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 GeoBasis programme collects data describing the physical and geomorphological environment in Zackenberg, North East Greenland. This includes meteorology, carbon flux and energy exchange, snow cover and permafrost, soil moisture, –chemistry and nutrient balance, hydrology, river discharge and – sediment
The objective of the station is to facilitate ecosystem research in the High Arctic. According to the framework programme of Zackenberg Ecological Research Operations (ZERO) this includes: - Basic quantitative documentation of ecosystem structure and processes; - Baseline studies of intrinsic short-term and long-term variations in ecosystem functions; - Retrospective analyses of organic and inorganic material to detect past ecosystem changes; - Experimental studies enabling predictions of ecosystem responses to Global Change. The programme is coordinated with Nuuk Ecological Research Operations (see below) within the Framework of Greenland Ecosystem Monitoring (GEM). Main gaps: Winter dynamics
The objective is to allow comparative studies of ecosystem dynamics in relation to climate variability and change in respectively a high arctic and low arctic setting as Nuuk Basic comprises the same components as Zackenberg. According to the framework programme of Zackenberg Ecological Research Operations (ZERO) this includes: - Basic quantitative documentation of ecosystem structure and processes; - Baseline studies of intrinsic short-term and long-term variations in ecosystem functions; - Retrospective analyses of organic and inorganic material to detect past ecosystem changes; - Experimental studies enabling predictions of ecosystem responses to Global Change. The programme is coordinated with Zackenberg Ecological Research Operations (see above) within the Framework of Greenland Ecosystem Monitoring (GEM). Main gaps: Winter dynamics
In 2013 a new ecosystem monitoring programme “DiskoBasis” was initiated at Arctic Station on Disko Island, Greenland. The project is partly funded by the Danish Energy Agency. The primary objective of DiskoBasis is to establish baseline knowledge on the dynamics of fundamental physical parameters within the environment/ecosystem around Arctic Station. This initiative extends and complements the existing monitoring carried out at Arctic Station by including several new activities –especially within the terrestrial and hydrological/fluvial field. DiskoBasis include collection of data in the following sub-topics; • Gas flux, meteorology and energy balance • Snow, ice and permafrost • Soil and soil water chemistry • Vegetation phenology • Hydrology -River water discharge and chemistry • Limnology -Lake water chemistry • Marine -Sea water chemistry
Measurements of gamma-radiation in the environment (from ground to cosmos). Radioactivity in Intensive Net is measured on the soil surface at 28 sites in Sweden. The measurements are continuous and sound the alarm if radioactivity increases. Measured is the dose rate of gamma radiation. Radioactivity in Extensive Net is concerned all municipalities in Sweden which has got one instrument for gamma radiation measurement and each county board has got two. Every seventh month they measure radioactivity at two to four predefined spots as reference measurement. Radioactivity in Air is conducted at five stations with air filter sampling and analysis of radioactivity maintained by Swedish Defence Research Agency (FOI). Out of these stations Umeå and Kiruna are located in northern Sweden.
This project has been divided into two new projects: The Swedish Forest Soil Inventory and the Swedish National Forest Inventory.
The Swedish National Forest Inventory has the task of describing the state and changes in Sweden's forests. The inventory gathers basic information on forests, soils and vegetation. It includes most aspects concerning soils, for example: soil types, soil chemistry including organic matter, water conditions and content of stones and boulders. Acidification, nitrogen deposition and the contribution by soils to climate change are some of the current issues dealt with. Regularly reported variables are: forest state, injuries, and growth, logging operations, new forest stand, and environmental assessment. Invented variables on permanent sampling plots include: position in the landscape, field vegetation, site conditions, soil sampling, assesment of soil characteristics, chemical analysis of soil in O-, B-, BC- and C-horizons.
This project was previously a part of the project: National Survey of Forest Soils and Vegetation.
The Swedish Forest Soil Inventory (SFSI) is part of the national environmental monitoring programme Forests and collects information about soil conditions and chemistry from around 23 500 permanent plots throughout Sweden. One tenth of these sampling plots are re-visited each year. The inventory is commissioned by the Swedish Environmental Protection Agency and is carried out by the Department of Soil and Environment at the Swedish University of Agricultural Sciences (SLU).
The inventory gathers basic information on soils and vegetation on predominantly forest land, but also semi-natural grassland and wetland below the alpine forest limit. It includes most aspects concerning soils, for example: soil types, soil chemistry including organic matter, water conditions and content of stones and boulders. Acidification, nitrogen deposition and the contribution by soils to climate change are some of the current issues dealt with. There is a close collaboration between the SFSI and the National Forest Inventory (NFI), and the inventoried plots are a subset of the NFI plots. .
The first sampling for the soil and vegetation inventory of arable land was done in 1994-1995. The program covers arable land in Sweden and is designed to describe the state of Swedish arable land and the quality of the crop in relation to soil status, cultivation measures, and means of operation. At present soil sampling is made in 2000 fixed sampling points visited every 10th year.
Iceland GeoSurvey ÍSOR is a self‐financing, state‐owned, non‐profit institution in the field of natural sciences, it’s main activity being related to the geothermal industry in Iceland and abroad. It was established 2003, when the GeoScience Division of Orkustofnun (the National Energy Authority of Iceland), was spun off as a separate entity according to the law of Iceland GeoSurvey no. 86, March 26th 2003 (http://www.althingi.is/lagas/135a/2003086.html). The main role of ÍSOR is to work on projects and research in the field of natural resources and energy, as the directive board of the institute decides. ÍSOR offers research consulting services worldwide on most aspects of geothermal exploration, development, and utilization, and provide training and education on related issues. It is based on six decades of continuous experience in the field of geothermal and hydropower research and development. The focus is on geothermal exploration, development, and utilization, but cover also many other geoscience‐related fields as well, including groundwater studies, marine geology, and environmental monitoring. Main gaps: Not specified Network type: Field stations Thematic observations
Project aims indicate of changes of main terrestrial cryosphere components – glaciers and permafrost. Research on glaciers assumes both to inspect recent changes (mass balance, geometry, thermal structure and widely understood dynamics) and to reconstruct past events (especially in base on subaqual records in the marine-part forefields of the tide-water glaciers). Selected research results are part of the World Glacier Monitoring Service (WGMS). The most widely studied are Waldemar Glacier, Irene Glacier and Elise Glacier. Several research aspects, such as geometry of glaciers are investigated for more than 30 years, since first NCU Polar Expedition in 1975. Permafrost investigations are focused on the depth of the summer active layer thawing and thermal properties of it. Selected results constitutes a part of Circumpolar Active Layer Monitoring (CALM) programme.
1. To establish, on the basis of common methods, a periodic inventory of damage caused to forests, in particular by atmospheric pollution. 2. To establish or extend, in a co-ordinated and harmonious way, the network of observation plots required to draw up that inventory. 3. To conduct intensive, continuous surveillance of forestry ecosystems. 4. To establish or extend, in a co-ordinated and harmonious way, a network of permanent observation plots required for such intensive, continuous surveillance.
Vascular plants and mosses are also terrestrial bioindicators for radioactive fallout, The summer fodder of reindeer consist of 200- 300 vascular plants . Therefore vascular plants are an important link in the foodchain plants - reindeer/game - man. STUK has several permanent plant sampling sites, usually in the vicinity of the lichen plots. Only a few of of them are included in Finnish NIP. The results obtained are gammanuclide or occasionally also 90Sr concentrations, Bq/kg.
Geochemical mapping project based on multimaterial and -elemental method covering the NW Russia and adjacent areas of Finland and Norway. NW-Russia is of strategic importance not only for Europe but also for the sosio-economic development of the whole Russia for its richness in natural resources. Their use must be based on environmentally acceptable principles. In addition, within the area exist numerous industrial centres whose environmental impacts are unknown. The information produced by the project is significant for the future development of the area and remedial measures of the environment. The project lead by the applicant, will be carried out in 1999-2003 in cooperation with Russian and Norwegian partners.
Lichens are the best terrestrial bioindicators for radioactive fallout and also the most important link in foodchain lichen - reindeer - man. Generally, Fenced permanent sampling plots are used to study the biological half-life of 137Cs in lichen. However, some of the STUKs sampling plots are unfenced which are subjected to grazing by reindeer. Start year: early 60's as a project of the Radiochemistry Department of University in Helsinki. Stuk's participation since 1975. Data are collected from 1961, 1980, 1982 or 1986, continuously every 3-5 years. Data processing/work-up and data archiving/reporting work are conducted from 1961, 1980, 1982. Continous data sets from 1986 to 2010.
Monitoring follows groundwater level and quality as well as changes in soil humidity and frost depth in winter.
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).
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.
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 (www.stacja.arktyka.com), 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.
The study includes comprehensive study of the geographical environment in the area of Polar Station of Maria Curie-Skłodowska University in Calypsobyen (NW part of Wedel Jarlsberg Land, Svalbard). Currently, studies have been carried out within research projects: - Dynamics of matter circulation in the polar catchment are a subject to deglaciation processes (Scottelva, Spitsbergen) (DYNACAT) - 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) - Mechanisms of fluvial transport and sediment supply to Arctic river channels with various hydrological regimes (SW Spitsbergen) (ARCTFLUX)
More information about the following long-term observing activity will be available in due course. • Soil survey program description: http://www.ak.nrcs.usda.gov/soils/index.html • Soil climate survey program description: http://www.ak.nrcs.usda.gov/soils/SoilClimateSites/SoilClimateSites.html • For information and data, contact: Rick McClure, email@example.com