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: 21 - 40 of 108 Next
21. Hydrometeorological monitoring

Hydrometeorological monitoring program produces real time information on precipitation and snow water equivalent. Information is utilized in modeling and forecasting floods and snow load. As part of the program, information of evaporation is produced with WMO standards. The program is coordinated by Finnish Environment Institute (SYKE). Finnish meteorological institute and Lapland regional centre for economic development, transport and the environment manage measurements and field work.

Climate Hydrometeorology Climate change snow water equivalent Arctic monitoring evaporation. precipitation
22. 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
23. 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

24. 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
25. 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
26. JAMSTEC: measurement network in collaboration with Russian, Mongolian and US Institutes

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

Climate Atmosphere
27. 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
28. 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.

29. Ice-drifting buoy observation in sea ice area of the Arctic Ocean

Ice-drifting buoy observation in sea ice area of the Arctic Ocean Main gaps: not well documented…

Hydrography Climate Sea ice Oceanography Atmosphere
30. Observation of Greenhouse Gases using Aircraft and Tower Network in Siberia

Cooperation with: ・Institute of Atmospheric Optics, Tomsk, Russia ・Permafrost Institute, Yakutsk, Russia ・Central Aerological Observatory, Moscow, Russia ・Institute of Microbiology, Moscow, Russia

Climate Pollution sources Atmosphere
31. Dynamic Response of Arctic Tidewater Glaciers to Climate Change (GLACIODYN-T)

University of Silesia in close cooperation with the Institute of Geophysics, Polosh Academy of Sciences (PAS) has developed and maintain monitoring of glaciers in SW Spitsbergen, Svalbard. Monitoring network of land ice masses in Southern Spitsbergen is aimed to study the response of tidewater glaciers to climate warming, with focus on mass loss due to calving. Seasonal and interannual changes in glacier flow velocity, fluctuation of terminus position and calving rate are studied for better understanding of ice berg calving. The target glacier Hansbreen has a comprehensive ground observing system (Figure 21). It consists of mass balance stakes, automatic weather stations (AWS), time lapse GPS survey of velocity at stake T4, two time lapse cameras, automatic laser ranger and panoramic radar for measurements of ice cliff fluctuations. Moreover, mass balance, including snow cover studies are conducted every year since 1989. In some years high frequency ground penetrating radar is used for snow thickness measurements along the same profiles on the glacier. Satellite remote sensing is used for extraction of data on glacier flow velocity and fluctuation of termini and calculation of mass loss by calving. Up-to-dated inventory of glaciers in Southern Spitsbergen has been done by remote sensing methods (Figure 23). Studies are conducted in cooperation with Spanish, Norwegian and Italian partners. Cooperation with Institute of Oceanology, PAS (since 2010) is developed to monitor sea water parameters for studies of sea water - ice cliff interaction. Main gaps: Gaps in series of observations due to failures of equipment, lack of power supply or damage by polar bears. Long term tide and wave record required. More tidewater glaciers advisable with monitoring of flow velocity by GPS as ground truth data for calibration of remote sensing survey.

32. Hans Glacier Monitoring (HGM) (HGM)

Main objectives of Hans Monitoring Network are collecting long-term record of mass-balance measurements and surface glacier velocities. Additionally we collect meteorological parameter at 3 AWSs located in ablation and accumulation area and ELA.

33. Sodankylä-Pallas super site of the Finnish Meteorological Institute (FMI) (Sodankylä-Pallas)

Atmosphere monitoring, cryosphere monitoring, atmosphere-biosphere interaction. In situ monitoring with automatic and manual systems (e.g. synoptic meteorological observations since 1908), measurements with ground-based reference systems of space-borne remote sensing instruments Network type: In situ monitoring with automatic and manual systems (e.g. synoptic meteorological observations since 1908), measurements with ground-based reference systems of space-borne remote sensing instruments

Geology Atmosphere Ecosystems
34. ArcticNet Network of Excellence Observing Program

ArcticNet brings together scientists and managers in the natural, human health and social sciences with their partners in Inuit organizations, northern communities, government and industry to help Canadians face the impacts and opportunities of climate change and globalization in the Arctic. Over 110 ArcticNet researchers and 400 graduate students, postdoctoral fellows, research associates and technicians from 28 Canadian universities and 8 federal departments collaborate on 28 research projects with over 150 partner organizations from 15 countries. The major objectives of the Network are: • Build synergy among existing Centres of Excellence in the natural, human health and social Arctic sciences. • Involve northerners, government and industry in the steering of the Network and scientific process through bilateral exchange of knowledge, training and technology. • Increase and update the observational basis needed to address the ecosystem-level questions raised by climate change and globalization in the Arctic. • Provide academic researchers and their national and international collaborators with stable access to the coastal Canadian Arctic. • Consolidate national and international collaborations in the study of the Canadian Arctic. • Contribute to the training of the next generation of experts, from north and south, needed to study, model and ensure the stewardship of the changing Canadian Arctic. • Translate our growing understanding of the changing Arctic into regional impact assessments, national policies and adaptation strategies. Main gaps: [Not specified] Network type: Thematical observations:Yes Field stations: Yes on Land (see CEN sheet) and Marine (CCGS Amundsen) Community based observations: Yes Coordination: Yes

Oceanography Atmosphere Human health Ecosystems
35. Danish Meteorological Institute (DMI)

DMI operates general weather observation for meteorological and climatological services. DMI operates geomagnetic observatories in Greenland DMI monitores stratospheric ozone and UV radiation DMI operatetes ocean monitoring and operational icecharting

Oceanography Atmosphere Ecosystems
36. Umhverfisstofnun ‐ The Environment Agency of Iceland (Umhverfisstofnun)

The Environment Agency operates under the direction of the Ministry for the Environment. It's role is to promote the protection as well as sustainable use of Iceland’s natural resources, as well as public welfare by helping to ensure a healthy environment, and safe consumer goods. Areas of operation: 1. Information and advice for the public, businesses and regulatory authorities 2. Monitoring of environmental quality 3. Evaluation of environmental impact assessment and development plans 4. Operation supervision, inspection, operating permits, etc. 5. Assessment of conservation effects and registration of unique nature 6. Management and supervision of designated protected areas 7. Wildlife management and conservation 8. Eco‐labeling 9. Labeling and handling of toxic as well as other hazardous substances 10. Coordination of health and safety in public places 11. Coordination of local environmental and health inspectorates 12. Genetically modified organisms (GMO) Main gaps: Metadata archives and metadata availability Network type: ‐ Thematic observations ‐ Community based observations ‐ Coordination

Geology Oceanography Atmosphere Ecosystems
37. Centre d'études nordiques (CEN) Observing Program (CEN)

The Centre for Northern Studies (; CEN: Centre d’études nordiques) is an interuniversity centre of excellence for research involving Université Laval, Université du Québec à Rimouski and the Centre Eau, Terre et Environnement de l'Institut national de la recherche scientifique (INRS). Members also come from the following affiliations: Université de Montréal, Université du Québec à Chicoutimi, à Montréal and à Trois-Rivières, Université de Sherbrooke, and the College François-Xavier Garneau. The CEN is multidisciplinary, bringing together over forty researchers including biologists, geographers, geologists, engineers, archaeologists, and landscape management specialists. The CEN community also counts two hundred graduate students, postdoctoral fellows, and employees. CEN’s mission is to contribute to the sustainable development of northern regions by way of an improved understanding of environmental change. CEN researchers analyze the evolution of northern environments in the context of climate warming and accelerated socio-economic change and train highly qualified personnel in the analysis and management of cold region ecosystems and geosystems. In partnership with government, industry and northern communities, CEN plays a pivotal role in environmental stewardship and development of the circumpolar North. CEN research activities are focused on three themes: 1 -Structure and function of northern continental environments. 2 -Evolution of northern environments in the context of global change. 3-Evaluation of the risks associated with environmental change and development of adaptation strategies. In 2009, CEN organised an international workshop with the European SAON network SCANNET and also partners throughout Canada. The workshop culminated in the formal incorporation of CEN stations within SCANNET ( Main gaps: [Not specified] Network type: CEN operates the CEN Network, an extensive network of meteorological and field stations that were established in consultation with northern communities. The CEN Network comprises over 75 climate and soil monitoring stations and eight field stations distributed across a 4000 km North-South gradient from boreal forest to the High Arctic. The eight field stations are situated at the following sites: Radisson, Whapmagoostui- Kuujjuarapik, Umiujaq, Lac à l’Eau Claire (in the proposed new park Tursujuq), Boniface River, Salluit, and Bylot and Ward Hunt Islands, which are part of two National Parks in Nunavut. The main field station at the heart of the CEN Network is at Whapmagoostui-Kuujjuarapik.

Oceanography Atmosphere Ecosystems
38. Hydrological issues of the glacierized Waldemar River catchment

Recently observed changes in glacierized areas significantly influences on water circulation features in those regions. Project assumes hydrological research in Waldemar River catchment as the example of the High-Arctic glacierized basin. Those investigations began in late 1970’s. From that date substantial changes in catchment characteristic are observed (e.g. decrease degree of glaciation). Glacier-fed river characteristics are well recognized all over the globe. But still there is a need to define how contemporary deglaciation processes affects the water circulation cycle. Basics hydrological features in Waldemar River Catchment are continuously investigated since 1995. In the close feature, a HIWRC programme will be expanded to include research of major glaciohydrological processes in catchment (e.g. internal glacial drainage and it contribution to total outflow). Study assume measurements in a few river points – both in close vicinity of glacier (with no other than glacial water source tributaries) and in lowest part of catchment (with periglacial tributaries).

39. Morphogenetic and morphodynamics conditions of development of the coast of the NW part of Wedel Jarlsberg Land (Spitsbergen) in the late Vistulian and Holocene (MORCOAST)

Arctic coast is extremely sensitive and important area of interaction between land and sea. The diagnosis of the mechanisms governing the polar zone is of fundamental importance for tracing the evolution of the coast caused by climate change. Diagnosis of morphogenesis and morphodynamics of the polar coast becomes important in recent years, a research priority, not only from the scientific point of view, but also practical. Therefore, the key aims of the project include: - determining the dynamics of morphogenetic processes with particular emphasis on marine processes within the coastal zone in the context of climate change after the Little Ice Age (LIA) and the development of model of the coast functioning during this period. - to try to reference this model to the development of the coast at the turn of Vistulian and Holocene (14-8 ka) by defining the stages of shaping the shoreline including glaciizostatic and eustatic and elements of tectonical and lithological features of the coastal zone.

Soils Oceanography
40. Nicolaus Copernicus University Polar Station, Spitsbergen (NCU PS)

The Polar Station of the University of Nicolaus Copernicus is located in the western part of the Oscar II Land, in the northern part of the coastal Kaffiøyra Lowland which is closed by the Forlandsundet from the west. The undertaken research included almost all components of the geographical environment. Scientific programs put pressure on research in glaciology, glacial geomorphology, permafrost and periglacial processes, as well as climatologic and botanical studies. Since 1995 glaciological research and the studies of permafrost of various ground types and their seasonal thawing, as well as meteorological observations have been the major issues on the research agenda. Glaciers pose the dominating feature of the Kaffiøyra region. Since the 19th century their area has decreased by about 30%. Thus, one of the main scientific issues studied there is the course and the reasons for the change in the glaciers’ range. This can be achieved by studying mass balance of the glaciers. Presently, mass balance of four glaciers is studied: the Waldemarbreen, the Irenebreen, the Elisebreen and the Aavatsmarkbreen. 39 The research includes both the summer balance (ablation and outflow from the glaciers) and the winter snow accumulation. The detailed research plans also refer to two large glaciers which end up in the sea. Those are the Aavatsmarkbreen in the north and the Dahlbreen in the south of the Kaffiøyra. Currently, subaquatic glacial relief of the bays in the Forlandsundet region is under scrupulous investigation. The results of the research can be obtained from the station’s website (, from the publications by the World Glaciological Monitoring Service (WGMS- IAHS), as well as the website of the Circumpolar Active Layer Monitoring (CALM- IPA). The research carried out in the N.Copernicus University Polar Station has enabled numerous scientists of most specialties of the Earth sciences (glaciology, climatology, hydrology, geomorphology, pedology and botany) to collect material for numerous papers, including master and doctoral theses. Scientific attractiveness of the Kaffiøyra’s geoecosystem has been appreciated by scientists from various scientific centres in Poland and elsewhere, who take part in interdisciplinary expeditions organized every year. The most Polish polar research in the north-west Spitsbergen is based on the N.Copernicus University Polar Station Once the station has had an extension addend, it can host 10-15 people at any one time. The new section of the station is 32 sq. m downstairs and 24 sq. m upstairs. This includes a study, a workshop, a bedroom as well as two bedroom entresols. The extension is connected with the old section of the station, which includes a living room and a bedroom, but there is also a separate entrance to the new part of the station. Additionally, the station gained extra storage floor, a laboratory, a bathroom, as well as a garage to keep boats, snowmobiles and engines. All together the station now has about 100 sq. m. The station is used 3 to 4 months annually, but it is possible to stay there for as long as a whole year. It is equipped with necessary technical facilities, motor-generators, solar panels, motorboats and snowmobiles. More important measurement equipment includes: a weather station with the basic measuring instruments (the measurements conducted since 1975); automatic weather stations (with the measurements taken at any intervals); limnigraphs and loggers installed in the selected watercourses (measurements of water levels, flow rates and the selected physicochemical features of water since 1975); a system of ablation poles installed on the glaciers; ice drills; loggers for measuring ground temperatures and ice temperatures, and others. The extension of the station in 2007 enabled larger groups of scientists to work and conduct research. The fact that both the living and laboratory space has been enlarged is especially important, as the station is often visited by scientists from all over the world. As a result, the extension will make it possible to intensify current international contacts, as well as start new co-operation projects in the Kaffiøyra region.

Soils Environmental management Atmosphere