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Directory entires that have specified Greenland as one of the geographic regions for the project/activity and are included in the AMAP, ENVINET, SAON and SEARCH directories. Note that the list of regions is not hierarchical, and there is no relation between regions (e.g. a record tagged with Nunavut may not be tagged with Canada). To see the full list of regions, see the regions list. To browse the catalog based on the originating country (leady party), see the list of countries.
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To provide the data necessary for quantifying the dynamics of arctic ecosystems, i.e. at the two field sites at respectively Zackenberg (Northeast Greenland) and Nuuk (West Greenland) Main gaps: Winter dynamics
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
The purpose of the BioBasis programme is to monitor basic qualitative and quantitative elements of biodiversity in the terrestrial ecosystems at Zackenberg in Northeast Greenland. The programme provides data on typical High Arctic species and processes that can be expected to react on year to year variation in climate as well as long-term climate change. It includes 30 variables of terrestrial and limnic plant, arthropod, bird and mammal dynamics in the Zackenberg valley.
Monitoring climatological and hydrological parameters in a low arctic environment.
The objective of the project is to identify compounds in Arctic environmental and human samples, which have not previously been studied in the Arctic. By using both high performance liquid chromatography (HPLC) or gas chromatography (GC) HPLC and GC techniques, a broad spectrum of compounds of different polarity will be covered, including metabolites
The objective of this project is to improve the current situation of incomparable Arctic data and lack of routine analyses of short-chain chlorinated paraffins (SCCPs). The project will work towards an agreement on one method, which will be implemented and described in terms of quality parameters and analytical protocols, as is common practice in chemical monitoring programmes
The aim of the present project is to continue the monitoring of contaminants Greenland biota in order to detect temporal and geographical changes including screening and retrospective analyses of "new" contaminants of increasing concern. Furthermore, temporal trend monitoring of selected biomarkers (e.g. bone mineral density and histopathological changes) in polar bear are included in the monitoring as these have shown to be sensitive to stressors such as contaminants. The project will provide the fundamental basic knowledge of temporal trends and feed into international geographical trend studies of mainly long range transport of contaminants in the atmosphere and biota to Greenland. The project will provide an important input to international convention works such as the Stockholm Convention and the Long-range Trans-boundary Air Pollution.
The main objective is to quantify the annual mass loss of the Greenland ice sheet, track changes in the extent of local glaciers and ice caps, and track changes in the position of the ice-sheet margin. Network type: - Observing and modelling the ice-sheet surface-mass balance - Quantifying the mass loss caused by iceberg calving - Monitoring the change of glaciers and ice caps in Greenland - Outlook
Important progress has been made in recent decades to describe and understand how arctic terrestrial vertebrate interact, especially concerning predator-prey interactions. Indirect interactions between different prey species modulated by shared predators (e.g. Arctic fox) are believed to have important impacts on the structure and/or dynamics of some communities. Yet, our understanding of these types of interactions is still fragmentary. To fill that gap, we will build on ongoing projects exploring related questions in Canada (Marie-Andrée Giroux, Nicolas Lecomte, Joël Bêty) and Greenland (Olivier Gilg, Niels M. Schmidt), while taking advantage of existing networks (ADSN in North America and “Interactions” program in Greenland and Eurasia). The aim of the project is to promote the implementation of several common protocols that will (1) improve each collaborator’s knowledge at the site level and, more importantly, that will (2) be merged across sites and years to improve our understanding of the functioning and the influence of indirect interactions on arctic vertebrate communities in general.
Five types of data have been identified (by the 5 initiators of the project already mentioned above) as being mandatories to answer questions related to this topic. These data sets will be collected using 5 specific protocols described in the following chapters:
Monitoring of the sea-level
Dual purpose: Supporting geographical infrastructure in and around Greenland Monitoring changes in Greenland ice sheet as part of GNET
The GeoBasis programme collects data describing the physical and geomorphological environment in Zackenberg, North East Greenland. This includes CO2-flux, snowcover and permafrost, soil moisture, –chemistry and nutrient balance, hydrology, river discharge and –sediment. GeoBasis also supports the ClimateBasis programme with service and datahandling during the field season.
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
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.
Our objective in present SAON meeting was to know more about SAON activities and plannings to coordinate and promote guidelines criteria for observations in the ARctic Present Spain Research in Arctic is performed mainly for universities and scientific institutions , down the responsability of the Science Department with the support of several national institutions including the Defense Department and Foreign Affairs Institutions are coordinated by the National Polar Committee. The National Scientific Program finance the activities in the polar zones Although our main scientific activities are in Antarctica the activity of Spain in Arctic is rapidly increasing following the fact that Arctic research is a priority task in our Science Program At present we have detected 16 scientific groups working activelly in the differnts fields of Arctic topics (glaciology, meteorology, permafrost, high atmosphere, ecology, physical oceanography, marine geology and biology) These activities are mainly performed in cooperation with Arctic countries Institutions via institutional or researchers contacts About our media to work in Arctic ocean Spain has at present two multiporposes oceanographic research ships In the last years our Ocanographic ship Hesperides has developed two campaigns in The area of Greenland and Svalvars Island in the fields of marine Geology , marine biology and physical oceanography For next summer Hesperides will perform a third oceanographic campaign close to the Atlantic coast of Greenland Other national institutions have been working in marine biology campaigns including fisheries stock evolution Spain has a National Centre of Polar Data were all researchers must enter their raw data gathered in the polar campaigns We considerer , at present , our interest to cooperate inside SAON board, considering that besides other possible cooperation to SAON tasks could be a cooperation with our Polar Data Centre
Temporal trend monitoring of contaminants in atmosphere and biota in Greenland. Modelling the atmospheric transport pathways and deposition of contaminants in the Arctic as well as determination of climate related parameters.
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
NASA satellites (Figure 13) support an extensive Global Water Cycle science focus area and contribute to high accuracy, stable, sustained observations and associated modeling for terrestrial hydrology and cryosphere studies. Derived geophysical products for terrestrial hydrology and cryosphere are available from the NSIDC’s Distributed Active Archive Center (DAAC). They include: soil moisture and snow water equivalent from AMSR-E; Greenland ice sheet altimetry and global land surface altimetry from ICESat/GLAS; snow cover extent/area from MODIS; surface albedo and temperature from AVHRR Pathfinder. SAR data obtained from a variety of foreign satellites since 1991 are archived at the ASF DAAC. SAR data provide opportunities for change detection, including interferometric SAR (InSAR) studies of glacier and ice sheet surface elevation and dynamics (ice velocity maps), land surface elevation, and soil moisture. GRACE has been used to determine the mass loss from the Greenland ice sheet and from glaciers in southeast Alaska. The surface elevation of the Greenland ice sheet is mapped using ICESat, and the Advanced Spaceborne Thermal Emission and Reflec¬tion Radiometer (ASTER) is used to acquire imagery and topography of the ice sheet.