Cruise Report R/V Oceania, AREX 2007
|
|
|
- Melina Lloyd
- 5 years ago
- Views:
Transcription
1 Powstańców Warszawy 55, PL Sopot, P.O. Box 68 March 15, 2008 Cruise Report R/V Oceania, AREX 2007 Ship: R/V Oceania Cruise: AREX 2007 Dates: Port Calls: Gdansk (Poland) Longyearbyen (Spitsbergen) Number of Scientist: 14 Chief Scientist: dr Waldemar Walczowski Principal Project: DAMOCLES WP3 Research Area: Greenland Sea 1
2 Damocles - WP3. Oceans: Task 3.1 Input Function, Task 3.2 Shelf/Basin Exchange Jan Piechura, Waldemar Walczowski, Jaromir Jakacki, Robert Osiński, Piotr Wieczorek, Ilona Goszczko, Małgorzata Kitowska (IO PAS). 1. Observations in 2007 AREX 2007 cruise of the R/V Oceania was performed in the period of June August CTD (conductivity, temperature, depth) profiles along 11 sections were done (Fig.1, Tab. 1). As in previous years sections were perpendicular to the general direction of the Atlantic Water flow. The AW domain in the Greenland Sea is situated between the Barents Sea slope and system of underwater ridges: Mohns Ridge and Knipovich Ridge. Through convergence of the isobaths in the northern part, AW domain forms a wedge, wide in the southern part and narrower in the northern end. Complicated bottom topography significantly influences the currents pattern and structure. Coverage in the southern part of the investigated area is spare in comparison to the northern one. This causes less accurate horizontal distribution of properties in the region south of the Bear Island. As before, our main effort was concentrated in the northern part of the Atlantic Domain where processes controlling the AW inflow into Arctic Ocean through the Fram Strait and the westward recirculation occur. For CTD measurements the Seabird SBI9/11plus probe was used. The probe was serviced before the cruise. Temperature and conductivity sensors were calibrated by the Sea-Bird Electronics service. Water samples collected by means of the rosette water sampler SBE32 were analysed at IOPAS laboratory with the Guildline Autosal 8400A. Currents measurements by means of the lowered Acoustic Doppler Current Profiler (LADCP) were performed at the CTD stations. The self-recording 300 khz RDI device was used to profile entire water column during the standard CTD casts. During the whole cruise sustained currents measurements by the ship-mounted ADCP, RDI 150 khz were performed. 2
3 Figure 1: Measurements performed during Arex 2007 experiment Some preliminary results As formerly, 2007 cruise results acknowledged that there are two branches of Atlantic Water in the Greenland Sea which flow northward. First, main branch of the West Spitsbergen Current flows along the Barents Sea continental slope and Spitsbergen shelf break. Second, colder and less saline branch continues along the Mohns and Knipovich Ridges as a jet stream of the Arctic Front. The force which is responsible for convergence of both branches of AW west of the Spitsbergen coast is bottom topography. Moreover, merely a part of northward running AW moves into the Arctic Ocean, primarily along the Spitsbergen slope; western branch of AW mostly recirculates westward as Return Atlantic Current. AW enters into the Greenland Sea as a wide flow of warm and more saline water separated from the Norwegian coast by the less saline Norwegian Coastal Current. Due west, the Arctic Front located over the Mohns Ridge separates AW from colder and less saline Arctic Waters. Appreciable part of AW flowing along the Norwegian coast continues eastward into the Barents Sea, the rest goes on northward as two divided arms. One of them is related to the Barents Sea slope. Jet streams of the Arctic Front form the second arm of AW. Salinity and temperature of the eastern and western branch are considerably different; AW carried by the eastern flow is much warmer and more saline than the western one. Distance between the branches in the southern part of WSC is about 150 km and in the northern part - only 30 km. In central and northern part of the WSC recirculation of AW
4 occurs. Only part of AW, which flows along the shelf break, continues northward through the Fram Strait into the Arctic Ocean. Measurements at all sections of the area between northern Norway and the Fram Strait performed in summer 2007 show decrease of the AW temperature and salinity. In 2006 the extreme high temperatures of the West Spitsbergen Current core were observed and lower temperatures of the West Spitsbergen Current in 2007 was not so surprising. Also, the extreme northward extension of the warm Atlantic Water was observed in 2006 (Fig 5a). In 2007 the 5 isotherm at 100 dbar moved back to its position from 2005 (Fig 5b). In summer 2007 Atlantic Water was colder than in 2006 (Fig 5, 6). For example at section N (Fig 3 and Fig 6) mean temperature and salinity at 200 dbar was in 2006 respectively 4.50 C and 35.13, whereas in 2007 it has dropped to 3,84 C and However, at this level temperature value was still 0.69 C higher than mean, and both temperature and salinity trends for this period are positive. Fig. 7 presents the distribution of baroclinic currents kinetic energy and baroclinic currents at 100 dbar (calculated for the reference level of 1000 m) in summer Intensive inflow into the Greenland Sea over the Mohn Ridge and division of this inflow is well visible. Fig. 2. T-S diagram for all stations: a) in summer 2006 and b) in summer
5 Fig. 3. Potential temperature (upper panel) and salinity in summer 2007 at section N (76 30 N). Fig. 4. Potential temperature (upper panel) and salinity in summer 2007 at section Z (~78 N). 5
6 Fig. 5. Temperature at 100 dbar in June-July 2006 (left hand side) and Fig. 6. Mean salinity (upper panel) and mean temperature in summer (July) at section N (76 30 N) at 200 m, between E. 6
7 Fig. 7. June-July Baroclinic flow kinetic energy distribution (colour scale), and baroclinic currents at 100 dbar. Reference level 1000 m. Table 1: CTD stations and some of their main parameters. There were 11 regular sections performed in No Station Latitude Longitude Date, Time Depth File Section V1 1 V ' N ' E 19-Jun :18: ar07_001 2 V ' N ' E 19-Jun :11: ar07_002 3 V ' N ' E 19-Jun :58: ar07_003 4 V ' N ' E 20-Jun :54: ar07_004 5 V ' N ' E 20-Jun :35: ar07_005 6 V ' N ' E 20-Jun :35: ar07_006 7 V ' N ' E 20-Jun :33: ar07_007 8 V ' N ' E 20-Jun :43: ar07_008 9 V ' N ' E 20-Jun :44: ar07_ V ' N ' E 20-Jun :06: ar07_010 7
8 11 V ' N ' E 20-Jun :48: ar07_ V ' N ' E 20-Jun :21: ar07_ V ' N ' E 21-Jun :03: ar07_ V ' N ' E 21-Jun :07: ar07_ V ' N ' E 21-Jun :06: ar07_ V ' N ' E 21-Jun :04: ar07_ V ' N ' E 21-Jun :55: ar07_ V ' N ' E 21-Jun :47: ar07_ V ' N ' E 21-Jun :25:38 70 ar07_019 Section H 20 H ' N ' E 21-Jun :11: ar07_ H ' N ' E 22-Jun :35: ar07_022a 22 H ' N ' E 22-Jun :52: ar07_ H ' N ' E 22-Jun :57: ar07_ H ' N ' E 22-Jun :29: ar07_ H ' N ' E 22-Jun :09: ar07_ H ' N ' E 22-Jun :16: ar07_ H ' N ' E 22-Jun :47: ar07_ H ' N ' E 22-Jun :29: ar07_ H ' N ' E 22-Jun :01: ar07_ H ' N ' E 22-Jun :55: ar07_ H ' N ' E 23-Jun :50: ar07_ H ' N ' E 23-Jun :36: ar07_ H ' N ' E 23-Jun :19: ar07_ H ' N ' E 23-Jun :13: ar07_ H ' N ' E 23-Jun :12: ar07_ H ' N ' E 24-Jun :12: ar07_ H ' N ' E 24-Jun :38: ar07_ H ' N ' E 24-Jun :31: ar07_ H ' N ' E 24-Jun :48: ar07_ K ' N ' E 25-Jun :08: ar07_ H ' N ' E 25-Jun :29: ar07_ H ' N ' E 25-Jun :01: ar07_042 Section K 43 K ' N ' E 26-Jun :22: ar07_ K ' N ' E 26-Jun :13: ar07_044 Section 0 45 O ' N ' E 29-Jun :37: ar07_ O ' N ' E 29-Jun :19: ar07_ O ' N ' E 29-Jun :11: ar07_ O ' N ' E 29-Jun :22: ar07_048 8
9 49 M ' N ' E 29-Jun :13: ar07_049 Section S 50 S ' N ' E 01-Jul :32: ar07_ S ' N ' E 01-Jul :16: ar07_ S ' N ' E 01-Jul :30: ar07_ S ' N ' E 01-Jul :32: ar07_ S ' N ' E 01-Jul :58:18 95 ar07_ S ' N ' E 01-Jul :15: ar07_ S ' N ' E 02-Jul :40: ar07_ S ' N ' E 02-Jul :41: ar07_ S ' N ' E 02-Jul :54: ar07_ S ' N ' E 02-Jul :23: ar07_ S ' N ' E 02-Jul :33: ar07_ S ' N ' E 02-Jul :55: ar07_ S ' N ' E 02-Jul :38: ar07_ S ' N ' E 02-Jul :36: ar07_ S ' N ' E 03-Jul :19: ar07_ S ' N ' E 03-Jul :23: ar07_ S ' N ' E 03-Jul :03: ar07_ S ' N ' E 03-Jul :30: ar07_ S ' N ' E 03-Jul :21: ar07_068 Section O cd 69 O ' N ' E 07-Jul :45: ar07_ M ' N ' E 07-Jul :14: ar07_ O ' N ' E 07-Jul :14: ar07_ O ' N ' E 07-Jul :33: ar07_ O ' N ' E 07-Jul :47: ar07_ O ' N ' E 07-Jul :53: ar07_ O ' N ' E 08-Jul :12: ar07_ O ' N ' E 08-Jul :33: ar07_ O ' N ' E 08-Jul :54: ar07_ O ' N ' E 08-Jul :13: ar07_ O ' N ' E 08-Jul :41: ar07_ O ' N ' E 08-Jul :10: ar07_ O ' N ' E 08-Jul :09: ar07_ O ' N ' E 08-Jul :40: ar07_082 Section V2 83 V ' N ' E 09-Jul :22:55 30 ar07_ V ' N ' E 09-Jul :05:42 55 ar07_ V ' N ' E 09-Jul :35: ar07_ V ' N ' E 09-Jul :35: ar07_086 9
10 87 V ' N ' E 09-Jul :58: ar07_ V ' N ' E 09-Jul :36: ar07_ V ' N ' E 09-Jul :20: ar07_ V ' N ' E 09-Jul :49: ar07_ V ' N ' E 09-Jul :01: ar07_ V ' N ' E 09-Jul :45: ar07_ V ' N ' E 09-Jul :05:38 60 ar07_093 Section K cd 94 K ' N ' E 10-Jul :33: ar07_ K ' N ' E 10-Jul :51: ar07_ K ' N ' E 10-Jul :39: ar07_ K ' N ' E 10-Jul :45: ar07_ K ' N ' E 10-Jul :27: ar07_ K ' N ' E 10-Jul :15: ar07_ K ' N ' E 10-Jul :24: ar07_100 Section N 101 N ' N ' E 11-Jul :16: ar07_ N ' N ' E 11-Jul :16: ar07_ N ' N ' E 12-Jul :28: ar07_ N ' N ' E 12-Jul :21: ar07_ N ' N ' E 12-Jul :23: ar07_ N ' N ' E 12-Jul :51: ar07_ N ' N ' E 12-Jul :26: ar07_ N ' N ' E 12-Jul :57: ar07_ N ' N ' E 12-Jul :45: ar07_ N ' N ' E 13-Jul :50: ar07_ N ' N ' E 13-Jul :46: ar07_ N ' N ' E 13-Jul :35: ar07_ N ' N ' E 13-Jul :05: ar07_ N1P ' N ' E 13-Jul :21: ar07_ N ' N ' E 13-Jul :49: ar07_ N2p ' N ' E 13-Jul :18: ar07_ N ' N ' E 13-Jul :33: ar07_ N3P ' N ' E 13-Jul :29: ar07_ N ' N ' E 14-Jul :56: ar07_ N4P ' N ' E 14-Jul :44: ar07_120 Section Z 121 Z ' N ' E 14-Jul :14: ar07_ Z ' N ' E 14-Jul :21: ar07_ Z ' N ' E 14-Jul :56: ar07_ Z ' N ' E 14-Jul :53: ar07_124 10
11 125 Z ' N ' E 15-Jul :25: ar07_ Z ' N ' E 15-Jul :03: ar07_ Z ' N ' E 15-Jul :19: ar07_ Z ' N ' E 15-Jul :52: ar07_ Z ' N ' E 15-Jul :17: ar07_ Z ' N ' E 15-Jul :06: ar07_ Z ' N ' E 15-Jul :52: ar07_ Z ' N ' E 15-Jul :15: ar07_ Z ' N ' E 16-Jul :21: ar07_133 Section EB2 134 EB ' N ' E 16-Jul :18: ar07_ EB ' N ' E 16-Jul :37: ar07_ EB ' N ' E 16-Jul :54: ar07_ EB ' N ' E 16-Jul :34: ar07_ EB ' N ' E 17-Jul :54: ar07_ EB ' N ' E 17-Jul :32: ar07_ EB ' N ' E 17-Jul :36: ar07_ EB ' N ' E 17-Jul :59: ar07_ EB ' N ' E 17-Jul :20: ar07_ EB ' N ' E 17-Jul :30: ar07_ EB ' N ' E 18-Jul :55: ar07_ EB ' N ' E 18-Jul :28: ar07_ EB ' N ' E 18-Jul :48: ar07_ EB ' N ' E 18-Jul :46: ar07_ EB ' N ' E 18-Jul :38: ar07_ EB ' N ' E 18-Jul :12: ar07_149 Kongsfjorden 150 KG ' N ' E 18-Jul :38: ar07_150 Section EX 151 EX ' N ' E 20-Jul :19: ar07_ EX ' N ' E 20-Jul :20: ar07_ EX ' N ' E 20-Jul :21: ar07_ EX ' N ' E 20-Jul :25: ar07_ EX ' N ' E 20-Jul :34: ar07_ EX ' N ' E 20-Jul :02: ar07_ EX ' N ' E 20-Jul :36: ar07_ EX ' N ' E 21-Jul :15: ar07_ EX ' N ' E 21-Jul :20: ar07_ EX ' N ' E 21-Jul :31: ar07_160 Section X 161 X ' N ' E 21-Jul :23: ar07_161 11
12 162 X ' N ' E 21-Jul :51: ar07_ X ' N ' E 21-Jul :34: ar07_ X ' N ' E 21-Jul :18: ar07_ X ' N ' E 22-Jul :32: ar07_ X ' N ' E 22-Jul :28: ar07_ X ' N ' E 22-Jul :13: ar07_ X ' N ' E 22-Jul :18: ar07_ X ' N ' E 22-Jul :19: ar07_ X ' N ' E 22-Jul :05: ar07_ X ' N ' E 22-Jul :39: ar07_ X ' N ' E 22-Jul :00: ar07_172 12
Cruise 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)
Cruise 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
Pathways of the Greenland Sea warming
GEOPHYSICAL RESEARCH LETTERS, VOL. 34, L10608, doi:10.1029/2007gl029974, 2007 Pathways of the Greenland Sea warming Waldemar Walczowski 1 and Jan Piechura 1 Received 12 March 2007; revised 23 April 2007;
Prod: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
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
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
Changes 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.
Advancements 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
On 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
Observed 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
Red Sea - Dead Sea Water Conveyance Study Program Additional Studies
Red Sea - Dead Sea Water Conveyance Study Program Additional Studies Red Sea Study Final Report Annex 1 Field and laboratory activities carried out during the study and their results July 213 TABLE OF
The California current is the eastern boundary current that lies to the west of
I. INTORDUCTION A. California Current System The California current is the eastern boundary current that lies to the west of North America. The California current flows from north, Washington, to south,
Directed 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
PUBLICATIONS. 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
Title. 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
Atlantic 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
The 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
Baltic Sea Research Institute
Baltic Sea Research Institute Warnemuende (IOW) Cruise Report No. 44/96/ 04 R/V "A.v.Humboldt" MESODYN Cruise 01 to 12 March 1996 Stolpe Furrow / Baltic Sea This report is based on preliminary data and
Arctic 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
Upper 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
The East Greenland Current and its contribution to the Denmark Strait overflow
ICES Journal of Marine Science, 59: 1133 1154. 2002 doi:10.1006/jmsc.2002.1284, available online at http://www.idealibrary.com on The East Greenland Current and its contribution to the Denmark Strait overflow
Dense 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
EXPORT PATHWAYS FROM THE SUBPOLAR NORTH ATLANTIC OCEAN
CRUISE REPORT EXPORT PATHWAYS FROM THE SUBPOLAR NORTH ATLANTIC OCEAN R/V Oceanus Cruise OC 395-2 July 9-23, 2003 1. Introduction and Objectives The importance of the pathways of the ocean s meridional
Supplemental Material
10.1175/JPO-D-17-0239.1 TSUBOUCHI ET AL. The Arctic Ocean Seasonal Cycles of Heat and Freshwater Fluxes: Observation-Based Inverse Estimates Takamasa Tsubouchi, a Sheldon Bacon, a Yevgeny Aksenov, a Alberto
The Deep Overflow through the Faroe Bank Channel
ICES 1999 Annual Science Conference C M 1999/L:19 Nordic Seas Exchanges The Deep Overflow through the Faroe Bank Channel Svein Østerhus, University of Bergen, Norway, svein@gfi.uib.no Bogi Hansen & Regin
Polish-Norwegian Research Fund. MINUTES Kick Off Meeting - AWAKE PNRF-234-A I-1/07
MINUTES Kick Off Meeting - AWAKE PNRF-23-A I-1/07 Date: January 11-12, Place: Institute of Oceanology PAS, Poland, Sopot, Powstancow Warszawy 55 Participants: As per the attached attendance list Monday,
APPENDIX 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
ICES 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,
MINUTES Progress meeting of the AWAKE Project November 4-5 th, 2010, Sopot
MINUTES Progress meeting of the AWAKE Project November 4-5 th, 2010, Sopot Thursday, November 4 th - meeting started at 02:00 pm. Jan Piechura (IOPAS, project coordinator) welcomed participants, the meeting
The 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
Isopycnal 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
Temperature 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
Exchange 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,
Generation and Evolution of Internal Waves in Luzon Strait
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Generation and Evolution of Internal Waves in Luzon Strait Ren-Chieh Lien Applied Physics Laboratory University of Washington
Analysis of Physical Oceanographic Data from Bonne Bay, September 2002 September 2004
Physics and Physical Oceanography Data Report -1 Analysis of Physical Oceanographic Data from Bonne Bay, September September Clark Richards and Brad deyoung Nov. 9 Department of Physics and Physical Oceanography
Water-mass formation and distribution in the Nordic Seas during the 1990s
ICES Journal of Marine Science, 61: 846e863 (24) doi:1.116/j.icesjms.24.5.3 Water-mass formation and distribution in the Nordic Seas during the 199s Johan Blindheim and Francisco Rey Blindheim, J., and
Johan Blindheim. Institute of Marine Research P.O.Box 1870 N-5011 Bergen - Nordnes Norway ABSTRACT
Not to be cited without prior reference to the author. International Council for the Exploration of the Sea C.M. 1986/C:14 Hydrography Commitee ARCTIC INTERMEDIATE WATER IN THE NORWEGIAN SEA by Johan Blindheim
Proceedings of Meetings on Acoustics
Proceedings of Meetings on Acoustics Volume 19, 2013 http://acousticalsociety.org/ ICA 2013 Montreal Montreal, Canada 2-7 June 2013 Acoustical Oceanography Session 2aAO: Seismic Oceanography 2aAO8. Current-eddy
Geostrophic Current Analysis through the CenCal Box
Geostrophic Current Analysis through the CenCal Box LT Sean P. Yemm OC357 Winter Quarter, 23 I. Introduction A. California Current System The California Current System is composed of numerous jets, filaments,
LET 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
SCIENTIFIC 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
Circulation 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;
Observations 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,
Forcing 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
53 contributors for 35 individual reports in 2009 show 5% of figures today
A Group Approach to Understanding Ecosystem Dynamics in the Northeast Pacific Ocean William Crawford and James Irvine, Fisheries and Oceans Canada (DFO) * * * 53 contributors for 35 individual reports
Ocean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity?
Name: Date: TEACHER VERSION: Suggested Student Responses Included Ocean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity? Introduction The circulation
National 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
A 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
Interannual changes in the zooplankton community structure on the southeastern Bering Sea shelf and Chukchi Sea during summers of
Interannual changes in the zooplankton community structure on the southeastern Bering Sea shelf and Chukchi Sea during summers of 1991 29 22 27 Shiberia Chukchi Sea Alaska Pacific Summer Water Bering Sea
On 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,
IWISE: Observations of Internal Wave and Tide Generation in the Luzon Strait Using Shipboard Surveys and Oceanographic Moorings
DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. IWISE: Observations of Internal Wave and Tide Generation in the Luzon Strait Using Shipboard Surveys and Oceanographic
Hydrographic Structure and Transport of Intermediate Water in the Kuroshio Region off the Boso Peninsula, Japan
Journal of Oceanography, Vol. 60, pp. 487 to 503, 2004 Hydrographic Structure and Transport of Intermediate Water in the Kuroshio Region off the Boso Peninsula, Japan KOSEI KOMATSU 1 *, YUTAKA HIROE 1,
Observation of Oceanic Structure around Tosa-Bae Southeast of Shikoku
Journal of Oceanography Vol. 50, pp. 543 to 558. 1994 Observation of Oceanic Structure around Tosa-Bae Southeast of Shikoku YOSHIHIKO SEKINE, HARUKI OHWAKI and MOTOYA NAKAGAWA Institute of Oceanography,
The Baffin Island and West Greenland. Current Systems in Northern Baffin Bay: Synoptic Observations and Climatological. Context
The Baffin Island and West Greenland Current Systems in Northern Baffin Bay: Synoptic Observations and Climatological Context Andreas Münchow 5 University of Delaware, Newark, Delaware, U.S.A. Kelly K.
Homework 5: Background Ocean Water Properties & Stratification
14 August 2008 MAR 110 HW5: Ocean Properties 1 Homework 5: Background Ocean Water Properties & Stratification The ocean is a heterogeneous mixture of water types - each with its own temperature, salinity,
Baroclinic 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
Barotropic 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
Hydrography and circulation west of Sardinia in June 2014
https://doi.org/10.5194/os-13-889-2017 Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Hydrography and circulation west of Sardinia in June 2014 Michaela Knoll
Serial No. N4167 NAFO SCR Doc. 99/95. SCIENTIFIC COUNCIL MEETING SEPTEMBER 1999 (Joint NAFO/ICES/PICES Symposium on Pandalid Shrimp Fisheries)
NOT TO CITED WITHOUT PRIOR REFERENCE TO THE AUTHOR(S) Northwest Atlantic Fisheries Organization Serial No. N4167 NAFO SCR Doc. 99/95 SCIENTIFIC COUNCIL MEETING SEPTEMBER 1999 (Joint NAFO/ICES/PICES Symposium
On the fate of the Antarctic Slope Front and the origin of the Weddell Front
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109,, doi:10.1029/2003jc002053, 2004 On the fate of the Antarctic Slope Front and the origin of the Weddell Front Karen J. Heywood and Alberto C. Naveira Garabato
Physical 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,
2004 State of the Ocean: Physical Oceanographic Conditions in the Newfoundland and Labrador Region
Canadian Science Advisory Secretariat Science Advisory Report 25/18 Research vessel CCGS Teleost 24 State of the Ocean: Physical Oceanographic Conditions in the Newfoundland and Labrador Region Background
Heat 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.
ICES 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,
How to form halocline water?
How to form halocline water? Atlantic water - cannot form Halocline water simply by mixing (Aagaard, 1981) Surface Water Adapted from Steele and Boyd, 1998 ADVECTIVE HC Temp Fresh Salty Aagaard et al,
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution
CRUISE SUMMARY REPORT
CRUISE SUMMARY REPORT Centre: DOD Ref. No.: FOR COLLATIMG CENTRE USE Is data exchange restricted Yes In part No Page 1 SHIP enter the full name and international radio call sign of the ship from which
The fieldwork during the Polarstern cruise ANT XVI/2 as a contribution to the study of bottom water formation and sea ice transport in the Weddell Sea
The fieldwork during the Polarstern cruise ANT XVI/2 as a contribution to the study of bottom water formation and sea ice transport in the Weddell Sea Fahrbach, E 1, S. Harms 2, H. Hellmer 1, A. Jenkins
DIAMIX an experimental study of diapycnal deepwater mixing in the virtually tideless Baltic Sea
BOREAL ENVIRONMENT RESEARCH 7: 363 369 ISSN 1239-6095 Helsinki 23 December 2002 2002 DIAMIX an experimental study of diapycnal deepwater mixing in the virtually tideless Baltic Sea Anders Stigebrandt 1),
A numerical ocean circulation model of the Norwegian and Greenland Seas
Prog.Oceanog. VoL 27, pp. 365-402, 1991. 0079-6611/91$0.00+ 30 Printed M Great Britain. All rights reserved. 01991 Pergaman Press plc A numerical ocean circulation model of the Norwegian and Greenland
Chapter 6. Antarctic oceanography
Chapter 6 Antarctic oceanography The region of the world ocean bordering on Antarctica is unique in many respects. First of all, it is the only region where the flow of water can continue all around the
Meridional circulation in the western coastal zone: Qinyan Liu +$ & Rui Xin Huang +* Guangzhou, China. February 2, 2010
Meridional circulation in the western coastal zone: II. The regulation by pressure gradient set up through basin scale circulation and the western boundary current transport Qinyan Liu +$ & Rui Xin Huang
introduction National Council of Teachers of Mathematics.
1 introduction The National Science Education Standards developed under the auspices of the National Research Council specifies Science as Inquiry as major content standard for all grade levels. The activities
Hydrography 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
Variations of Kuroshio Intrusion and Internal Waves at Southern East China Sea
Variations of Kuroshio Intrusion and Internal Waves at Southern East China Sea Ren-Chieh Lien Applied Physics Laboratory University of Washington Seattle, Washington 98105 phone: (206) 685-1079 fax: (206)
Variability 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
On climatological mass, heat, and salt transports through the Barents Sea and Fram Strait from a pan-arctic coupled ice-ocean model simulation
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 109,, doi:10.1029/2001jc001039, 2004 On climatological mass, heat, and salt transports through the Barents Sea and Fram Strait from a pan-arctic coupled ice-ocean
Synoptic Flow and Density Observations near an Arctic Shelf Break
1402 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 27 Synoptic Flow and Density Observations near an Arctic Shelf Break ANDREAS MÜNCHOW Institute of Marine and Coastal Sciences, Rutgers University, New Brunswick,
Cruise and Data Report: R/V Shana Rae operations in support of April 2015 AirSWOT campaign, April 17-20, 2015
Cruise and Data Report: R/V Shana Rae operations in support of April 2015 AirSWOT campaign, April 17-20, 2015 J. Thomas Farrar, Benjamin Hodges, Sebastien Bigorre Physical Oceanography Department Woods
General 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 -
Wintertime 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.
ICEBERGS IN THE BARENTS SEA
ICEBERGS IN THE BARENTS SEA Mapping ice and snow conditions in the Barents Sea, part-report 1 Icebergs Leif J Dalsgaard, Petroleum Safety Authority Norway Tore Syversen, Sintef Mars Goals Achieve better
Forecasting Polar Lows. Gunnar Noer The Norwegian Meteorological Institute in Tromsø
Forecasting Polar Lows Gunnar Noer The Norwegian Meteorological Institute in Tromsø Longyearbyen Hopen Bear Island Jan Mayen Tromsø Gunnar Noer Senior forecaster / developer for polar meteorology The Norwegian
Supplement of Transport of volume, heat, and salt towards the Arctic in the Faroe Current
Supplement of Ocean Sci., 11, 743 757, 2015 http://www.ocean-sci.net/11/743/2015/ doi:10.5194/os-11-743-2015-supplement Author(s) 2015. CC Attribution 3.0 License. Supplement of Transport of volume, heat,
Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.
Earth s Oceans & Ocean Floor Date: Feelin Blue What are Earth s five main oceans? Almost of Earth is covered by water. On a map, the continents appear as huge islands surrounded by a vast global ocean.
UHI Research Database pdf download summary
UHI Research Database pdf download summary Effects of glacier runoff and wind on surface layer dynamics and Atlantic Water exchange in Kongsfjorden, Svalbard; a model study Sundfjord, Arild; Albretsen,
Upper 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
Problems 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
ARTICLE IN PRESS. Deep-Sea Research II
Deep-Sea Research II 57 () 73 737 Contents lists available at ScienceDirect Deep-Sea Research II journal homepage: www.elsevier.com/locate/dsr The circulation and water masses of the Antarctic shelf and
SIO 210 Problem Set 2 October 17, 2011 Due Oct. 24, 2011
SIO 210 Problem Set 2 October 17, 2011 Due Oct. 24, 2011 1. The Pacific Ocean is approximately 10,000 km wide. Its upper layer (wind-driven gyre*) is approximately 1,000 m deep. Consider a west-to-east
1. 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.
Serial 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
Canadian Ice Service
Canadian Ice Service Key Points and Details concerning the 2009 Arctic Minimum Summer Sea Ice Extent October 1 st, 2009 http://ice-glaces.ec.gc.ca 1 Key Points of Interest Arctic-wide The Arctic-wide minimum
Regional 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
Benefits of Spatial Collaboration in Arctic Research Project Using ArcGIS Online
Benefits of Spatial Collaboration in Arctic Research Project Using ArcGIS Online Dr. Nataliya Marchenko Prof. Aleksey Marchenko The University Centre in Svalbard, Longyearbyen, Norway Arctic Technology
Results of oceanographic analyses conducted under JARPA and possible evidence of environmental changes.
SC/D06/J30 Results of oceanographic analyses conducted under JARPA and possible evidence of environmental changes. Tomowo Watanabe*, Takashi Yabuki**, Toshio Suga**, Kimio Hanawa**, Koji Matsuoka*** and
Global Weather Trade Winds etc.notebook February 17, 2017
Global Weather 1 north pole northern hemisphere equator southern hemisphere south pole 2 We have seasons because of the Earth's tilt The seasons are opposite in the northern and southern hemispheres winter
Circulation and Transport in the Western Boundary Currents at Cape Farewell, Greenland
1854 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 39 Circulation and Transport in the Western Boundary Currents at Cape Farewell, Greenland N. P. HOLLIDAY, S.BACON, J.ALLEN, AND E.
The Arctic Crossroads
The Arctic Crossroads The Influence of the Mendeleev Ridge and the Chukchi Borderland on the Large-scale Circulation of the Arctic Ocean Rebecca Woodgate and Knut Aagaard, University of Washington Jim
Laboratory Benchmark for Models of the Transport in the Kara Sea
Laboratory Benchmark for Models of the Transport in the Kara Sea Thomas McClimans SINTEF Civil and Environmental Engineering N-7465 Trondheim Norway voice: +47 73592417 fax: +47 73 592376 email: thomas.mcclimans@civil.sintef.no
ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY. Lecture 2
ATOC 5051 INTRODUCTION TO PHYSICAL OCEANOGRAPHY Lecture 2 Ocean basins and relation to climate Learning objectives: (1)What are the similarities and differences among different ocean basins? (2) How does