Mulige prosjekter til masteroppgaver
Hovedinnhold
En kort presentasjon av veilederne finner du her.
Atlantic Water variability in the East Greenland Current in Fram Strait
The Arctic Ocean is rapidly changing due to the so-called Atlantification, which is associated with the poleward expansion of warm Atlantic waters and corresponding sea-ice loss. The East Greenland Current (EGC) in Fram Strait transports returning Atlantic Water to the south, partially arriving here from the Arctic Ocean and partially after recirculation within the strait. Additional temperature sensors have been added to the long-term mooring array in the western Fram Strait to better resolve and analyse the temperature stratification between the Polar Water in the upper 100 m and the Atlantic Water with its core at ~ 200 to 240 m depth. This research topic will encompass:
- Analysing the variability of Atlantic Water temperature in the EGC core and on the East Greenland shelf from thermistor data between 2020 and 2024.
- Investigating the temperature stratification throughout time, from daily to seasonal to interannual timescales.
- Investigating the variability of the stratification (rising or lowering of the Atlantic Water) in relation to atmospheric forcing and sea ice conditions.
This master project will be based at the Norwegian Polar Institute (NPI) in Tromsø and provides the opportunity to join a 3-week research cruise to the Fram Strait in (late) summer 2025, where we will recover new moored instrumentation and collect CTD data from the EGC.
Contact: Laura de Steur (NPI), Stefanie Semper (GFI)
Lavfrekvente bølger
Lavfrekvente bølger (infragravity waves, LF-bølger) kan frigis i stormsituasjoner når bølgegruppene fra stormen kommer inn på grundt vann ca 50-100 m. På dypt vann har bølgene en bølgehøyde på noen få cm, med perioder på 30-300 s, og bølgelengder fra 1000 m og oppover. Strømmen varierer med samme periode som bølgene. Slike veldig lange bølger kan penetrere inn i områder som er beskyttet fra normale lange vindgenererte bølger. De har også en evne til å skape bevegelser i flytende konstruksjoner som ellers, takket være størrelsen sin, ville vært stort sett upåvirkede av overflatebølger. De lavfrekvente bølgene har blitt dokumentert og modellert når de frigis langs kyster med strender og blir reflektert ut på åpent hav, men vi vet ikke i hvor stor grad disse dannes på norsk sokkel og om bølgene kan fortsette innover i fjordene, siden det hittil ikke har blitt gjort målinger som kan brukes til å undersøke det. Data fra tidevannsstasjoner har vanligvis en tidsoppløsning på 60 s, men på tidevannsstasjonen i Måløy logger Kartverket nå med 1 Hz, noe som gjør det mulig å analysere for LF-bølger.
Oppgaven vil bestå i å analysere tidevannsmålingene fra Måløy samt stasjoner i Nordsjøen for å kartlegge og dokumentere eventuelle forekomster av LF-bølger.
Contact: Birgitte Furevik (MET & GFI)
What drives the fate of icebergs in the Arctic?
Being able to forecast the trajectory and decay of icebergs is an important issue both for safe navigation and fixed assets in the Arctic. Iceberg movements are driven by ocean currents, tides, winds, waves and sea ice motions, but which of these factors are the most important?
The master project will consist in testing an iceberg simulation module using high-quality forecasts of winds, currents and sea ice drift and comparing the simulations against icebergs tagged by the International Ice Patrol. The technical implementation of the iceberg model into the OpenDrift package is taken care of by researchers at NERSC and MET Norway. The work will consist in testing the respective contributions of tides, waves and sea ice on the trajectory and melting of icebergs.
The work will take place at NERSC, as part of the European funded project ACCIBERG, in collaboration with MET Norway and DMI, Denmark. The project will become the first freely available iceberg forecast, triggered on demand from a mobile phone.
The work can either be a 6-months full-time project from January to June 2024 or a more flexible arrangement finishing in June 2024.
Contact: Lars H. Smedsrud or Laurent Bertino (NERSC)
Overturning in the Nordic Seas
We offer several topics for MSc projects in physical oceanography through the "Resilient northern overturning in a warming climate" group (ROVER). The overall objectives of the group are to better understand the ocean-atmosphere interaction that leads to dense-water formation in the Nordic Seas, with particular focus on the marginal ice zone along east Greenland, and its importance to the global overturning circulation. Suggested topics are
- air-sea-ice interaction in the marginal ice zone east of Greenland
- water mass transformation in the Greenland and Iceland Seas
- boundary current dynamics
The approach will be to use a combination of shipborne and autonomous measurements as well as numerical models.
Contact: Kjetil Våge
Antarctic Polar oceanography
- Shelf break exchange in the Weddell Sea
Why do warm water enter the continental shelf during summer but not in winter? The cross shelf break flow will be studied using results from laboratory experiments and/or numerical modelling supported by observations
- Hydrography near an ice shelf front
How does the hydrography near an ice shelf front change throughout the year / from year to year? The hydrography will be studied using moored instrumentation and CTD profiles
Contact: Elin Darelius
Ocean Mixing Processes
We conduct observation-based research on ocean mixing processes. Typically data sets are already collected and available for analysis. But we also try to integrate students in research cruises for collecting their own data for a Master's study.
- investigate the hydrography and mixing in fjords
- internal wave field properties inferred from moored observations near Yermak Plateau, Arctic Ocean
- eddies in the Norwegian Sea (using data collected under the PROVOLO project and NorEMSO)
- frontal processes across the Mohn Ridge inferred from shipboard and ocean lider observations (using data collected under the PROVOLO project and NorEMSO)
Contact: Ilker Fer
Structure and variability of boundary currents observed by ocean gliders
Our ocean glider facility NorGliders has been operating gliders in the Nordic Seas. Some of these missions have concentrated on sampling the boundary current of warm Atlantic Water over the slopes off Norway and off Spitsbergen. We offer Master's projects to study the structure, dynamics and variability of Atlantic Water currents at Svinøy and Gimsøy sections and in the West Spitsbergen Current
Contact: Ilker Fer
Drivers of decadal variability in the Atlantic: role of wind stress
Climate predictions in the North Atlantic are especially promising on decadal timescales. However, what the major drivers of decadal variations in the North Atlantic is still uncertain. The atmosphere forces variability in the Atlantic, but is it only the heat fluxes or can the wind stress itself change the temperature and circulation in the North Atlantic Ocean on decadal timescales?
Tasks: Analyze the Atlantic Ocean circulation in an experiment with the Norwegian earth system model (NorESM) where observed wind stress is prescribed to the ocean surface over the Atlantic, and compare the circulation with a fully coupled historical simulation with the same model.
Contact: Lea Svendsen, Helene Asbjørnsen, Marius Årthun
Current-induced wave refraction along great circles and their impact on the wave height variability
Refraction of ocean waves due to near-surface currents causes areas with focusing and de-focusing of wave energy, which pose a severe threat for navigation at sea. This project aims on further developing a recently published open-source ray tracing model in Python by solving the governing equations in spherical coordinates, as well as including other relevant functionality. The code will be applied on already existing wave buoy observations in the Agulhas current to further understand the physics behind the observed wave height variability. The student should be familiar with Python programming.
Contact: Trygve Halsne (trygveh@met.no) and Øyvind Breivik
Lagrangian analysis of large scale North Atlantic dynamics
How are advection pathways affected by natural variability and abrupt changes in ocean circulation? Multiple lines of evidence suggest that the North Atlantic ocean may exhibit abrupt circulation changes. The characteristics and drivers of these changes pose a puzzle to the prediction of future changes in the North Atlantic. This project will investigate the pathways of the signals of abrupt decadal events using Lagrangian analysis of general ocean circulation models. The aim is to investigate and create an understanding for the physical processes involved. The project is part of the Bjerknes strategic project DYNASOR which aims to clarify how currents and other features of the North Atlantic Ocean interact. Fundamental programming knowledge is necessary; however, ample supervision and support will be provided.
Contact: Andreas Born, Helene Asbjørnsen, Ina Nagler
High-frequency variability in the northwestern Iceland Sea
The northwestern Iceland Sea has not been studied much previously due to the lack of wintertime measurements. Only with the recent retreat of sea ice toward Greenland, this area has become more accessible. A mooring that was deployed in the northwestern Iceland Sea returned two-year long time series of temperature with a temporal resolution of up to 30 s. This unique data set will be used to investigate small-scale processes and high-frequency variability in the upper water column.
Contact: Stefanie Semper, Ilker Fer, and Kjetil Våge
Klimatrender i kyst og fjordstrøk
Kombinere målinger fra Hardangerfjorden og faste overvåkningsstasjoner på kysten med NorKyst800, modellarkiv med 800m oppløsning langs hele norskekysten 1995-2020, for å identifisere endringer i det fysiske miljøet og mulige konsekvenser for fjordøkosystemene.
Kontaktperson: Mari Myksvoll (mari.myksvoll@hi.no)
Spredning av lakselus langs norskekysten
Kjøre partikkelspredningsmodell for lakselus langs hele norskekysten med det eksisterende modellarkivet NorKyst800 (1995-2020) for å kartlegge innstrømningsepisoder i ulike fjordsystemer, og diskuterer hvordan det fysiske miljøet påvirker bæreevnen for akvakultur i produksjonsområdene.
Kontaktperson: Mari Myksvoll (mari.myksvoll@hi.no)
Arctic Polar Oceanography and sea ice
We offer topics on the longer term changes and variability of sea ice and oceanography in the Arctic Ocean, using a mix of climate models, process models,and observations. The existing climate model simulations, through cooperation with the Climate group using the Norwegian Earth System Model (NorESM), can be used for evaluation and analysis.
- Barents Sea Ice Cover variability the last 450 years
- Rapid Ice Loss events in NorESM simulations
Contact: Lars Henrik Smedsrud
Stormflo i Sognefjorden
Sjøkartverket har en unik måleserie av vannstand på flere posisjoner i Sognefjorden. Målingene begynte i juli 2018, og pågår fremdeles. Det betyr at disse måleseriene dekker de to store stormflo episodene vi hadde i vinter 2019-2020, og vil gi ny innsikt i hvordan vannstand i Sognefjorden varierer med forskjellige pådrag fra atmosfære, tidevann og ferskvannsavrenning. Havforskingen har også strømmålere ute som dekker de samme episodene, og disse dataene vil være tilgjengelige for en Master student. Havforskingen kan også hjelpe til med modelleringsdata. Studenten får dermed tilgang til veiledning fra to av våre institusjoner som ansetter mange oseanografer: Sjøkartverket og Havforskingsinstituttet.
Kontakt på GFI: Elin Darelius
A wave energy climatology for Norwegian waters.
The wave energy flux is the relevant quantity for estimating the potential for wave energy production. Using the 10-km resolution hindcast archive NORA10 which spans the period 1957 to present, the student will investigate the wave energy potential in Norwegian waters. The NORA10 archive was developed and is maintained by the Norwegian Meteorological Institute and is the authoritative reference data set for historical wind and wave climate in the Norwegian Sea, the North Sea and the BarentsSea.
Supervisor: Øyvind Breivik (oyvind.breivik@met.no)
Wave effects in the upper ocean.
The ocean surface boundary layer is influenced by the presence of surface waves. The waves affect the ocean through wave breaking, modification of the momentum flux from the atmosphere (wind stress) and through the Stokes drift, a second-order wave effect that causes material transport. The NEMO model has recently been set up on a regional scale and can be used to quantify the impact of the wave field on a high-resolution ocean model. Relevant questions are how the upwelling and the mixing is affected by waves in the North Sea. Good coding skills are required.
Supervisors: Øyvind Breivik (oyvind.breivik@met.no) and Lichuan Wu (SMHI)
Geophysical modelling of real oil spills in the Gulf of Mexico.
A generic, open source, ocean trajectory framework (OpenDrift - https://opendrift.github.io/) has been developed at the Norwegian Meteorological Institute. Through partners in Florida we have obtained satellite observations (shape files) describing the development of a real spill from the Taylor pipeline in the Gulf of Mexico over several days. Ocean surface drifter data from the region are also available. A master student is sought to run experiments with the Open Oil module using various parameterizations and to compare with observations for analysis. Forcing will be provided from a high resolution ocean model and atmospheric and wave models from the European Center for Medium Range Weather Forecasting (ECMWF). The project will involve collaboration with the University in Miami and other US partners. The student should be confident in Python programming.
Supervisors: Lars Robert Hole (lrh@met.no) and Øyvind Breivik (oyvind.breivik@met.no)
Storm surge modeling in Vietnam using ROMS and analytical models.
The Norwegian Meteorological Institute (MET Norway) collaborates with the National Hydro-Meteorological Service of Vietnam (NHMS) on a capacity building project sponsored by the Norwegian government. The main purpose of the project is geohazard disaster prevention. NHMS has upgraded their ocean model system to the Regional Ocean Models System (ROMS) (http://myroms.org). MET Norway uses ROMS in a nested configuration from 20km (entire Arctic Ocean) to 4km to 800m(the Norwegian coast). This model system also acts as input for the oil drift and search and rescue models. In this master project we propose to use a simple 2D setup of ROMS and compare with tidal observation in Vietnam. Vietnam currently has 17 operational tidal stations with hourly or 6 hourly observations. The data can also be compared with analytical formulas. The work will involve numerical simulations and statistical analysis. The student will collaborate with scientists at MET Norway and NHMS and can also expect to travel to Vietnam.
Supervisor: Lars R. Hole (lrh@met.no) and Øyvind Breivik (oyvind.breivik@met.no)