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Projektet er en fortsættelse og videreudvikling af det igangværende projekt FARMON og har til formål at forlænge og forbedre monitering af to strømsystemer gennem færøsk territorialfarvand, som udveksler vand, varme og salt mellem Arktis og resten af Verdenshavet. Den ene af disse er strømmen af koldt vand fra Arktis gennem dybet af Færøbanke kanalen (FB-overflow), som transporterer varme og kuldioxid fra atmosfæren ned i Verdenshavets dybe vandmasser. Den anden er Færøstrømmen, som er den stærkeste transportør af ocean varme mod Arktis med indvirkning på klima, fiskebestande og isudbredelse. Endvidere vil projektet studere opsplitningen af Færøstrømmen i to separate strømgrene med forskellig indflydelse på forskellige områder og processer i Arktis. Projektet vil omfatte feltaktivitet fra sommer 2018 til sommer 2019 med udlagte måleinstrumenter og tilsammen fire hydrografiske togter med forskningsskib. Indsamlede måledata vil blive analyseret sammen med satellitdata og historiske observationer med henblik på at forlænge de mere end 20 år lange tidsserier for de to strømsystemers transporter. Et nyt indsatsområde inden for FARMON II vil være mere detaljerede studier af FB-overflow vandets egenskaber. Tidligere har vore målinger vist en langsom opvarmning af bundvandet i Færøbanke kanalen siden begyndelsen af dette århundrede uden at dette dog har medført reduceret massefylde. Nu ser denne opvarmning imidlertid ud til at have accelereret, samtidig som saltholdigheden i de øvre lag er faldet. Vi vil derfor foretage mere detaljerede målinger for at følge opvarmningen og dens indvirkning på massefylde og dermed på den termohaline forcering af den såkaldte AMOC (Atlantic Meridional Overturning Circulation).
The WOW project is a cooperation between Havstovan (Faroe Marine Research Institute, HAV) and the Danish Meteorological Institute (DMI) to 1) measure the overflow of cold water from the Arctic into the rest of the World Ocean through the Western Valley of the Iceland-Faroe Ridge, to 2) allow the effects of this flow to be adequately simulated in climate model projections of the thermohaline circulation and the heat transport towards the Arctic, and to 3) design a low-cost monitoring system for this flow.
The purpose of this project is to measure and calculate pCO2 and pH in high Arctic coastal sea ice. The measured pCO2 and pH values can be compared to the calculated values based on measurements of salt, temperature, TCO2 and TA ratios in the sea ice, which will be measured concurrently. Since algorithms for pCO2 calculations have not yet been developed for sea ice, this will contribute with useful knowledge.
The GeoBasis Disko monitoring program started in 2017 as a part of the cross disciplinary Greenland Environmental Monitoring (GEM) program. GeoBasis Disko is an integrated part of the GeoBasis program, following the same standards as in Nuuk and Zackenberg (two other GEM sites) and largely focusing on the same parameters and methodologies. GeoBasis Disko is finaced by Danish Ministry of Energy, Utilities and Climate.
A close collaboration and synergy with Arctic Station that is manned year round makes it possible to collect and carry out measurements also during winter.As location Qeqertarsuaq on the south coast of the Disko island, represent a Greenlandic west coast climate, with annual mean temperatures just below 0°C, with discontinuous permafrost, and as such remarkably different from the two existing GEM sites. Further, the Disko bay area is highly interesting from a socioeconomic perspective due its high population and active fishery industry, and as one of the most popular tourist destinations in Greenland.
The primary objective of GeoBasis Disko is to establish baseline knowledge on the dynamics of fundamental abiotic terrestrial parameters within the environment/ecosystem around Arctic Station. This is done through a long term collection of data that includes the following sub-topics;
GeoBasis focuses on selected abiotic parameters in order to describe the state of Arctic terrestrial environments and their potential feedback effects in a changing climate. As such, inter-annual variation and long-term trends are of paramount importance.
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 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
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
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
Projektet har til formål at forlænge og forbedre monitering af to strømsystemer gennem færøsk territorialfarvand, som udveksler vand, varme og salt mellem Arktis og resten af Verdenshavet. Den ene af disse er strømmen af koldt vand fra Arktis gennem dybet af Færøbanke kanalen, som transporterer varme og kuldioxid fra atmosfæren ned i Verdenshavets dybe vandmasser. Den anden er Færøstrømmen, som er den stærkeste transportør af ocean varme mod Arktis med indvirkning på klima, fiskebestande og isudbredelse. Endvidere vil projektet studere opsplitningen af Færøstrømmen i to separate strømgrene med forskellig indflydelse på forskellige områder og processer i Arktis. Projektet vil omfatte feltaktivitet fra sommer 2017 til sommer 2018 med udlagte måleinstrumenter og tilsammen fire hydrografiske togter med forskningsskib. Indsamlede måledata vil blive analyseret sammen med satellitdata og historiske observationer med henblik på at forlænge de ca. 20 år lange tidsserier for de to strømsystemers transporter samt at rationalisere det eksisterende moniteringssystem, således at det i fremtiden vil være mindre afhængigt af kostbare in situ målinger.
Ice sheet meltwater and sediment discharge is measured at only very few sites in Greenland. The measurements provide detailed insights into ice sheet surface melting, englacial meltwater routing, subglacial erosion, etc., and their importance increase with the lengthening of the time series. Monitoring was initiated by IGN (Copenhagen University) in 2006, and taken over by the Geological Survey of Denmark and Greenland in 2014. Data are available through the Programme for Monitoring of the Greenland Ice Sheet (www.PROMICE.dk).
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
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 meteorology, carbon flux and energy exchange, snow cover and permafrost, soil moisture, –chemistry and nutrient balance, hydrology, river discharge and – sediment
Monitoring climatological and hydrological parameters in a low arctic environment.
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.
AMAP Core project 2016-2018 is a continuation of previous project which was initiated in 1994. The programme is a monitoring programme of contaminant concentrations in Greenland animals with the objective to follow the temporal trends. The programme includes also screening of contaminants of emergent concerns of selected samples and in some cases retrospective studies of such compounds. Monitoring of temporal trends of effects and biomarkers in samples of polar bears is also included.
The main objective is resource monitoring of Greenland Halibut.
The Arctic Station is located on the south coast of the Disko Island in central west Greenland. It is thus facing the Disko Bay and is characterized by an arctic, marine climate. There are 3 building comprising guest facilities, staff accomodation, laboratory and library that are located in a nature sanctuary, approximately 1 km west of a small town, Qeqertarsuaq (formerly Godhavn), with ca. 1100 inhabitants. Within the town community is located all necessary service facilities, incl. several shops, bank, postoffice, church and a hospital. The station offers a 'state of the art' platform for year-round environmental research. The Arctic Station maintains a stat-of-the-art automatic weather station located in the immediate vicinity of the Arctic Station. The datalogging at Arctic Station (every half hour) comprises: air temperatur, humidity, incoming and outgoing radiation, wind speed and direction, rainfall, ground temperatures (5, 60 and 150 cm below surface) and temperature in solid rock 2 metre below surface. In addition to the above the station also maintains a freshwater, a marine and a terrestrial monitoring program. The whole moitoring program is call DiskoBasic.
CBMP is a cornerstone monitoring program of Conservation of Arctic Flora and Fauna (CAFF). It is a international network of scientists, government agencies, Indigenous organizations and conservation groups working together to harmonize and integrate efforts to monitor the Arctic's living resources. (... more to be edited from the co-lead countries)