Spreading and reproduction limitations of the American comb jelly Mnemiopsis leidyi in the Baltic Sea

Size: px
Start display at page:

Download "Spreading and reproduction limitations of the American comb jelly Mnemiopsis leidyi in the Baltic Sea"

Transcription

1 Not to be cited without prior reference to the author ICES CM 2010/K:07 Spreading and reproduction limitations of the American comb jelly Mnemiopsis leidyi in the Baltic Sea Maiju Lehtiniemi 1*, Andreas Lehmann 2, Jamileh Javidpour 2 and Kai Myrberg 1 1 Finnish Environment Institute, Marine Research Center, P.O.Box 140, FI Helsinki, Finland *Contact author: maiju.lehtiniemi@ymparisto.fi, phone: Leibniz Institute of Marine Sciences, Duesternbrookerweg 20, Kiel, Germany Extended abstract Based on the information on salinity and temperature needed for survival and reproduction, areas within the Baltic Sea have been identified where the American comb jelly, Mnemiopsis leidyi could potentially survive and reproduce. In addition physical drift modeling has been used to investigate the potential dispersion of Mnemiopsis with the assumption that the invasion occurred via advection from the Kattegat through the Danish Straits into the western Baltic Sea. In the low saline surface layer the dispersion is mainly driven by the wind, in the lower saline layer the dispersion is controlled by the baroclinic flow field and bottom topography. Model runs showed that the natural spreading via deep water currents from the Bornholm Basin where it presently occurs, towards north and east is limited by topographic obstacles and low advection velocities. However, if Mnemiopsis would be transported in the ballast water of a ship to the northern latitudes it might survive but not reproduce in a sufficient rate to establish a new population. Thus due to combined effects of low salinity and low temperature it is not probable that Mnemiopsis could establish permanent populations in the central or northern Baltic Sea. It seems that Mnemiopsis could only reproduce at higher rate in the southern parts of the sea. If under climate change the salinity in the Baltic Sea will further decrease the establishment of Mnemiopsis would be even less probable in the north although water temperature would increase. Keywords: American comb jelly, Baltic Sea, physical factors, reproduction, survival, drifting The most important global pathway for new species introductions is ship traffic including transfers by both ballast water (and sediments) and ship fouling (Molnar et al. 2008). Shipping is very effective in species transport due to easy overcome of natural dispersal barriers e.g. too saline or cold water in the open ocean. It is important to note that over 80 % of all marine introductions have been unintentional and 31 % of the marine introductions have happened via ballast waters of ships (Molnar et al. 2008). After establishment a non-indigenous species may also spread further from the primary site of introduction via a combination of natural dispersal and human-associated transport mechanisms. Currents and related drifts are among important natural dispersal pathways, which transport particles and organisms both vertically and horizontally, and may serve as a pathway for secondary spread for alien species as well. The Baltic Sea is one of the largest brackish seas in the world. It is a semi-enclosed basin connected to the main Atlantic Ocean only via the Danish Straits. The water exchange through these straits is limited, and as a consequence of the positive freshwater balance the Baltic Sea water mass is brackish, with mean salinity of about 7 one fifth of the salinity of normal ocean waters (Fig. 1.). All euryhaline and eurythermal species are potential invaders to the Baltic Sea. Since most originate from

2 warmer areas, global warming can be expected to increase future invasions (e.g. Paavola et al. 2005). However, the ability of these species to survive and reproduce in low salinity is a key factor to determine their invasion success. Figure 1. Bottom salinity measured on R/V Aranda in June 2009 and Mnemiopsis leidyi observations. The northern and easternmost areas (blue squares; Haslob et al. 2007, Huwer et al. 2008, Janas and Zgrundo 2007) and stations (blue dots; observations done on R/V Aranda 2010) where M. leidyi has been observed and stations where it has not been observed (red dots) in the Baltic based on observations of adult individuals with lobes or genetic analyses. The stations for temperature-salinity plots are included in the map. One of the recent invaders is the American comb jelly, Mnemiopsis leidyi A. Agassiz 1865, which has caused large ecosystem perturbations in the Black Sea and the adjacent areas (Vinogradov et al. 1989). The first records of M. leidyi in northern European waters were made in 2005 in Oslofjorden, Norway (Oliveira 2007), then later in the North Sea, off the western coast of the Netherlands (Faasse and Bayha 2006), and on the Swedish west coast, in Skagerrak and in the Kiel Bight, southern Baltic Sea in autumn 2006 (Javidpour et al. 2006, Hansson 2006). In it was widely distributed in the Danish waters (Tendal et al. 2007). The species is easily identified from other ctenophores when the lobes have been developed, which are characteristic for adult specimens. However, small individuals i.e. cydippid stage larvae are difficult to identify to species without applying genetic methods (Gorokhova et al. 2009). This identification problem led to confusion to widely think that M. leidyi has spread to almost the whole Baltic Sea (e.g. Lehtiniemi et al. 2007). However, based on genetic analysis the species occurring in the central and northern Baltic Sea is proved to be an arctic comb jelly (Mertensia ovum) (Gorokhova et al. 2009). In light of the new accumulating genetic evidence it seems most probable that M. leidyi has not been found north or east of the Bornholm Basin and the Bay of Gdansk (Fig. 1). Although showing wide tolerance to physical parameters, M. leidyi is clearly close to the limit of its occurrence in such conditions where both salinity and temperature are near the lowest tolerance limits. To be able to establish permanently, M. leidyi should be able to reproduce, which

3 requires better environmental conditions compared with the conditions in which it survives. The aim of this study is to identify most probable areas where M. leidyi could disperse, survive and furthermore reproduce in the Baltic Sea with respect to circulation and hydrographic conditions. Baltic Sea Ice-Ocean Model (BSIOM) -the numerical model, used in this study, is a general threedimensional coupled sea ice-ocean model of the Baltic Sea (Lehmann and Hinrichsen 2000). The coupled sea ice-ocean model is forced by meteorological data taken from the Swedish Meteorological and Hydrological Institute (SMHI Norrköping, Sweden) meteorological database (Lars Meuller, pers. comm.) which covers the whole Baltic drainage basin on a regular grid of 1 x 1 with a temporal increment of 3 hours. The database, which for modelling purposes is further interpolated onto the model grid, includes surface pressure, precipitation, cloudiness, air temperature and water vapour mixing ratio at 2 m height and the geostrophic wind. BSIOM has been run for the period starting from an existing model run covering the period Three-dimensional fields of temperature and salinity as well as the current field have been extracted as daily averages from the model to be further used in a Lagrangian particle tracking model (Hinrichsen et al. 1997). Thus, circulation and drift track model are operated subsequently. Drifters were released in two areas where Mnemiopsis leidyi was reported to occur in May and November 2007: Bornholm Basin and Stolpe Channel (Fig. 2.). All drift experiments run until the end of the year To be able to predict the invasion and survival possibilities of M. leidyi in the central and northern Baltic Sea we searched salinity and temperature information from certain port areas, which could be either source or destination ports in the translocation of this species via ship's ballast water (Table 1). Table 1. Details of the ports chosen for the port survey. Port Country Source / destina tion Rotterdam Port Gothenburg Port Port of New Orleans The Netherlands S Description of the port Largest seaport in Europe with an annual throughput of more than 400 million tons of goods Sweden S Largest container terminal in the Nordic region Alabama, USA S Most visited US port in 2009 by the ships which transport cargo directly to Finnish (northern Baltic) harbors Primorsk Port Russia D Largest port in the Baltic by export volume Klaipeda Port Lithuania D 8 th largest port by export volume Tallinn harbour Port Kokkola of Estonia D Third largest port by traffic volume as well as by export volume in the Baltic Finland D 15 th largest port in the Baltic by transported dry bulk volume Mnemi present Yes Location North-eastern coast of the Atlantic Yes In a transition area between the North and Baltic Seas Yes In the native area of M. leidyi on the western coast of the Atlantic No No No Eastern end of the Gulf of Finland Eastern coast of the central Baltic at the mouth of the Curonian lagoon Southern coast of the Gulf of Finland Reference Faasse Bayha 2006 & Hansson et al Purcell et al. 2001, Statistics of FTA Saurama et al Saurama et al Saurama et al No Bothnian Bay Saurama et al To identify typical temperature and salinity conditions of the different sub-basins of the Baltic Sea (stations marked in Fig. 1) we used TS-diagrams (modified form Leppäranta and Myrberg 2009).

4 Experiments to determine egg production and larval survival at different salinities were conducted in the laboratory. Experiments were done at five salinity levels (5, 10, 15, 20 and 30 ) representative for the Baltic Sea gradient and at 18 C temperature. Adult Mnemiopsis leidyi (ca 2 cm) were sampled from Kiel Fjord during summer 2008 for the experiments. Figure 2. Patterns of dispersal of Mnemiopsis leidyi in the central Baltic Sea by using the Lagrangian particle-tracking model. Launching positions of drifters (black circles in squares) released in May 2007 (upper panel) and November 2007 (lower panel) in the area where M. leidyi is known to occur and end positions (red circles) in December Colors denote sub-basins of origin: green (Bornholm Basin) and yellow (Stolpe Channel). In May the drifters were launched from m and in November from m depths according to the observations (Haslob et al. 2007, Huwer et al. 2008). The drifters released in areas and water column parts where Mnemiopsis leidyi is reported to occur in May and November 2007 show that in months time the northernmost drifters end up to the northern Baltic Proper (Fig. 2). However, the majority of the drifters stay in the Bornholm Basin and in the central Baltic Sea. Small part of the drifters turns back with the cyclonic circulation in the eastern side of Gotland. No drifters released in May 2007 end up to the coastal areas, but all stay in the deeper parts of the southern and central Baltic basins. In addition to natural dispersal M. leidyi may spread in ships' ballast waters over the central Baltic Sea to the northern parts. If the ballast water is taken in when the ship leaves the harbors in the east (Rotterdam port) or west (port of New Orleans) coast of the Atlantic it is possible that the salinity difference is too large (even > 30 ) between the ballast water and the ambient water in a Baltic port. This would mean that ctenophores in the ballast water could not survive when discharged to any of the central or northern Baltic ports. The reproduction experiments conducted in different salinities show that M. leidyi produces eggs at a sufficient rate in salinities from 10 to 20 to establish permanently, although in 10 salinities the production rate is significantly lower than in 15 and 20 salinities (Tukey HSD test:

5 p=0.001 and p=0.003, respectively). In 5 or 30 no eggs were produced (Fig. 3). Larval survival was high in salinities ranging from 15 to 30, 10 being the lowest salinity were larvae survived. In 5 no larvae survived. M n e m i o p s i s e g g p r o d u c t i o n N r. e g g s d i n a d -1 y s a l i n i t y M n e m i o p s i s l a r v a e s u r v i v a l -1 % o f l a r v a e s u r v i v e d 6 d a y s a l i n i t y Figure 3. Egg production (number of eggs produced by one ctenophore per day) and larval survival (percentage of larvae survived per day) of Mnemiopsis leidyi in 18 C in different salinities from 5 to 30. Average ± SD. The hydrographic conditions (temperature and salinity) enabling M. leidyi to survive and reproduce in the Baltic Sea are marked in the Temperature-Salinity diagrams for stations in all sub-basins of the sea (Fig. 4). The required environmental conditions for survival are met on all studied stations and subbasins except in the northernmost basin, the Bothnian Bay (station F2), where all TS measurements fall outside the survival range. The salinity and temperature requirements for reproduction are much higher and therefore not met in most of the sub-basins (Fig. 4). The only areas where TS measurements lay inside the range enabling reproduction are in the western Baltic Sea: in the Kiel Bight.

6 Figure 4. Temperature-Salinity plots for stations from different sub basins of the Baltic Sea (starting from the southern and westernmost stations in Kiel Fjord in upper left corner and ending to the northernmost station F2 in lower right corner). Black dots show temperature and salinity measurements taken by CTD on board research vessels (except for Kiel Fjord ). The light blue indicates the temperature and salinity ranges where Mnemiopsis leidyi could survive and light orange indicates the ranges for reproduction.

7 Figure 5. Maps showing hypoxic: oxygen level between 0-2 ml l -1 (grey) and anoxic: oxygen <0 ml l -1 (black) areas in August Oxygen measurements are taken onboard R/V Aranda (Finnish Environment Institute) during HELCOM monitoring cruises. One important factor, in addition to salinity and temperature, influencing survival of M. leidyi is the oxygen content of the water. The strong stratification, which prevents mixing of the water column, causes deep-water anoxia and hypoxia in the central Baltic Sea (Fig. 5). This most probably affects M. leidyi survival during slow drifting from the southern Baltic Sea via deep water currents (Fig. 2).

8 We have shown that the probability for Mnemiopsis leidyi spreading from the Bornholm basin with currents to the central or northern parts of the Baltic Sea is very low due to the combination of short life cycle of these ctenophores, low drift speed near the halocline and large anoxic areas in the central Baltic. The survival of the species -if it would anyhow spread to the north- would be possible although the difficult combination of low salinity, low temperature and low food availability would lower the survival rate. We predict that the only real possibility for M. leidyi introduction would be via ballast waters of ships coming from the southern Baltic when the source population would be already adapted to a more close salinity with northern salinities. The higher requirements of temperature and salinity for reproduction make effective reproduction possible only in the western parts of the Baltic Sea. In the central and northern Baltic Sea the species could not reproduce and thus establish permanent populations. References: Faasse MA and Bayha KM (2006) The ctenophore Mnemiopsis leidyi A. Agassiz 1865 in coastal waters of the Netherlands: an unrecognized invasion? Aquatic Invasions 1 (4): Gorokhova E, Lehtiniemi M, Viitasalo-Frösen S, Haddock SHD (2009) Molecular evidence for the occurrence of ctenophore Mertensia ovum in the northern Baltic Sea and implications for the status of the Mnemiopsis leidyi invasion. Limnol Oceanogr 54(6): Hansson HG (2006) Ctenophores of the Baltic and adjacent Seas the invader Mnemiopsis is here! Aquat Invasions 1(4): Haslob H, Clemmesen C, Schaber M, Hinrichsen HH, Schmidt JO, Voss R et al. (2007) Invading Mnemiopsis leidyi as a potential threat to Baltic fish. Mar Ecol Prog Ser 349: Hinrichsen, H. H., A. Lehmann, M. A. St. John & B. Bru gge, Modelling the cod larvae drift in the Bornholm Basin in summer Continental Shelf Research 17(14): Huwer, B., Storr-Paulsen, M., Riisgård, H. U., Haslob, H. (2008) Abundance, horizontal and vertical distribution of the invasive ctenophore Mnemiopsis leidyi in the central Baltic Sea, November Aquat. Inv., 3, Janas U, Zgrundo A (2007) First record of Mnemiopsis leidyi A. Agassiz, 1865 in the Gulf of Gdańsk (southern Baltic Sea). Aquat Invasions 2(4): Javidpour J, Sommer U, Shiganova T (2006) First record of Mnemiopsis leidyi A. Agassiz 1865 in the Baltic Sea. Aquat Invasions 1(4): Lehmann, A. & H. H. Hinrichsen (2000). On the wind driven and thermohaline circulation of the Baltic Sea. Physics and Chemistry of the Earth, Part B: Hydrology, Oceans and Atmosphere 25: Lehtiniemi M, Pääkkönen JP, Flinkman J, Katajisto T, Gorokhova E, Karjalainen M, Viitasalo S, Björk H (2007) Distribution and abundance of the American comb jelly (Mnemiopsis leidyi) A rapid invasion to the northern Baltic Sea during Aquat Invasions 2(4): Leppäranta M, Myrberg K (2009) Physical Oceanography of the Baltic Sea. Springer-Verlag Berlin- Heidelberg-New York, 378 pp.

9 Molnar, JL, Gamboa, RL, Revenga, C. and Spalding, MD (2008) Assessing the global threat of invasive species to marine biodiversity. Front Ecol Environ 6(9): , doi: / Oliveira OMP (2007) The presence of the ctenophore Mnemiopsis leidyi in the Oslofjorden and considerations on the initial invasion pathways to the North and Baltic Seas. Aquatic Invasions 2 (3): Paavola, M, Olenin, S, Leppäkoski, E (2005) Are invasive species most successful in habitats of low native species richness across European brackish water seas? Estuarine, Coastal and Shelf Science 64 (2005) Purcell JE, Decker MB (2005) Effects of climate on relative predation by scyphomedusae and ctenophores on copepods in Chesapeake Bay during Limnol Oceanogr 50(1): Purcell JE, Shiganova TA, Decker MB, Houde ED (2001) The ctenophore Mnemiopsis in native and exotic habitats: U.S. estuaries versus the Black Sea basin. Hydrobiol 451: Saurama, A, Särkijärvi J, Helminen, R, Holma, E, Hytti, M, Tarkki, V and Haapakangas, E-L (2008) Baltic Port List 2007 Annual cargo statistics of ports in the Baltic Sea Region. University of Turku, Merenkulkualan koulutus- ja tutkimuskeskus, p Tendal OS, Jensen KR and Riisgård HU (2007) Invasive ctenophore Mnemiopsis leidyi widely distributed in Danish waters. Aquatic Invasions 2 (4): Vinogradov ME, Shushkina EA, Musayeva EI and Sorokin PY (1989) A new exotic species in the Black Sea: the ctenophore Mnemiopsis leidyi (Ctenophora: Lobata). Oceanology 29:

Distribution and abundance of the American comb jelly (Mnemiopsis leidyi) - a rapid invasion to the northern Baltic Sea during 2007

Distribution and abundance of the American comb jelly (Mnemiopsis leidyi) - a rapid invasion to the northern Baltic Sea during 2007 https://helda.helsinki.fi Distribution and abundance of the American comb jelly (Mnemiopsis leidyi) - a rapid invasion to the northern Baltic Sea during 2007 Lehtiniemi, Maiju 2007 Lehtiniemi, M, Pääkkönen,

More information

Abundance, horizontal and vertical distribution of the invasive ctenophore Mnemiopsis leidyi in the central Baltic Sea, November 2007

Abundance, horizontal and vertical distribution of the invasive ctenophore Mnemiopsis leidyi in the central Baltic Sea, November 2007 Aquatic Invasions (2008) Volume 3, Issue 2: 113-124 doi: 10.3391/ai.2008.3.2.1 2008 The Author(s). Journal compilation 2008 REABIC Open Access Research Article Abundance, horizontal and vertical distribution

More information

HELSINKI COMMISSION HELCOM MONAS 4/2002 Monitoring and Assessment Group Fourth Meeting Warnemünde, Germany, October 2002

HELSINKI COMMISSION HELCOM MONAS 4/2002 Monitoring and Assessment Group Fourth Meeting Warnemünde, Germany, October 2002 HELSINKI COMMISSION HELCOM MONAS 4/2002 Monitoring and Assessment Group Fourth Meeting Warnemünde, Germany, 21-25 October 2002 Agenda Item X Document code: Date: Submitted by: To be filled in by the Secretariat

More information

Baltic Sea modelling as a tool for the study of past climates. Anders Omstedt

Baltic Sea modelling as a tool for the study of past climates. Anders Omstedt Baltic Sea modelling as a tool for the study of past climates Anders Omstedt An example: The Swedish Hydrographic Expedition 1877 Fredrik Laurentz Ekman The Swedish Hydrographic Expedition 1877 compared

More information

Frequencies and pathways forcing major inflows to the Baltic Sea

Frequencies and pathways forcing major inflows to the Baltic Sea 12th Polish German Seminar The Baltic Sea at the middle of the 21st Century 13.-14.10.2014, Sopot, Poland Frequencies and pathways forcing major inflows to the Baltic Sea Andreas Lehmann, Piia Post*, Katharina

More information

American Harris mud crab Rhithropanopeus harrisii

American Harris mud crab Rhithropanopeus harrisii American Harris mud crab Rhithropanopeus harrisii (Gould, 1841) in the Gulf of Gdańsk (southern Baltic Sea): distribution, population structure and basic physiological processes Joanna Hegele-Drywa Alien

More information

POPULATION DYNAMICS AND PREDATION IMPACT OF THE INTRODUCED CTENOPHORE MNEMIOPSIS LEIDYI IN THE GULLMARS FJORD, WEST COAST OF SWEDEN

POPULATION DYNAMICS AND PREDATION IMPACT OF THE INTRODUCED CTENOPHORE MNEMIOPSIS LEIDYI IN THE GULLMARS FJORD, WEST COAST OF SWEDEN POPULATION DYNAMICS AND PREDATION IMPACT OF THE INTRODUCED CTENOPHORE MNEMIOPSIS LEIDYI IN THE GULLMARS FJORD, WEST COAST OF SWEDEN Lene Friis Møller & Peter Tiselius Dep. Of Marine Ecology Kristineberg

More information

APPENDIX B PHYSICAL BASELINE STUDY: NORTHEAST BAFFIN BAY 1

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

More information

Simulated halocline variability in the Baltic Sea and its impact on hypoxia during

Simulated halocline variability in the Baltic Sea and its impact on hypoxia during JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, VOL. 118, 6982 7000, doi:10.1002/2013jc009192, 2013 Simulated halocline variability in the Baltic Sea and its impact on hypoxia during 1961 2007 Germo V ali, 1,2

More information

Leibniz Institute for Baltic Sea Research Warnemünde

Leibniz Institute for Baltic Sea Research Warnemünde Leibniz Institute for Baltic Sea Research Warnemünde r/v Heincke Monitoring cruise Cruise- No. 06 / HK / 10 / 02 13 th 20 th May 2010 Kiel Bight to northern Gotland Sea This report is based on preliminary

More information

HELCOM Red List Category: Previous HELCOM Red List threat assessments BSEP 75 (HELCOM 1998): BSEP 113 (HELCOM 2007): Greater concern stated by:

HELCOM Red List Category: Previous HELCOM Red List threat assessments BSEP 75 (HELCOM 1998): BSEP 113 (HELCOM 2007): Greater concern stated by: English name: Code in HELCOM HUB: Baltic Sea seasonal sea ice AC Characteristic species: Phytoplankton (diatoms, autotrophic flagellates, dinoflagellates), heterotrophic bacteria, zooplankton (heterotrophic

More information

Ingestion-rate method for measurement of clearance rates of the ctenophore Mnemiopsis leidyi

Ingestion-rate method for measurement of clearance rates of the ctenophore Mnemiopsis leidyi Aquatic Invasions (2010) Volume 5, Issue 4: 357 361 doi: 10.3391/ai.2010.5.4.04 2010 The Author(s). Journal compilation 2010 REABIC Open Access Research article Ingestion-rate method for measurement of

More information

Memo of the on-line meeting of the HELCOM EN-Marine Litter (30 May 2017)

Memo of the on-line meeting of the HELCOM EN-Marine Litter (30 May 2017) Memo of the on-line meeting of the HELCOM EN-Marine Litter (3 May 217) A working meeting of the HELCOM EN-Marine Litter was held on 3 May 217 as an online meeting. The list of participants is contained

More information

Temperature, Salinity and Density Measurements in the Coastal Waters of the Rudsar, South Caspian Sea

Temperature, Salinity and Density Measurements in the Coastal Waters of the Rudsar, South Caspian Sea Journal of the Persian Gulf (Marine Science)/Vol.1/No.1/September 2010/9/27-35 Temperature, Salinity and Density Measurements in the Coastal Waters of the Rudsar, South Caspian Sea Jamshidi, Siamak 1 ;

More information

Temperature, Salinity and Density Measurements in the Coastal Waters of the Rudsar, South Caspian Sea

Temperature, Salinity and Density Measurements in the Coastal Waters of the Rudsar, South Caspian Sea Journal of the Persian Gulf (Marine Science)/Vol.1/No.1/September 2010/9/27-35 Temperature, Salinity and Density Measurements in the Coastal Waters of the Rudsar, South Caspian Sea Jamshidi, Siamak1; Abu

More information

Coastal Oceanography. Coastal Oceanography. Coastal Waters

Coastal Oceanography. Coastal Oceanography. Coastal Waters Coastal Oceanography Coastal Oceanography 95% of ocean life is in coastal waters (320 km from shore) Estuaries and wetlands are among most productive ecosystems on Earth Major shipping routes, oil and

More information

Leibniz Institute for Baltic Sea Research Warnemünde

Leibniz Institute for Baltic Sea Research Warnemünde Leibniz Institute for Baltic Sea Research Warnemünde FS Alkor Monitoring cruise Cruise- No. Al 43a 4 th February 14 th February 214 Kiel Bight to northern Gotland Sea This report is based on preliminary

More information

State of the Ocean 2003: Physical Oceanographic Conditions in the Gulf of St. Lawrence

State of the Ocean 2003: Physical Oceanographic Conditions in the Gulf of St. Lawrence Ecosystem Status Report 24/2 Oceanographic sampling gear State of the Ocean 23: Physical Oceanographic Conditions in the Gulf of St. Lawrence Background The physical oceanographic environment influences

More information

Characteristics and variability of the vertical thermohaline structure in the Gulf of Finland in summer

Characteristics and variability of the vertical thermohaline structure in the Gulf of Finland in summer Boreal Environment Research 16 (suppl. A): 73 83 2011 ISSN 1239-6095 (print) ISSN 1797-2469 (online) helsinki 31 March 2011 Characteristics and variability of the vertical thermohaline structure in the

More information

Subtidal permanently flooded with tidal water. Irregularly exposed surface exposed by tides less often than daily

Subtidal permanently flooded with tidal water. Irregularly exposed surface exposed by tides less often than daily Types of Wetlands Tidal Systems COASTAL WETLAND ECOSYSTEMS Tidal Salt Marshes Tidal Freshwater Marshes Mangrove Wetlands Tidal Estuarine Wetland 1 Definition and Formation of Estuaries u Estuary : partially

More information

Oceanographic Conditions in the Gulf of St. Lawrence during 1999

Oceanographic Conditions in the Gulf of St. Lawrence during 1999 Fisheries and Oceans Science Pêches et Océans Sciences DFO Science Laurentian Region Stock Status Report G4-01 (2000) Researh vessel CCGS Martha L. Black Oceanographic Conditions in the Gulf of St. Lawrence

More information

Types of Wetlands. Tidal Systems

Types of Wetlands. Tidal Systems Types of Wetlands Tidal Systems 1 COASTAL WETLAND ECOSYSTEMS Tidal Salt Marshes Tidal Freshwater Marshes Mangrove Wetlands 2 Tidal Estuarine Wetland 3 Definition and Formation of Estuaries Estuary: : partially

More information

SCIENTIFIC COUNCIL MEETING JUNE B. Petrie, R. G. Pettipas, W. M. Petrie and V. V. Soukhovtsev

SCIENTIFIC COUNCIL MEETING JUNE B. Petrie, R. G. Pettipas, W. M. Petrie and V. V. Soukhovtsev NOT TO BE CITED WITHOUT PRIOR REFERENCE TO THE AUTHOR(S) Northwest Atlantic Fisheries Organization Serial No. N5361 NAFO SCR Doc. 07/14 SCIENTIFIC COUNCIL MEETING JUNE 2007 Physical Oceanographic Conditions

More information

Baltic Sea Research Institute

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

More information

Ocean Boundary Currents Guiding Question: How do western boundary currents influence climate and ocean productivity?

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

More information

Highly Persisting Patch Formation Areas and Their Interannual Variability in the Gulf of Finland, the Baltic Sea.

Highly Persisting Patch Formation Areas and Their Interannual Variability in the Gulf of Finland, the Baltic Sea. Andrea Giudici and Tarmo Soomere Institute of Cybernetics - Tallinn University of Technology Highly Persisting Patch Formation Areas and Their Interannual Variability in the Gulf of Finland, the Baltic

More information

Combatting nutrient spillage in the Archipelago Sea a model system for coastal management support

Combatting nutrient spillage in the Archipelago Sea a model system for coastal management support Combatting nutrient spillage in the Archipelago Sea a model system for coastal management support H. Lauri% H. Ylinen*, J. Koponen*, H. Helminen* & P. Laihonen* ' Environmental Impact Assessment Centre

More information

Appendix 3. Jaspers et al. Appendix 3

Appendix 3. Jaspers et al. Appendix 3 Appendix 3 Figure S1 Location information of 13 monitoring stations across northern Europe (station number, locality name and decimal position), where presence/absence of the invasive comb jelly Mnemiopsis

More information

Seatrack Web Developments

Seatrack Web Developments Seatrack Web Seatrack Web Developments HELCOM RESPONSE 16/2012, 21 November 2012 Johan Mattsson, DCOO Seatrack Web Contents Short overview Recent developments Online demonstration (experimental) Questions

More information

A Synthesis of Results from the Norwegian ESSAS (N-ESSAS) Project

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

More information

Ocean Circulation. In partnership with Dr. Zafer Top

Ocean Circulation. In partnership with Dr. Zafer Top Ocean Circulation In partnership with Dr. Zafer Top Samantha Hampton Honors Science December 15, 2014 Ocean Circulation is the large scale movement of waters in the ocean basins. Dr. Zafer Top studies

More information

Please be ready for today by:

Please be ready for today by: Please be ready for today by: 1. HW out for a stamp 2. Paper and pencil/pen for notes 3. Be ready to discuss what you know about El Nino after you view the video clip What is El Nino? El Nino Basics El

More information

Activity #2 - Major Ocean Surface Currents

Activity #2 - Major Ocean Surface Currents Activity #2 - Major Ocean Surface Currents Concepts # 3 & 6 # 3 Atmospheric cells and ocean gyres redistribute heat from low to high latitudes, which influences climate, weather, and ocean temperature.

More information

Baltic Sea Research Institute Warnemünde

Baltic Sea Research Institute Warnemünde INSTITUT FÜR OSTSEEFORSCHUNG WARNEMÜNDE an der Universität Rostock BALTIC SEA RESEARCH INSTITUTE Baltic Sea Research Institute C r u i s e R e p o r t r/v "Prof. A. Penck" Cruise- No. 07PE / 07 / 07 23

More information

The Rossby Centre Ocean model applied to the Arctic Ocean using ERA-40

The Rossby Centre Ocean model applied to the Arctic Ocean using ERA-40 The Ocean model applied to the Arctic Ocean using ERA-40 H.E. Markus Meier, R. Döscher, K. Wyser /SMHI, Norrköping and K. Döös MISU, Stockholm University, Stockholm Ocean model (RCO) based on the BRYAN-COX-SEMTNER

More information

Leibniz Institute for Baltic Sea Research Warnemünde

Leibniz Institute for Baltic Sea Research Warnemünde Leibniz Institute for Baltic Sea Research Warnemünde Monitoring cruise FS Elisabeth Mann Borgese Cruise- No. EMB-0 30 th April th May 2014 Western and Central Baltic Sea This report is based on preliminary

More information

On the structure and dynamics of the water in the Słupsk Furrow*

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,

More information

Climatic Conditions Around Greenland 1995

Climatic Conditions Around Greenland 1995 NAFO Sci. Coun. Studies, 27: 39 47 Climatic Conditions Around Greenland 1995 M. Stein Institut fur Seefischerei, Palmaille 9 D-22767 Hamburg, Federal Republic of Germany Abstract The annual review of variability

More information

1. Oceans. Example 2. oxygen.

1. Oceans. Example 2. oxygen. 1. Oceans a) Basic facts: There are five oceans on earth, making up about 72% of the planet s surface and holding 97% of the hydrosphere. Oceans supply the planet with most of its oxygen, play a vital

More information

Same Risk Area Concept An area based approach to exemptions

Same Risk Area Concept An area based approach to exemptions Same Risk Area Concept An area based approach to exemptions Can ships operating solely in a specified area be exempted from the discharge criteria of the BWMC? Is the area based approach for risk assessment

More information

Winds and Currents in the Oceans

Winds and Currents in the Oceans Winds and Currents in the Oceans Atmospheric Processes Density of air is controlled by temperature, pressure, and moisture content. 1. Warm air is less dense than cold air and moist air is less dense than

More information

Towards an improved mechanistic understanding of major saltwater inflows into the Baltic Sea. Background. back to Navigation

Towards an improved mechanistic understanding of major saltwater inflows into the Baltic Sea. Background. back to Navigation Background page 1/21 major Baltic inflow = voluminous inflow of highly saline water into the Baltic Sea importance hydrographic structure and salinity balance deep water oxygenation (ecosystems!) characteristics

More information

The Arctic Crossroads

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

More information

Oceanography Quiz 2. Multiple Choice Identify the choice that best completes the statement or answers the question.

Oceanography Quiz 2. Multiple Choice Identify the choice that best completes the statement or answers the question. Oceanography Quiz 2 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. The highest and lowest tides are known as the spring tides. When do these occur? a.

More information

Cyanobacterial blooms in the Baltic Sea

Cyanobacterial blooms in the Baltic Sea Cyanobacterial blooms in the Baltic Sea Author: Martin Hansson, SMHI Key Message Cyanobacterial blooms in the Baltic Sea show large inter-annual variability both in intensity and coverage. Nutrient conditions

More information

Storm surges in the easternmost Gulf of Finland during operation of the Flood Protection Barrier of St. Petersburg

Storm surges in the easternmost Gulf of Finland during operation of the Flood Protection Barrier of St. Petersburg Storm surges in the easternmost Gulf of Finland during operation of the Flood Protection Barrier of St. Petersburg V.Ryabchenko 1, P.Andreev 2, A.Averkiev 3, A.Dvornikov 1, K.Klevanny 4, V.Tsepelev 2 1

More information

National Polish services using regional products

National Polish services using regional products Oceanographic services for the European regions - session organized by EuroGOOS European Maritime Day, Gdańsk, 20th May 2011 Polish Baltic Frédéric Chopin Philharmonic, Chamber Green Hall National Polish

More information

Wednesday, November 15, 2017

Wednesday, November 15, 2017 Wednesday, November 15, 2017 Northern Europe: Physical Geography Objective: Locate and describe the various traditional regions of Western Europe. Outline how the physical geography varies from region

More information

Supplementary Figure 1 Surface distribution and concentration of the dinoflagellate N. scintillans

Supplementary Figure 1 Surface distribution and concentration of the dinoflagellate N. scintillans Supplementary Figure 1: Surface distribution and concentration of the dinoflagellate N. scintillans (cells l-1) in the Arabian Sea during the winter monsoons of 2000-2011 (1-100 cells l-1, 8000-10,000

More information

Arctic stowaways: the potential for species introduction to occur in Svalbard associated with shipping Progress report January 2012

Arctic stowaways: the potential for species introduction to occur in Svalbard associated with shipping Progress report January 2012 Arctic stowaways: the potential for species introduction to occur in Svalbard associated with shipping Progress report January 2012 Chris Ware, Inger Greve Alsos Jørgen Berge, Jan H. Sundet og Per Arneberg

More information

Federal Research Institute Institute for Baltic Sea Fishery. Cruise Report. RV Solea Cruise Jan Hesse, Cornelius Hammer

Federal Research Institute Institute for Baltic Sea Fishery. Cruise Report. RV Solea Cruise Jan Hesse, Cornelius Hammer 1 von 17 03.12.2008 15:26 Betreff: Arbeitsbericht Hesse/Hammer Von: "Marion Nickel" Datum: Mon, 10 Nov 2008 11:29:13 +0100 An: Federal Research Institute

More information

Upper Ocean Circulation

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

More information

Homework 5: Background Ocean Water Properties & Stratification

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,

More information

Estimating the Mean Temperature and Salinity of the Chesapeake Bay Mouth

Estimating the Mean Temperature and Salinity of the Chesapeake Bay Mouth Estuaries Vol. 25, No. 1, p. 1 5 February 2002 Estimating the Mean Temperature and Salinity of the Chesapeake Bay Mouth RICARDO A. LOCARNINI,LARRY P. ATKINSON*, and ARNOLDO VALLE-LEVINSON Center for Coastal

More information

Finnish Maritime Administration BULLETIN 5/

Finnish Maritime Administration BULLETIN 5/ Finnish Maritime Administration BULLETIN 5/23.5.2008 VOLUNTARY BALLAST WATER EXCHANGE IN THE NORTH-EAST ATLANTIC AND THE BALTIC SEA Invasive non-indigenous species, contained in ships ballast water, may

More information

Annex I to Target Area Assessments

Annex I to Target Area Assessments Baltic Challenges and Chances for local and regional development generated by Climate Change Annex I to Target Area Assessments Climate Change Support Material (Climate Change Scenarios) SWEDEN September

More information

Second Session of the Pan-Arctic Regional Climate Outlook Forum (PARCOF-2), virtual forum, October 2018

Second Session of the Pan-Arctic Regional Climate Outlook Forum (PARCOF-2), virtual forum, October 2018 Second Session of the Pan-Arctic Regional Climate Outlook Forum (PARCOF-2), virtual forum, October 2018 Consensus Statement for the Arctic Winter 2018-2019 Season Outlook Climate change in the Arctic is

More information

2. Can you describe how temperature and dissolved solids changes the density of water?

2. Can you describe how temperature and dissolved solids changes the density of water? Unit 4: Oceanography LT 4.1 Density: I can explain the role density plays to help form some currents. #1 Yes I can: 1. Can you explain what density is and how you calculate it? 2. Can you describe how

More information

Page 1 of 5 Home research global climate enso effects Research Effects of El Niño on world weather Precipitation Temperature Tropical Cyclones El Niño affects the weather in large parts of the world. The

More information

The 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 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 information

General Comment on Lab Reports: v. good + corresponds to a lab report that: has structure (Intro., Method, Results, Discussion, an Abstract would be

General Comment on Lab Reports: v. good + corresponds to a lab report that: has structure (Intro., Method, Results, Discussion, an Abstract would be General Comment on Lab Reports: v. good + corresponds to a lab report that: has structure (Intro., Method, Results, Discussion, an Abstract would be a bonus) is well written (take your time to edit) shows

More information

Species specific geographical distribution patterns in a warm Barents Sea: haddock vs. cod

Species specific geographical distribution patterns in a warm Barents Sea: haddock vs. cod Species specific geographical distribution patterns in a warm Barents Sea: haddock vs. cod Nordic Climate-Fish 2nd Conference: Latitudinal changes in marine resources, exploitation and society within the

More information

REVIEW OF ALTERNATE BALLAST WATER EXCHANGE ZONES FOR VESSEL TRAFFIC TO NEWFOUNDLAND AND LABRADOR AND THE CANADIAN ARCTIC

REVIEW OF ALTERNATE BALLAST WATER EXCHANGE ZONES FOR VESSEL TRAFFIC TO NEWFOUNDLAND AND LABRADOR AND THE CANADIAN ARCTIC Canadian Science Advisory Secretariat Science Advisory Report 2010/026 REVIEW OF ALTERNATE BALLAST WATER EXCHANGE ZONES FOR VESSEL TRAFFIC TO NEWFOUNDLAND AND LABRADOR AND THE CANADIAN ARCTIC Figure 1:

More information

North Sea Ballast Water Exchange Area

North Sea Ballast Water Exchange Area HELSINKI and OSPAR COMMISSIONS HELCOM/OSPAR TG BALLAST 8-2017 Joint HELCOM/OSPAR Task Group on Ballast Water Management Convention Exemptions Eighth Meeting Helsinki, Finland, 16-17 November 2017 Document

More information

National Oceanography Centre. Research & Consultancy Report No. 36

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

More information

New perspectives of climate change impacts on marine anthropogenic radioactivity in Arctic regions

New perspectives of climate change impacts on marine anthropogenic radioactivity in Arctic regions New perspectives of climate change impacts on marine anthropogenic radioactivity in Arctic regions M. Karcher 1,3, I. Harms 2, R. Gerdes 3, W.J.F. Standring 4, M. Dowdall 4, P. Strand 4 1 O.A.Sys Ocean

More information

Surface Circulation Ocean current Surface Currents:

Surface Circulation Ocean current Surface Currents: All Write Round Robin G1. What makes up the ocean water? G2. What is the source of the salt found in ocean water? G3. How does the water temperature affect the density of ocean water? G4. How does the

More information

BALTEX A science broker for the Baltic Sea region

BALTEX A science broker for the Baltic Sea region AGU Fall Meeting San Francisco, 16 December 2010 BALTEX A science broker for the Baltic Sea region Marcus Reckermann Joakim Langner Anders Omstedt Hans von Storch What is BALTEX? BALTEX is an environmental

More information

Future climate impacts on Puget Sound oceanography: the North Pacific and hydrological context

Future climate impacts on Puget Sound oceanography: the North Pacific and hydrological context Western Washington University Western CEDAR Salish Sea Ecosystem Conference 2014 Salish Sea Ecosystem Conference (Seattle, Wash.) Apr 30th, 1:30 PM - 3:00 PM Future climate impacts on Puget Sound oceanography:

More information

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are

The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are 11.1 Ocean Basins The surface of the ocean floor is as varied as the land. The five major oceans, from largest to smallest, are w the Pacific w the Atlantic w the Indian w the Southern w the Arctic The

More information

Water Stratification under Wave Influence in the Gulf of Thailand

Water Stratification under Wave Influence in the Gulf of Thailand Water Stratification under Wave Influence in the Gulf of Thailand Pongdanai Pithayamaythakul and Pramot Sojisuporn Department of Marine Science, Faculty of Science, Chulalongkorn University, Bangkok, Thailand

More information

ALKOR 346: First IFM-GEOMAR - HYPOX expedition to the Gotland Basin underway.

ALKOR 346: First IFM-GEOMAR - HYPOX expedition to the Gotland Basin underway. ALKOR 346: First IFM-GEOMAR - HYPOX expedition to the Gotland Basin underway. From 18. Sept to 6 Oct. R/V ALKOR is working in the eastern Gotland Basin (central Baltic Sea.). The cruise led by R. Olaf

More information

HYDROCHEMICAL STRUCTURE OF BLACK SEA HYDROGEN SULFIDE. Galina Shtereva Institute of Oceanology - BAS

HYDROCHEMICAL STRUCTURE OF BLACK SEA HYDROGEN SULFIDE. Galina Shtereva Institute of Oceanology - BAS HYDROCHEMICAL STRUCTURE OF BLACK SEA HYDROGEN SULFIDE Galina Shtereva Institute of Oceanology - BAS Hydrological structure The Black Sea is one of the largest enclosed seas in the world Upper Mixed layer

More information

Carbon pathways in the South Atlantic

Carbon pathways in the South Atlantic Carbon pathways in the South Atlantic Olga T. Sato, Ph.D. Paulo Polito, Ph.D. olga.sato@usp.br - polito@usp.br Oceanographic Institute University of São Paulo Olga Sato and Paulo Polito (IOUSP) Carbon

More information

Salinity Gradients in the Mission-Aransas National Estuarine Research Reserve. Kimberly Bittler GIS and Water Resources Fall 2011

Salinity Gradients in the Mission-Aransas National Estuarine Research Reserve. Kimberly Bittler GIS and Water Resources Fall 2011 Salinity Gradients in the Mission-Aransas National Estuarine Research Reserve Kimberly Bittler GIS and Water Resources Fall 2011 INTRODUCTION Freshwater inflow has a widely recognized influence on estuary

More information

Density, Salinity & Temperature

Density, Salinity & Temperature Density, Salinity & Temperature Density and Oceans l Density = how much mass is contained in a given unit volume (density = mass/volume). l Temperature, salinity and pressure work together to determine

More information

Serial No. N4167 NAFO SCR Doc. 99/95. SCIENTIFIC COUNCIL MEETING SEPTEMBER 1999 (Joint NAFO/ICES/PICES Symposium on Pandalid Shrimp Fisheries)

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

More information

I. Definitions. A. Weather--day by day variations in temperature (temp), winds, pressure and precipitation (ppt)

I. Definitions. A. Weather--day by day variations in temperature (temp), winds, pressure and precipitation (ppt) CLIMATE UNIT I. Definitions A. Weather--day by day variations in temperature (temp), winds, pressure and precipitation (ppt) B. Climate--average seasonal weather for an area, usually described in terms

More information

I. Ocean Layers and circulation types

I. Ocean Layers and circulation types OCEAN Title CIRCULATION slide I. Ocean Layers and circulation types 1) Ocean Layers Ocean is strongly Stratified Consists of distinct LAYERS controlled by density takes huge amounts of energy to mix up

More information

Cruise Report R/V Oceania, AREX 2007

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 information

Leibniz Institute for Baltic Sea Research Warnemünde

Leibniz Institute for Baltic Sea Research Warnemünde Leibniz Institute for Baltic Sea Research Warnemünde C r u i s e R e p o r t r/v "Elisabeth Mann Borgese" Cruise-No. EMB 128 Monitoring Cruise 10 May 20 May 2016 Kiel Bight to Northern Baltic Proper This

More information

Weather & Ocean Currents

Weather & Ocean Currents Weather & Ocean Currents Earth is heated unevenly Causes: Earth is round Earth is tilted on an axis Earth s orbit is eliptical Effects: Convection = vertical circular currents caused by temperature differences

More information

Cruise Report R.V. Oceania, AREX2004

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)

More information

Cruise Report. RV Oceania, AREX2011. Institute of Oceanology Polish Academy of Sciences. the Norwegian, Greenland and Barents Seas

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

More information

2/15/2012. Earth System Science II EES 717 Spring 2012

2/15/2012. Earth System Science II EES 717 Spring 2012 Earth System Science II EES 717 Spring 2012 1. The Earth Interior Mantle Convection & Plate Tectonics 2. The Atmosphere - Climate Models, Climate Change and Feedback Processes 3. The Oceans Circulation;

More information

Climate change in the Baltic Sea Basin

Climate change in the Baltic Sea Basin Climate change in the Baltic Sea Basin Anna Rutgersson, Uppsala University, Sweden and the BACCII author team Baltic Sea Climate Change assessment ( Baltic Earth - Earth system science for the Baltic Sea

More information

The California current is the eastern boundary current that lies to the west 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,

More information

FINNISH INSTITUTE OF MARINE RESEARCH CRUISE REPORT. R/V Aranda. Cruise 2 / February - 22 April 2002

FINNISH INSTITUTE OF MARINE RESEARCH CRUISE REPORT. R/V Aranda. Cruise 2 / February - 22 April 2002 FINNISH INSTITUTE OF MARINE RESEARCH CRUISE REPORT R/V Aranda Cruise 2 / 2002 11 February - 22 April 2002 The report is based on preliminary data and is subject to changes. Finnish Institute of Marine

More information

The 2 nd war winter Arctic Skagerrak

The 2 nd war winter Arctic Skagerrak - C - Three war years cold package 147 The 2 nd war winter Arctic Skagerrak Cold center, Kristiansand, Oslo, Gothenburg Three known cities in Norway and Sweden mark roughly the sea area called Skagerrak,

More information

The North Atlantic Oscillation: Climatic Significance and Environmental Impact

The 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 information

A new fauna intercalibration typology

A new fauna intercalibration typology A new fauna intercalibration typology WFD Intercalibration - 2nd phase - Baltic GIG Auftraggeber: Landesamt für Natur und Umwelt Schleswig-Holstein Hamburger Chaussee 25 24220 Flintbe Author: Torsten Berg

More information

Coastal Ocean Circulation Experiment off Senegal (COCES)

Coastal Ocean Circulation Experiment off Senegal (COCES) DISTRIBUTION STATEMENT A. Approved for public release; distribution is unlimited. Coastal Ocean Circulation Experiment off Senegal (COCES) Pierre-Marie Poulain Istituto Nazionale di Oceanografia e di Geofisica

More information

Isopycnal Analysis of Near-surface Waters in the Norwegian-Barents Sea Region. by Tom Rossby, Vladimir Ozhigin, Victor Ivshin, and Sheldon Bacon

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

More information

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) 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 information

Temperature and salinity fluctuations in the Norwegian Sea in relation to wind

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

More information

Explain the impact of location, climate, natural resources, and population distribution on Europe. a. Compare how the location, climate, and natural

Explain the impact of location, climate, natural resources, and population distribution on Europe. a. Compare how the location, climate, and natural SS6G10 Explain the impact of location, climate, natural resources, and population distribution on Europe. a. Compare how the location, climate, and natural resources of Germany, the United Kingdom and

More information

Seasonal variations of vertical structure in the deep waters of the Southern Caspian Sea

Seasonal variations of vertical structure in the deep waters of the Southern Caspian Sea 278 Research in Marine Sciences Volume 3, Issue 1, 2018 Pages 278-286 Seasonal variations of vertical structure in the deep waters of the Southern Caspian Sea Somayeh Nahavandian 1,*, and Alireza Vasel

More information

SUPPORTING MATERIAL Tracing the origin of dioxins in Baltic air using an atmospheric modeling approach

SUPPORTING MATERIAL Tracing the origin of dioxins in Baltic air using an atmospheric modeling approach SUPPORTING MATERIAL Tracing the origin of dioxins in Baltic air using an atmospheric modeling approach Victor Shatalov 1, Jana H. Johansson 2, Karin Wiberg 3, Ian T. Cousins 2 1 Meteorological Synthesizing

More information

Adopt a Drifter Lesson Plan by Mary Cook, Middle School Science Teacher, Ahlf Jr. High School, Searcy, Arkansas

Adopt a Drifter Lesson Plan by Mary Cook, Middle School Science Teacher, Ahlf Jr. High School, Searcy, Arkansas Adopt a Drifter Lesson Plan by Mary Cook, Middle School Science Teacher, Ahlf Jr. High School, Searcy, Arkansas Do Ocean Surface Currents Influence Climate? Objectives Students will construct climographs

More information

Where is all the water?

Where is all the water? Where is all the water? The distribution of water at the Earth's surface % of total Oceans 97.25 Ice caps and glaciers 2.05 Groundwater 0.68 Lakes 0.01 Soils 0.005 Atmosphere (as vapour) 0.001 Rivers 0.0001

More information