean circulation. Atmosphere, Ocean, Climate Dynamics EESS 146B/246B
Lecture 4:the observed mean circulation Atmosphere, Ocean, Climate Dynamics EESS 146B/246B The observed mean circulation Lateral structure of the surface circulation Vertical structure of the circulation
More informationAnticipated changes in the Nordic Seas marine climate: Scenarios for 2020, 2050, and 2080.
Anticipated changes in the Nordic Seas marine climate: Scenarios for 2020, 2050, and 2080. By Tore Furevik 1, Helge Drange 2, and Asgeir Sorteberg 1,3 1 Geophysical Institute, University of Bergen 2 Nansen
More informationThe Bremen NOAC observing system in the subpolar North Atlantic
US AMOC 2014, Seattle The Bremen NOAC observing system in the subpolar North Atlantic Dagmar Kieke, Monika Rhein, Achim Roessler, Christian Mertens, Reiner Steinfeldt, and Linn Schneider NOAC North Atlantic
More informationDense water plumes SW off Spitsbergen Archipelago (Arctic) in
Dense water plumes SW off Spitsbergen Archipelago (Arctic) in 2014-2017 Bensi Manuel 1, Langone L. 2, Kovacevic V. 1, Ursella L. 1, Goszczko I. 5, Rebesco M. 1, De Vittor C. 1, Aliani S. 2, Miserocchi
More informationThe North Atlantic Oscillation: Climatic Significance and Environmental Impact
1 The North Atlantic Oscillation: Climatic Significance and Environmental Impact James W. Hurrell National Center for Atmospheric Research Climate and Global Dynamics Division, Climate Analysis Section
More informationHeat and freshwater budgets of the Nordic seas computed from atmospheric reanalysis and ocean observations
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116,, doi:10.1029/2011jc006939, 2011 Heat and freshwater budgets of the Nordic seas computed from atmospheric reanalysis and ocean observations O. H. Segtnan, 1 T.
More informationBarotropic instability in the West Spitsbergen Current
Click Here for Full Article JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115,, doi:10.1029/2009jc005996, 2010 Barotropic instability in the West Spitsbergen Current S. H. Teigen, 1 F. Nilsen, 1,2 and B. Gjevik
More informationONR Chair in Arctic Marine Science
ONR Chair in Arctic Marine Science Robert H. Bourke Department of Oceanography Naval Postgraduate School 833 Dyer Road, Bldg. 232, Rm. 328 Monterey, CA 93943-5122 Voice: (831) 656-2962 fax: (831) 656-2712
More informationDirected Reading. Section: Ocean Currents. a(n). FACTORS THAT AFFECT SURFACE CURRENTS
Skills Worksheet Directed Reading Section: Ocean Currents 1 A horizontal movement of water in a well-defined pattern is called a(n) 2 What are two ways that oceanographers identify ocean currents? 3 What
More informationTowards a more saline North Atlantic and a fresher Arctic under global warming
GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L21712, doi:10.1029/2006gl027264, 2006 Towards a more saline North Atlantic and a fresher Arctic under global warming I. Bethke, 1,2,3 T. Furevik, 2,3 and H. Drange
More informationChapter 6. Antarctic oceanography
Chapter 6 Antarctic oceanography The region of the world ocean bordering on Antarctica is unique in many respects. First of all, it is the only region where the flow of water can continue all around the
More informationIODP Proposal Cover Sheet 915 -
IODP Proposal Cover Sheet 915 - Pre North Atlantic Fjord Sediment Archives Received for: 2017-04-03 Title Proponents Fjord sediment archives: assessing the recent (post LGM) millennial to sub-decadal scale
More informationTitle. Author(s)Maslowski, Wieslaw. Citation 地球温暖化による劇変を解明する. 平成 20 年 6 月 24 日. 札幌市. Issue Date Doc URL. Type.
Title When will Summer Arctic Sea Ice Disappear? Author(s)Maslowski, Wieslaw Citation 地球温暖化による劇変を解明する. 平成 20 年 6 月 24 日. 札幌市 Issue Date 2008-06-24 Doc URL http://hdl.handle.net/2115/34395 Type conference
More informationNon-linear patterns of eddy kinetic energy in the Japan/East Sea
Non-linear patterns of eddy kinetic energy in the Japan/East Sea O.O. Trusenkova, D.D. Kaplunenko, S.Yu. Ladychenko, V.B. Lobanov V.I.Il ichev Pacific Oceanological Institute, FEB RAS Vladivostok, Russia
More informationPhysical Qualification and Quantification of the Water Masses in the Kongsfjorden- Krossfjorden System Cross Section
061215-086 1 Physical Qualification and Quantification of the Water Masses in the Kongsfjorden- Krossfjorden System Cross Section A.A. Piehl Harms 1, V. Tverberg 2, H. Svendsen 1, (1)Geophysical Institute,
More informationPathways of eddies in the South Atlantic Ocean revealed from satellite altimeter observations
GEOPHYSICAL RESEARCH LETTERS, VOL. 33,, doi:10.1029/2006gl026245, 2006 Pathways of eddies in the South Atlantic Ocean revealed from satellite altimeter observations Lee-Lueng Fu 1 Received 8 March 2006;
More informationThe Arctic Ocean Climate a balance between local radiation, advected heat and freshwater
The Arctic Ocean Climate a balance between local radiation, advected heat and freshwater Bert Rudels Finnish Meteorological Institute, Helsinki, Finland French Arctic Initiative, Collège de France, Paris,
More informationAnnual and interannual variability of sea level in the northern North Atlantic Ocean
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. C6, 3204, doi:10.1029/2002jc001459, 2003 Annual and interannual variability of sea level in the northern North Atlantic Ocean Denis L. Volkov and Hendrik
More informationThe Arctic Energy Budget
The Arctic Energy Budget The global heat engine [courtesy Kevin Trenberth, NCAR]. Differential solar heating between low and high latitudes gives rise to a circulation of the atmosphere and ocean that
More informationAdvancements and Limitations in Understanding and Predicting Arctic Climate Change
Advancements and Limitations in Understanding and Predicting Arctic Climate Change Wieslaw Maslowski Naval Postgraduate School Collaborators: Jaclyn Clement Kinney, Rose Tseng, Timothy McGeehan - NPS Jaromir
More informationOn the world-wide circulation of the deep water from the North Atlantic Ocean
Journal of Marine Research, 63, 187 201, 2005 On the world-wide circulation of the deep water from the North Atlantic Ocean by Joseph L. Reid 1 ABSTRACT Above the deeper waters of the North Atlantic that
More informationNational Oceanography Centre. Research & Consultancy Report No. 43
National Oceanography Centre Research & Consultancy Report No. 43 State of the eastern North Atlantic subpolar gyre: The Extended Ellett Line Programme Annual Report No. 2 N P Holliday 1 and S Gary 2 2014
More information4/29/2011. Mid-latitude cyclones form along a
Chapter 10: Cyclones: East of the Rocky Mountain Extratropical Cyclones Environment prior to the development of the Cyclone Initial Development of the Extratropical Cyclone Early Weather Along the Fronts
More informationDissertation for the degree philosophiae doctor (PhD) at the University of Bergen
Dissertation for the degree philosophiae doctor (PhD) at the University of Bergen Dissertation date: Preface An introductory part and a collection of papers constitute my thesis presented in partial fulfilment
More informationRecent and future changes of the Arctic sea-ice cover
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L20503, doi:10.1029/2008gl034813, 2008 Recent and future changes of the Arctic sea-ice cover Lars H. Smedsrud, 1 Asgeir Sorteberg, 1 and
More informationClimate Variability Studies in the Ocean
Climate Variability Studies in the Ocean Topic 1. Long-term variations of vertical profiles of nutrients in the western North Pacific Topic 2. Biogeochemical processes related to ocean carbon cycling:
More informationSerial No. N5876 NAFO SCR Doc. 11/001 SCIENTIFIC COUNCIL MEETING JUNE Oceanographic Investigations off West Greenland 2010
NOT TO BE CITED WITHOUT PRIOR REFERENCE TO THE AUTHOR(S) Northwest Atlantic Fisheries Organization Serial No. N5876 NAFO SCR Doc. 11/001 SCIENTIFIC COUNCIL MEETING JUNE 2011 Oceanographic Investigations
More informationAn Isopycnal View of the Nordic Seas Hydrography with focus on Properties of the Lofoten Basin.
An Isopycnal View of the Nordic Seas Hydrography with focus on Properties of the Lofoten Basin. T. Rossby a*, Vladimir Ozhigin b, Victor Ivshin b, and Sheldon Bacon c a Graduate School of Oceanography,
More informationBistability of the Atlantic subpolar gyre in a coarse-resolution climate model
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L24605, doi:10.1029/2007gl031732, 2007 Bistability of the Atlantic subpolar gyre in a coarse-resolution climate model A. Levermann 1,2
More informationOn the origin and propagation of Denmark Strait Overflow Water Anomalies in the Irminger Basin
On the origin and propagation of Denmark Strait Overflow Water Anomalies in the Irminger Basin Kerstin Jochumsen 1, Detlef Quadfasel 1, Manuela Köllner 1,2, Stephen Dye 3,4, Bert Rudels 5 and Heðinn Valdimarsson
More informationS12. The Arctic Ocean and Nordic Seas: Supplementary Materials
C H A P T E R S12 The Arctic Ocean and Nordic Seas: Supplementary Materials FIGURE S12.1 Principal currents of the Nordic Seas. Shaded currents show upper ocean circulation; thin black arrows show deep
More informationHydrography and biological resources in the western Bering Sea. Gennady V. Khen, Eugeny O. Basyuk. Pacific Research Fisheries Centre (TINRO-Centre)
Hydrography and biological resources in the western Bering Sea Gennady V. Khen, Eugeny O. Basyuk Pacific Research Fisheries Centre (TINRO-Centre) Bering Sea: deep-sea basin, shelf, and US-Russia convention
More informationEurasian Snow Cover Variability and Links with Stratosphere-Troposphere Coupling and Their Potential Use in Seasonal to Decadal Climate Predictions
US National Oceanic and Atmospheric Administration Climate Test Bed Joint Seminar Series NCEP, Camp Springs, Maryland, 22 June 2011 Eurasian Snow Cover Variability and Links with Stratosphere-Troposphere
More informationBaroclinic instability in the West Spitsbergen Current
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 116,, doi:10.1029/2011jc006974, 2011 Baroclinic instability in the West Spitsbergen Current S. H. Teigen, 1 F. Nilsen, 1,2 R. Skogseth, 1 B. Gjevik, 3 and A. Beszczynska
More informationHalocline structure in the Canada Basin of the Arctic Ocean
GEOPHYSICAL RESEARCH LETTERS, VOL. 32, L03605, doi:10.1029/2004gl021358, 2005 Halocline structure in the Canada Basin of the Arctic Ocean Koji Shimada, Motoyo Itoh, and Shigeto Nishino Institute of Observational
More informationICES Journal of Marine Science
ICES Journal of Marine Science ICES Journal of Marine Science (2012), 69(5), 833 840. doi:10.1093/icesjms/fss075 Atlantic water temperature and climate in the Barents Sea, 2000 2009 Vladimir D. Boitsov,
More informationOn the Circulation of Atlantic Water in the Arctic Ocean
2352 J O U R N A L O F P H Y S I C A L O C E A N O G R A P H Y VOLUME 43 On the Circulation of Atlantic Water in the Arctic Ocean MICHAEL A. SPALL Woods Hole Oceanographic Institution, Woods Hole, Massachusetts
More informationArne Biastoch Helmholtz Centre for Ocean Research Kiel. Modelling the Agulhas Current and its Coupling with the Atlantic Circulation
Arne Biastoch Helmholtz Centre for Ocean Research Kiel Modelling the Agulhas Current and its Coupling with the Atlantic Circulation The Agulhas System as a Key Region of the Global Oceanic Circulation
More informationLoss of sea ice during winter north of Svalbard
Tellus A: Dynamic Meteorology and Oceanography ISSN: (Print) 16-87 (Online) Journal homepage: http://www.tandfonline.com/loi/zela2 Loss of sea ice during winter north of Svalbard Ingrid H. Onarheim, Lars
More informationFronts in November 1998 Storm
Fronts in November 1998 Storm Much of the significant weather observed in association with extratropical storms tends to be concentrated within narrow bands called frontal zones. Fronts in November 1998
More informationBarents Sea ice cover reflects Atlantic inflow
Barents Sea ice cover reflects Atlantic inflow M. Årthun a,b,,t.eldevik a,b,l.h.smedsrud c,b, Ø. Skagseth d,b a Geophysical Institute, University of Bergen, Bergen, Norway b Bjerknes Centre for Climate
More informationRecent Variability in Western Boundary Currents on the Atlantic Slope from Moored Measurements and Altimetry
Fisheries and Oceans Canada Pêches et Océans Canada Canada Recent Variability in Western Boundary Currents on the Atlantic Slope from Moored Measurements and Altimetry John Loder 1, Yuri Geshelin 1, Igor
More informationStability and forcing of the Iceland-Faroe inflow of water, heat, and salt to the Arctic
doi:10.5194/os-6-1013-2010 Author(s) 2010. CC Attribution 3.0 License. Ocean Science Stability and forcing of the Iceland-Faroe inflow of water, heat, and salt to the Arctic B. Hansen 1, H. Hátún 1, R.
More informationClimate change impacts on the waters around the UK and Ireland: Salinity
MARINE CLIMATE CHANGE IMPACTS PARTNERSHIP: SCIENCE REVIEW Submitted June 2013 Published online 28 November 2013 doi:10.14465/2013.arc07.060-066 Climate change impacts on the waters around the UK and Ireland:
More informationICE DRIFT IN THE FRAM STRAIT FROM ENVISAT ASAR DATA
ICE DRIFT IN THE FRAM STRAIT FROM ENVISAT ASAR DATA Stein Sandven (1), Kjell Kloster (1), and Knut F. Dagestad (1) (1) Nansen Environmental and Remote Sensing Center (NERSC), Thormøhlensgte 47, N-5006
More informationMERIDIONAL OVERTURNING CIRCULATION: SOME BASICS AND ITS MULTI-DECADAL VARIABILITY
MERIDIONAL OVERTURNING CIRCULATION: SOME BASICS AND ITS MULTI-DECADAL VARIABILITY Gokhan Danabasoglu National Center for Atmospheric Research OUTLINE: - Describe thermohaline and meridional overturning
More informationMean Stream-Coordinate Structure of the Kuroshio Extension First Meander Trough
Mean Stream-Coordinate Structure of the Kuroshio Extension First Meander Trough 6 March, 2008 Penelope J. Howe, Kathleen A. Donohue, and D. Randolph Watts Graduate School of Oceanography University of
More information1. Introduction 2. Organization of the meeting 3. Project aims, hypothesis and structure 4. AWAKE phases 5. Project prolongation? 6.
Second meeting 1. Introduction 2. Organization of the meeting 3. Project aims, hypothesis and structure 4. AWAKE phases 5. Project prolongation? 6. Additional measurements? 7. Papers!!!!! 8. EGU 2015 9.
More informationWater mass modification in an Arctic fjord through cross-shelf exchange: The seasonal hydrography of Kongsfjorden, Svalbard
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110,, doi:10.1029/2004jc002757, 2005 Water mass modification in an Arctic fjord through cross-shelf exchange: The seasonal hydrography of Kongsfjorden, Svalbard Finlo
More informationOn the structure and dynamics of the water in the Słupsk Furrow*
On the structure and dynamics of the water in the Słupsk Furrow* OCEANOLOGIA, 39(1), 1997. pp.35 54. 1997, by Institute of Oceanology PAS. KEYWORDS Water transport Mesoscale dynamics Mixing Jan Piechura,
More information