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.

Displaying: 101 - 120 of 418 Next
101. Hydrological monitoring

Hydrological monitoring aims produce real time information of water level and discharge, ice thickness including freeze-up and break-up in winter from a network of monitoring stations. Monitoring data is utilized in water resource planning, water management and flood damage prevention. Monitoring is coordinated by Finnish Environmental Institute (SYKE).

Climate Climate change Ice River ice Arctic Temporal trends
102. Continous monitoring of gammanuclides, strontium (beta) and tritium in deposition in Finnish Lapland

Part of the continuous nationwide monitoring of radionuclides in Finland. The dose rate monitoring network in Finnish Lapland comprise 32 automatic measurement stations (Finnish nation-wide monitoring network consists of about 257 stations equipped with GM tubes). Three of the stations are equipped with LaBr3-detectors measuring a gammaspectrum with 10 minute intervals. The network is intended for civilian defence and surveillance purposes, not for research. It is a good early warning system in radiation fallout situation. Every monitoring station have individual alarm level: 7 days average dose rate + 0.1 microSv/h. The dense network indicate also the extent of the radioactive contamination.

tritium strontium Radioactivity caesium Radionuclides fallout nuclides Atmosphere iodine deposition
103. Monitoring of the effects of air pollution and climatic change on lakes

Monitoring of the water quality reflecting long-range transboundary air pollution including acidifying compounds, metals and POPs, and climatic change. Part of the sites are also including in biological monitoring. Monitoring sites are the most upland lakes and they are not under any significant human impact. Information is distributed to the UN Convention on Long-range Transboundary Air Pollution. Monitoring is managed by Finnish Environmental Institute (SYKE).

Biology air pollution Heavy metals Climate Acidification climate change Ecosystems POPs
104. Hydrogeological monitoring

Monitoring follows groundwater level and quality as well as changes in soil humidity and frost depth in winter.

Soils Climate Climate change frost Arctic Groundwater humidity.
105. Monitoring of airborne radioactive substances in Lapland

Part of the continuous nationwide monitoring of radionuclides in Finland. STUK is responsible for monitoring of radioactivities in atmosphere. STUK operates a network of eight aerosol samplers from which three are located in Finnish, Lapland at Rovaniemi, Sodankylä and Ivalo. The sampling is done either weekly or bi-weekly. Gammaspectroscopic measurements are done in the laboratory in Rovaniemi. The lowest activities are detected at microBq/m3 level.

sodium. beryllium Radioactivity caesium airborne radionuclide monitoring Radionuclides Atmosphere iodine
106. Monitoring of pollutants in fish and sediment

Monitoring aims to follow certain pollutant concentrations and their changes in fish tissue and sediment. Both inland lakes, one river and coastal areas are sampled. Lapland monitoring site is Lake Inarijärvi. Project is managed by Finnish Environment Institute (SYKE).

Biological effects Biology tissue pollutant Heavy metals Fish sediment. monitoring Persistent organic pollutants (POPs) Sediments Ecosystems
107. Oulanka, EMEP station, Northern Finland

Monitoring of air quality and deposition.

Atmospheric processes Ozone Heavy metals Long-range transport Acidification Contaminant transport Atmosphere Temporal trends
108. National deposition monitoring, Northern Finland

Monitoring of direct deposition. Project is run by Finnish Meteorological Institute (FMI).

Atmospheric processes Heavy metals Long-range transport Acidification Arctic Atmosphere Temporal trends
109. Pallas, AMAP station, Northern Finland

The overall objectives for operation of the station will follow those defined in the AMAP programme. The main interests are the levels and trends of airborne toxic pollutants (POPs and heavy metals) in northern Fennoscandia.

Atmospheric processes Organochlorines PCBs Arctic haze Heavy metals PAHs Long-range transport Acidification Contaminant transport Arctic Persistent organic pollutants (POPs) Pesticides Atmosphere Temporal trends
110. MISA. Miljøgifter i svangerskap og ammeperioden

Follow-up of mother-child cohort 515 childer and delivering women. Started 2006, will be followed due to AMAP protocol for 12 years

PCBs Heavy metals Persistent organic pollutants (POPs) HHAG Human health
111. Monitoring of the glaciers surrounding Malmbjerg

to monitor the mass balance and glacier flow of Arcturus Glacier and of Schuchert Glacier adjacent to Malmbjerg (Stauning Alps, E Greenland) Network type: commercial consultancy including in-situ monitoring, ablation stakes, ground penetrating radar, modelling

112. Overview of the State of the Arctic Hydrometeorological Observation Networks

In the context of the tasks SAON SG steering group, the topology of the Arctic hydrometeorological observation network can be presented in the following concise form: 1. Agrometeorological; 2. Actinometric; 3. Aerological (radiosounding); 4. Water balance; 5. Hydrological on rivers; 6. Hydrometeorological on lakes; 7. Glaciological; 8. Meteorological; 9. Marine hydrometeorological (in the coastal zone, river estuaries, open areas including marine vessel and expeditionary); 10. Avalanche; 11. Ozone measuring; 12. Heat balance; 13. Atmospheric electricity; 14. Water, soil and snow surface evaporation; 15. Chemical composition of water and air. Observation network data are operationally transferred to Roshydromet’s data telecommunication network except for those indicated in items 4, 7,12-15. The main networks in terms of the number of observation points and volume of information obtained are meteorological, marine hydrometeorological, river hydrological, aerological and actinometric ones. Meteorological observations are considered as the main type of observations. To establish a common database and control timely and complete collection and distribution of information, a catalog of meteorological bulletins is being created to be the plan of hydrometeorological information transfer from the sources to Roshydromet’s data telecommunication network to distribute among information recipients The catalog of meteorological observations is maintained by State Institution “Hydrometeorological Center” and State Institution “Main Radio-Meterological Center”. Electronic version of the catalogs of meteorological bulletins is maintained by State Institution “Main Radio-Meterological Center” and located on the Internet site The catalog of meteorological bulletins contains the following information: − Name of Roshydromet’s subordinate Federal State Institution and observation point to input data into the automated data system; − shortened title of the hydrometeorological bulletin in proper format; − observation data coded form; − hours of observation; − data transfer check time; − number of observation points taking part in one bulletin; − lists of five-digit indices for observation points. Changes are entered into the catalogs of meteorological bulletins quarterly. WMO’s WWW is considered as the main foreign information consumer. The lists of WMO correspondent stations are given in WMO publications # 9, vol. C, part 1 (Catalog of Meteorological Observations), vol. A (Observation Stations). 2. SAON is expected to stimulate the process of improving configuration and completeness of the circumpolar region monitoring system as a potential tool for international consolidation of the opportunities available in the functioning of observation networks in order to improve national standards quality and ensure more complete compliance of the Arctic research strategies proposed to socioeconomic needs and interests of Arctic countries 3. The catalog of points and main observations is given in Table 1 (see Fig. 1). The maximum development of the Russian hydrometeorological observations in the Arctic was reached in early 1980s, when information was received from 110 stations. In subsequent years, the number of stations decreased more than twice (Fig. 2). The current level of observations is determined by the functioning of a network consisting of 49 points two of which are automatic weather stations. Three points are temporarily removed from operation. In short term, 8 automatic stations are expected to be opened; while in medium and long term, the number of manned observation points will increase up to 52-54, and the number of automatic ones – up to 20-25. For the manned network, the meteorological program includes a set of eight-hour observations of: atmosphere pressure, wind parameters, air and soil temperature, relative humidity, weather phenomena, cloud height, visual range, precipitation, while for automatic weather stations – a set of reduced 4-hour observations. The marine hydrometeorological program includes coastal observation of temperature, water salinity (density), sea-level variations, heave, ice distribution (and thickness) as well as meteorological parameters under the change of observation conditions from hourly to ten-day observations. The river hydrological program is quite similar to the marine one. It does not include observations of water density, however, they can be included for the stations having a special status, measurement of water discharge, alluvia and chemical composition of water. The programs will include hourly and ten-day observations. The aerological program will include 1-2 –hour measurements of: atmosphere pressure and wind parameters on selected isobaric surfaces. Actinometric observations include measurement of 5 components of atmosphere radiation balance in case of the full program and measurement of total radiation under a reduced program. Network type: The main networks in terms of the number of observation points and volume of information obtained are meteorological, marine hydrometeorological, river hydrological, aerological and actinometric ones.

Oceanography Atmosphere Ecosystems
113. National Institute of Geophysics and Volcanology (INGV)

INGV operates in the Arctic region with observational activities in Svalbard, near the area of Ny-Ålesund, where the Institute has installed three stations to monitor ionospheric scintillation, currently in operation. In Svalbard, the PEGASO (Polar Explorer for Geomagnetic And other Scientific Observations) project has performed several stratospheric balloon launches (Pathfinders) with the aim of studying the Earth's magnetic field in an area with poor coverage measurements and of studying the possible trajectories of circumpolar winds at high altitudes. At the Greenland Base of Thule, INGV in collaboration with CNR, DMI (Danish Meteorological Institute), University of Rome La Sapienza and ENEA, carries out spectrometric observations for the analysis of stratospheric chemistry and mesosphere to monitor the ozone layer. In cooperation with In addition, an upper atmosphere permanent observatory for magnetosphere and Ionosphere sounding, including Auroras, and other geophysical processes is operated in Greenland, Zackemberg station in cooperation with Danish scientists. INGV is currently involved in the coordination of two European initiatives: a) EMSO (European Multidisciplinary seafloor Observatory) a European research infrastructure of ESFRI (European Strategy Forum on Research Infrastructures), which counts to establish a multi-parametric permanent network in the surrounding European seas, including the Arctic area. The project began in April 2008 with the participation of 11 European countries; b) EUROANDRILL, created under the aegis of the European Science Foundation, aims to drill key areas of polar areas to study past and future climate. The project involves the involvement of 10 European and 3 extra-European countries. The Institute is also active in other projects in the Arctic, in particular actively participates in the seismic network GLISN, developed from the existing stations in and around Greenland.

Geology Oceanography Atmosphere
114. Institute of Oceanography and Marine Geophysics (OGS)

OGS conducts scientific activities within the fields of Earth Sciences and Polar Science in the Arctic, primarily but not exclusively, in the sea with the vessel OGS-Explora. Current OGS activities in the Arctic include a) Pergamon, EU COST Action: European network for study and long-term monitoring of permafrost, gas hydrates and release of methane in the Arctic and climate change impacts; b) IBCAO (International Bathymetric Chart of the Arctic Ocean) to develop a digital bathymetric database to the north of 64°. OGS is the Editorial Board and provides multibeam data; c) Research activities in the frame of PNRA (Italian Antarctic and Arctic National Research Programme) through several projects devoted to paleoceanographic study of the thermohaline circulation on the Eirik Drift (Greenland and study of paleoclimate in the Barents Sea using geological and geophysical data from the International Polar Year EGLACOM cruise of OGS Explora. CORIBAR international project (IT, DE, ES, N, DK) will provided in the next 1-2 years new data for the last item, through MEBO drilling on board RV Maria S. Merian.

Oceanography Ecosystems
115. Italian National Agency for New Technologies, Energy and Sustainable Economic Development (ENEA) (ENEA)

Within the Unit for Environment and Energy Modeling (UTMEA), the Laboratory Earth Observations and Analyses within UTMEA (UTMEA-TER) carries out long-term observations of stratospheric chemistry and mesosphere in Greenland, Thule station. Stratospheric processes (evolution in atmospheric temperature, ozone depletion) and chemistry are monitored and investigated by stratospheric lidar as well as spectrometers, in strong cooperation with INGV and DMI. Since 1990 numerous measurement campaigns have been carried out, also on the international level (EASOE, SESAME, THESEO, ESMOS/Arctic. ENEA’s Diagnostics and Metrology Laboratory (UTAPRAD-DIM) has been participating in polar campaigns since the late 1990's. In particular, it has developed the laser spectrofluorimeter CASPER (patented) and prototypes of different lidar fluorosensor: for ships, underwater remotely operated vehicles and patented miniature Unmanned Aerial Vehicles. These instruments participated in 3 oceanographic cruises (2006, 2007 and 2008) at Svalbard, on board of the "Oceania" in the context of a collaboration with the Institute of Oceanology of the Polish Academy of Sciences. Their use is also envisaged under the Italian-Canadian CLIMAT (complementary use of lidar to improve bio-optical models derived from satellite system in the St. Lawrence).

Oceanography Atmosphere
116. JAMSTEC: measurement network in collaboration with Russian, Mongolian and US Institutes

Long-term Obs. Site.   Super-sites、experiment-sites Traverse Obs. Line

Climate Atmosphere
117. National Research Council (CNR) (CNR)

Italy’s leading national research institution, the CNR has been supporting research activity at Ny-Ålesund since 1997, when the scientific station “Dirigibile Italia” was acquired. This infrastructure supports Arctic research conducted by the national research community. In 2008, it was improved through the construction of the Amundsen-Nobile Climate Change Tower and the actikvity largely enlarged with the Climate Change Tower Integrated Project (CCT-IP - Scientific cooperation, particularly focused on atmospheric science including pollutants distribution and ozone studies, on oceanography and on marine biology and biodiversity was developed by CNR scientists in particular with NPI and AWI; CNR is coordinating actions (EU-GMOS project) to improve and implement the observational system related to mercury. CNR is also involved in the SIOS preparatory phase project, and in Italy it is engaged to coordinate interested Italian expertises in a common scientific plan and actively promote Italian participation to SIOS final multidisciplinary platform. In the years to come, CNR intends to promote the improvement of research activity and to reinforce international cooperation of the Italian research groups, and to provide a significant contribution to the observational system in the Arctic, following the lines recommended by SAON. Together with the improvement/development of a supersite at Ny-Ålesund and large contribution to SIOS, CNR will operate to contribute/sustain thematic networks (Polar-AOD for aerosol and GMOS for mercury leading from CNR).

Pollution sources Environmental management Oceanography Atmosphere Ecosystems
118. GRENE (Green Network of Excellence) (GRENE)

1. Priority Research Theme (1) Clarification of the mechanism of the Arctic amplification. (2) The role of Arctic in the global climate change and future projection. (3) Evaluation on the influence of the Arctic Environmental Change to the weather in the Japan area and fishery. (4) Future projection of the sea ice distribution in relation to the evaluation Arctic route. 2. Basic infrastructure (1) Arctic research cruises by Japanese and foreign ships/ice breaker. (2) Cloud radar system. (3) Data archive system. 3. Establishment of “Japan Consortium for Arctic Environment Research” 4. Budget size: 650, 000, 000 Japanese Yen per year. (appox. 8 million USD per year) Network type: research programme

Hydrography Climate Sea ice Oceanography Atmosphere
119. Hydrometric Observations

To provide for the collection, interpretation, and dissemination of surface water quantity data and information and services that are vital to meet a wide range of water management, engineering and environmental needs across Canada. Main gaps: The current hydrometric network is deficient in terms of understanding the regional hydrology and river regimes across Canada. The map below integrates Environment Canada’s two key frameworks: the National Drainage Area Framework with the National Terrestrial Ecological Framework to identify network deficiencies. In order to have sufficient information there needs to be at least one active hydrometric station measuring natural flow in each corresponding ecodistrict within a sub-sub drainage area. This strategy ensures that there will be sufficient information to understand the hydrological processes and the interrelationships with the landscape. This information is essential for research and enhancing our predictive capabilities and data transfer. As the map shows, areas of sufficiency are concentrated in the southern, more populated regions of the country. Network sufficiency declines to the north and northeast, with great extents of northern Canada having no coverage at all. Network type: in-situ.water level and streamflow monitoring stations

Oceanography Atmosphere Human health Ecosystems
120. Permafrost observational networks in Russia

Lack of consistent spatially representative and sufficiently long time series characterizing the state of permafrost and its dynamics under changing climatic conditions necessitates improvement and further development of observational networks. The purpose of this section is to provide an insight into the permafrost networks available in the Russian part of the Artic. Data characterizing the state and dynamics of Russian permafrost in the past several decades come from three independent sources. The first source of data is soil temperature observations up to 3.2 m. depth conducted at selected meteorological stations. These conventional measurements are not specifically targeted at studying permafrost parameters. Two other networks, authorized under the Global Climate Observing System (GCOS) and its associated organizations, have been developed for monitoring permafrost temperature and seasonal thaw depth. Temperature observations in the boreholes are conducted under the framework of the Thermal State of Permafrost (TSP) project. Another source is the data from the Circumpolar Active Layer Monitoring (CALM) project. Here we give brief description of these networks and results obtained so far for Russian permafrost regions. Main gaps: Although soil temperatures are measured at many of the Russian stations, observations in permafrost regions are sparse and do not capture the whole range of permafrost variability due to difference in climatic and biophysiographical conditions. • Evaluation of the soil temperature regime and dynamics through correlations with air temperatures is not an option, since only a small part of total variability is explained. • Other networks and measurements are needed to evaluate the dynamics of permafrost.