The full list of projects contains the entire database hosted on this portal, across the available directories. The projects and activities (across all directories/catalogs) are also available by country of origin, by geographical region, or by directory.
The main objective is resource monitoring of commercially important populations and non commercial species, West Greenland (several fish species and shrimps). Network type: ship survey
The main objective is resource monitoring of commercially important populations and non commercial species, East Greenland (several fish species and shrimps). Network type: ship survey
The main objective is resource monitoring (primarily Greenland Halibut). Surveys and sampling from the commercial fishery
The main objective is resource monitoring (primarily Greenland Halibut). Network type: Surveys and sampling from the commercial fishery
The main objective is to provide management advice for harvested species (large whales, narwhale and beluga, walrus). The surveys are conducted from fixed winged twin engine aircrafts with 2-4 observers, that systematically survey for marine mammals in the prime habitats in Greenland. Surveys are conducted as strip census, line transect, photographic survey or independent observer surveys. Target species and areas shift between years but it is attempted to maintain a 5-6 survey cycle in the areas with the largest hunting pressure (i.e. West Greenland). For East Greenland a survey cycle of 10 or more years will be maintained.
To acquire atmospheric data in support of both the prediction and detection of severe weather and of climate trend and variability research. This serves a broad range of users including researchers, policy makers, and service providers. Main gaps: Long-term, atmospheric monitoring in the North poses a significant challenge both operationally (e.g. in-situ automated snowfall measurements) and financially (charterd flights for maintenance and calibration).Most monitoring in the North is limited to populated areas. Attempts to develop an AMDAR capacity out of First Air and Canadian North fleets failed due to economical and technical difficulties. As demonstrated through impact studies, benefits of AMDAR in the North would be tremendous, however would require acquisition and deployment of specialized sensing packages such as TAMDAR (which includes measurements of relative humidity), development of datalink capacity through satellite communications (e.g. Iridium), and upgrading some aircraft systems when possible, especially the aircraft navigation systems. Network type: Atmospheric observing stations over land and sea composed of: - Surface Weather and Climate Network: o In-situ land stations comprising both Hourly stations and Daily Climate observations - Marine Networks: o Buoys (moored and drifting) o Ships: Automatic Volunteer Observing System - Upper Air Network: o In situ (radiosonde) o In situ Commercial Aircraft (AMDAR)
Is updated every day during the season, 2002-2007
Temperature, Salinity, pH, Oxygen, Hydrogensulphide, Phosphate, Total-Phosphorous, Nitrite, Nitrate, Ammonium, Total-Nitrogen, Alkalinity, Silicon, PON, POC, and Chlorophyll-a Zooplankton, Phytoplankton, Bacterial plankton, Zoobentos, Phytobentos, Seal, Sea Eagle, Amphipod, Sedimentation, Primary production, Klorophyll
The Swedish Meteorological and Hydrological Institute (SMHI) maps ice extent and type for shipping and weather prognoses (Table 6, #4.1). The ice extent at sea is of great importance for navigation, and assistance from an icebreaker is often needed, especially for harbors in the Bothnian Bay. Hence, ice conditions are mapped daily during the winter period, normally from the end of November until the end of May. Ice meteorologists take advantage of detailed reports about ice type and ice thickness from observers along the coast, e.g. pilots, special ice observers, and from the icebreakers passing through the ice-covered sea. Observations from helicopters are part of the regular icebreaking activities. Satellite images, especially from US weather satellites (NOAA-15, NOAA16 and NOAA-17), complement the ice reports and provide information on the large-scale ice situation on the scale 1 km x 1 km during clear sky conditions. More detailed ice information, down to the scale 20 m x 20 m, can be retrieved from a satellite-based instrument called Synthetic Aperture Radar (SAR). SAR sensors are also found onboard the Canadian RADARSAT (in operation since 1996) and on the European ENVISAT (since 2003) and provide information on the ice situation regardless of weather conditions and time of day. A good description of the ice situation is also needed as input data for weather prognosis models because the extent of sea ice has a major influence on weather (especially in coastal areas), and on temperature, cloudiness, and precipitation. Results from daily ice mapping are saved in a database from which e.g. climate statistics for the Baltic region may be generated.
The Seal and Sea Eagle subprogram (Table 4, #8.2.6) monitors marine top consumers as indicator species to assess harmful effects of environmental toxics. Hopefully, in the long run, the program will show that these species have natural reproduction, health, and population. At present the subprogram has no sampling network. In the Bothnian Bay, the Swedish Museum of Natural History (NRM) monitors grey seals, ringed seals, and European sea eagles. These observations will show the state and trends of population size, development, and health of seals and of reproduction, population size, and development of European sea eagles. The aim of early warning is to detect changes in reproduction, health, survival, and population trends that may result from changes in the marine environment.
The Integrated Coastal Fish Monitoring subprogram (Table 4, #8.2.5) documents the composition of the stationary fish community as well as the growth, general health situation, and reproduction success of perch (Perca fluviatilis) and burbot (Lota lota) as indicators of environmental toxics. Fish from one site close to Umeå is sent to Gothenburg University for analysis of biochemical, physiological, histological and pathogenic variables in perch.
The Free Water Body subprogram (Table 4, #8.2.4) aims to describe the effects of primarily overfertilization by means of hydrographical, chemical, and biological methods. One part of the program collects samples as frequently as 18 to 25 times per year at a few sea and coastal stations. Another part collects samples only once per year, during winter, to map the extent of areas with low oxygen content and the size of the nutrient pool, which gives the prerequisites for algal bloom in spring.
Metals and Organic Environmental Pollutants subprogram (Table 4, #8.2.3) will report mainly on environmental toxics in biota in the large sea basins, of which the Bothnian Bay and the Gulf of Bothnia are the farthest north. Sea mussels, fish, and bird eggs are collected and analyzed for the content of metals and organic toxics. The material is then stored at the Swedish Museum of Natural History (NRM) for possible later retrospective analyses.
The subprogram, Macro Fauna Soft Bottoms, contains trend and aerial monitoring of soft-bottom fauna in the Gulf of Bothnia. It is conducted by Umeå Marin Research Center (UmU-M) and includes basic sediment investigation and assessment of oxygen concentration in bottom waters. The aim is to observe if, and in what way, the structure of the bottom macro fauna changes. Changes may indicate over-fertilization and oxygen stagnation. Embryogenes of Amphipod (Monoporeia affinis and Pontoporeia femorata) and its environment is studied at 7 sites in Baltic Proper and 5 sites in Gulf of Bothnia as an indicator species of bottom sediment quality.
The IPY-project ‘COPOL’ has a main objective of understanding the dynamic range of man-made contaminants in marine ecosystems of polar regions, in order to better predict how possible future climate change will be reflected in levels and effects at higher trophic levels. This aim will be addressed by 4 integrated work packages covering the scopes of 1) food web contaminant exposure and flux, 2) transfer to higher trophic levels and potential effects, 3) chemical analyses and screening, 4) synthesis and integration. To study the relations between climate and environmental contaminants within a project period of four years, a “location-substitutes-time”-approach will be employed. The sampling is focussed towards specific areas in the Arctic, representing different climatic conditions. Two areas that are influenced differently by different water masses are chosen; the Kongsfjord on the West-coast of Spitzbergen (79N, 12 E) and the Rijpfjord North-East of Svalbard (80N, 22 E). The main effort is concentrated in the Kongsfjord. This fjord has been identified as particularly suitable as a study site of contaminants processes, due to the remoteness of sources, and for influences of climatic changes, due to the documented relation between Atlantic water influx and the climatic index North Atlantic Oscillation (NAO). The water masses of the Rijpfjord have Arctic origin and serves as a strictly Arctic reference. Variable Atlantic water influx will not only influence abiotic contaminant exposure, but also food web structure, food quality and energy pathways, as different water masses carry different phyto- and zooplankton assemblages. This may affect the flux of contaminants through the food web to high trophic level predators such as seabirds and seals, due to altered food quality and energy pathways.
The ZERO database contains all validated data from the Zackenberg Ecological Research Operations Basic Programmes (ClimateBasis, GeoBasis, BioBasis and MarinBasis). The purpose of the project is to run and update the database with new validated data after each succesfull field season. Data will be available for the public through the Zackenberg homepage linking to the NERI database. The yearly update is dependent on that each Basis programme delivers validated data in the proscribed format.
The aim of the project is to describe and model mercury accumulation up the Arctic food chain. Based on existing knowledge from old projects and new measurements made on frozen tissue samples. This project will contribute to a better understanding of the fate of mercury in the Arctic.
The aims of the project are: - to evaluate the fluxes of radionuclides in the water column and their accumulation in the sediment, on a short-time scale; - to determine the C/N and delta13C-delta15N ratios in suspended and sedimentary matter, and test their use as tracers of origin, composition and transformation pathways of organic particles. The selected study area is the Kongsfjord-Krossfjord system, Svalbard, considered as representative test-site for studying processes occurring in Arctic fjords. The focus of the project will be on the processes occurring at the glacier-sea interface, where enhanced lithogenic and biogenic particle fluxes are reported in summer. Specific methods will be used to trace the particle sources. The rate of accumulation-resuspension processes will also be investigated from the inner fjord to the outer continental shelf.
The general objective of this research concerns the quantitative and qualitative study of particulate matter retained in natural (sea-ice and sediment) and artificial (sediment traps) traps in order to determine the main origin (autochtonous and allochtonous) and the relative importance of different fractions of particulate matter and to follow their fate in the environment. To quantify the autochtonous origin of particulate matter, primary production, nutrient uptake, biomass distribution, phytoplankton community structure and fluxes in the first levels of the trophic chain will be investigated. Studies will be conducted in the sea-ice environment and in the water column and compared to the particle fluxes measured both in the water, using sediment traps and in the sediment, by radiometric chronology, in order to estimate the different contribution of these habitats to carbon export to the bottom. The zooplankton will be identified and counted and primary production, nutrient uptake and phytoplankton dynamics will be related to hydrological structure and nutrient availability in the environment. The Kongsfjord results particularly suitable for the main objective of this research as it is influenced by important inputs of both atmospheric (eolic and meteroric) and glacial origin and is characterised by a complex hydrological situation which may promote autochtonous productive processes, thus determining important particulate fluxes.