Arctic SDI catalogue
Arctic SDI catalogue (Arctic SDI)
Continents, countries, sea regions of the world.
Ministry of Transportation (MOT) Regional Boundary
Ministry of Transportation Regional Boundary is an exclusive geographic area within the province that the Ministry organizational unit is responsible for. Each Ministry Region is partitioned into one or more non-overlapping Ministry Districts that cover the entire Ministry Region
An interpretation of bedrock geology, topography and other sources of information that shows the potential for karst formations. This is a reconnaissance level map for all of British Columbia
Rýmingareitir í þéttbýli vegna snjóflóðahættu
Þjónustan sýnir rýmingarreiti á þéttbýlisstöðum landsins þar sem talin er snjóflóðahætta. Reitaskiptinguna hefur Veðurstofan gert í samráði við heimamenn, og birt á sérstökum kortum og byggja rýmingaráætlanir staðanna á þessari reitaskiptingu. Samkvæmt lögum um varnir gegn snjóflóðum og skriðuföllum (49/1997) ber Veðurstofu Íslands að gefa út viðvaranir um staðbundna snjóflóðahættu. Skal þá rýma húsnæði á reitum sem tilgreindir eru í viðvörun Veðurstofunnar.
This work is licensed under a Creative Commons Attribution 4.0 International License (CC-BY)
Byggt á hættu- og áhættumati vegna snjóflóða.
Base de donnees topographiques du Québec
This service is comprised of Provincial Wet Areas Mapping (WAM), which is the product of research work carried out by the Nexfor/Bowater Forest Watershed Research Centre at the University of New Brunswick (led by Dr. Paul Arp). This project was funded by several government and industry partners (see list of partners below). The WAM model predicts where water will naturally flow and/or accumulate in the landscape based on digital elevation (DEM) data and the known location of surface water bodies and wetlands. In essence, WAM is a "cartographically derived depth-to-water index." It is important for users of WAM to understand that depth values listed do not represent predicted depth to a water table or ground water, rather they are a relative wetness index which can be related to the likelihood of there being natural water flows (above or below ground) and accumulation of water as reflected by on-site drainage conditions (well, moderately well, imperfect, poor, very poor). WAM does not take into account soil conditions that may further influence drainage conditions (such as soil texture), nor does it predict flows and accumulations that are the result of human disturbance or infrastructure. The WAM project was completed under contract by the University of New Brunswick in 2005-2007. Contributing partners to the project were: - Nova Scotia Department of Natural Resources - Bowater Mersey Paper Ltd. - J.D. Irving Ltd. - Neenah Paper Inc. - StoraEnso Port Hawkesbury Ltd. - Nova Forest Alliance Model Forest - Agriculture and Agri-Food Canada - Parks Canada - Nova Scotia Environment and Labour - Service Nova Scotia WAM products made available here for public use are through the courtesy of project partners.
This dataset contains linear features constructed by beavers. The linear features are captured to scale on: * single line rivers * lakes * double line rivers We are no longer updating this data. It is best suited for historical research and analysis.
START - Figure 3.31 - Location and trends of lemming populations
Lemmings are currently being monitored at 38 sites. Their status and trends were determined based on data from these sites as well as recent data (since 2000) from an additional 11 previous monitoring sites (Figure 3-31). Of those sites monitored, Fennoscandia is overrepresented relative to the geographical area it covers, whereas Russia is underrepresented. Based on the skewed geographical coverage, more information is available for some species of lemmings than others, particularly the Norwegian lemming. STATE OF THE ARCTIC TERRESTRIAL BIODIVERSITY REPORT - Chapter 3 - Page 80 - Figure 3.31
https://geo.abds.is/geonetwork/54294151-9e15-4457-8a44-df2c0ec5ada5 http://geo.abds.is/geonetwork54294151-9e15-4457-8a44-df2c0ec5ada5
Regional divisions of the marine Arctic, as determined by the Marine Expert Monitoring Group of the Circumpolar Biodiversity Monitoring Programme (CBMP). The Circumpolar Marine Biodiversity Monitoring plan identifies eight Arctic Marine Areas where a suite of common parameters, sampling approaches and indicators will be used. Regionally specific parameters may also be applied. Exact boundaries may change over time to reflect changing bio-physical conditions. Published in the Arctic Marine Biodiversity Monitoring Plan, Chapter 2, page20 - released in 2011
Circumpolar Biodiversity Monitoring Program
Group of neighbouring municipalities joined together for the purposes of regional planning and managing common services (such as police or ambulance services). These groupings are established under laws in effect in certain provinces of Canada. Census division (CD) is the general term for provincially legislated areas (such as county, municipalité régionale de comté and regional district) or their equivalents. In other provinces and the territories where laws do not provide for such areas, Statistics Canada defines equivalent areas for statistical reporting purposes in cooperation with these provinces and territories. Census divisions are intermediate geographic areas between the province/territory level and the municipality (census subdivision).
Original metadata (https://catalogue.data.gov.bc.ca)
https://www.publicdocs.mnr.gov.on.ca/mirb/Beaver Dam - Documentation.docx
Original metadata (https://data.ontario.ca)
Original metadata (https://data.ontario.ca/fr)
Data Description (extracted from geohub)
Beaver Dam - Data Download Package (extracted from geohub)
Arctic Marine Biodiversity Monitoring Plan
Government of British Columbia; Government of British Columbia; Construction and Maintenance
Government of Canada; Library and Archives Canada
Government of British Columbia; Government of British Columbia; FAIB Data Management
Government of Ontario; Government of Ontario; Natural Resources and Forestry
Conservation of Arctic Flora and Fauna (CAFF)
Gouvernement du Canada; Ressources naturelles Canada
Baltic Sea - DIVAnd 4D 6-year seasonal analysis of Water body dissolved oxygen concentration 1950/2023 v2025
Running 6-year analysis of Water body dissolved oxygen concentration in the Baltic Sea. Four seasons (March-May, June-August, September-November, December-February). Every year of the time dimension corresponds to a 6-year centred average. Periods span between 1950-2023. Analyses for depths (m) (HELCOM standard depths): 0, 5, 10, 15, 20, 30, 40, 50, 60, 70, 80, 90, 100, 125, 150, 175, 200, 225, 250, 275, 300. Data Sources: observational data from SeaDataNet/EMODnet Chemistry Data Network. Description of DIVA analysis: Geostatistical data analysis by DIVAnd (Data-Interpolating Variational Analysis in n dimensions) tool. GEBCO_08 Grid (30 arc-seconds) topography is used for the contouring preparation. Files contain analysed fields, error fields and combined field with the deepest value for each grid point selected. Also pre-masked fields using relative error threshold 0.3 and 0.5 are included. In the analyses the horizontal correlation length is fixed to 80 km and decreasing towards the coastline, the vertical correlation length is varying with depth. Signal to noise ratio is fixed to 1.0. Background fields were created using data for the given time period and season. Log transformation was used in the analyses. No detrending, advection constraints or weighting are applied. Unit is umol/l.
Usage is subject to mandatory citation: "This resource was generated by EMODnet Chemistry under the support of DG MARE Call for Tender EASME/2019/OP/0003-lot4."
The data used as input for this product have been extracted from the EMODnet Chemistry Download Service: http://emodnet-chemistry.maris2.nl/v_cdi_v3/search.asp
Jarðfræðikort af Vesturgosbelti 1. útgáfa – 1:100.000
Gagnasafn [GDB] NI_J100v_Vesturgosbelt_1.utg: Jarðfræðikort af Vesturgosbelti Íslands í mælikvarði 1:100.00, 1. útg. [Geological map of the Western Volcanic Zone of Iceland in the scale of 1:100.000, 1st ed.] Kortið sýnir jarðlög, gíga, höggun, strik og halla, framhlaup og niðurföll, steingervinga, jökulrákir, jökulgarða, jökulkembur, malarása og fornar strandlínur stöðuvatna. Jarðlög eru flokkuð eftir aldri, gerð og samsetningu. Kortið var unnin í samstarfi Náttúrufræðistofnunar Íslands og Íslensku Orkurannsoknastofa. Tilvísun: Birgir V. Óskarsson, Ögmundur Erlendsson, Robert A. Askew, Árni Hjartarson, Magnús Á. Sigurgeirsson, Skafti Brynjólfsson og Sveinn Jakobsson 2022. Jarðfræðikort af Vesturgosbelti. 1.100.000. 1. útg. Garðabær: Náttúrufræðistofnun Íslands, Íslenskar Orkurannsóknir og Umhverfis- og Auðlindaráðuneytið. [The map displays bedrock geology, volcanic craters, tectonics, strike and dips, landslides and collapse pits, fossils, glacial striations, glacial moraines, flutes, eskers and ancient lake strandlines. Bedrock is classified by age, type, and composition. The map was completed in a collaborative project between the Icelandic Institute of Natural History and the Icelandic Geosurvey. Bibliographic reference: Birgir V. Óskarsson, Ögmundur Erlendsson, Robert A. Askew, Árni Hjartarson, Magnús Á. Sigurgeirsson, Skafti Brynjólfsson og Sveinn Jakobsson 2022. Geological map of the Western Volcanic Zone, Iceland. 1:100.000. 1st edition. Garðabær: Icelandic Institute of Natural History, Iceland GeoSurvey and Ministry for the Environment and Natural Resources.]
https://www.natt.is/is/midlun/opin-gogn Gögnin eru öllum opin – no limitations on public access
Kortlagning var unnin arinu 2019 og 2020 af jarðfræðingar hjá Nátturufræðistofnun Íslands (NÍ) og Íslensku Orkurannsoknastofa (ÍSOR). Gögnin var byggt úpp frá vetvangsvinnu jarðfræðingar hjá NÍ og ÍSOR tengt við útgefin gögn frá nokkrar heimildir. Sérstök áhersla var lögð á að uppfæra og auka nákvæmni eldri kortagagna og uppfæra jökullínur með fleiri uppfærðum upplýsingum frá Vedurstofunni. Kortið hefur verið athugað og yfirfarinn að innan. [Mapping was undertaken in the years 2019 and 2020 by geologists at the Icelandic Insitute of Natural History and the Icelandic Geosurvey. Field data was combined with previous mapping and published maps and other data.] Heimildir [Sources]: - Ásta R. Hjartardóttir, Páll Einarsson, and S. G. Björgvinsdóttir 2016. Fissure swarms and fracture systems within the Western Volcanic Zone, Iceland–effects of spreading rates. Journal of Structural Geology, 91, pp.39-53. - Arnór Karlsson og Oddur Sigurðsson 2001. Kjölur og kjalverðir. Árbók FÍ. - Árni Hjartarson 2014. Hallmundarkviða, eldforn lýsing á eldgosi. Náttúrufræðingurinn 84, 27-37. - Árni Hjartarson 2015. Hallmundarkviða, áhrif eldgoss á byggð og mannlíf í Borgarfirði. Náttúrufræðingurinn 85, 60-67. - Ágúst Guðmundsson 1987. Tectonics of the Thingvellir fissure swarm, SW Iceland. J Struct Geol 9:61–69. - Ágúst Guðmundsson 1996. Ofan Hreppafjalla milli Hvítár og Þjórsár í Árnessýslu. Árbók FÍ - Beasley, F.K. 2002. The structure and genesis of a typical Icelandic tuya, Efstadalsfjall, south-west Iceland. Univ. of St. Andrews, BSc Hon Essay, pp 1–93. - Birgir Jónsson 1969. Jarðfræði Haukholtasvæðis við Hvítá (with an English summary). Reykjavík apríl 1969. - Eason, D.E., Sinton, J.M. 2009. Lava shields and fissure eruptions of the Western Volcanic Zone, Iceland: evidence for magma chambers and crustal interaction. J Volcanol Geotherm Res 186:331–348. - Eason, D.E., Sinton, J.M., Karl Grönvold & Kurz, M.D. 2015. Effects of deglaciation on the petrology and eruptive history of the Western Volcanic Zone, Iceland. Bull Volcanol 77:47. - Freysteinn Sigurðsson 2004. Borgarfjarðarhérað milli Mýra og Hafnarfjalla. Árbók FÍ - Guðmundur Kjartansson 1943. Yfirlit og jarðsaga. Náttúrulýsing Árnessýslu, fyrri hluti. Árnesinga saga I. Árnesingafélagið, Reykjavík. - Guðmundur Kjartansson 1980 í Fold og vötn m.a. um Ísaldarlok á Kili o.fl. Reykjavík, Menningarsjóður 1980. Líka í Nátt. 1964 34 (1. Hefti) bls. 9-38. Guðmundur Kjartansson 1970. Úr sögu berggrunns og landslag á Miðsuðurlandi. Suðri; bls. 12-100 í 2. bindi 1970 - Haukur Jóhannesson 1980. Jarðlagaskipan og þróun rekbelta á Vesturlandi. Náttúrufræðingurinn 50, 13-31. - Haukur Jóhannesson 1989. Aldur Hallmundarhrauns í Borgarfirði. Fjölrit Náttúrfræðistofnunar Íslands 9, Náttúrufræðistofnun Íslands, Reykjavík. - Haukur Tómasson 1993. Jökulstífluð vötn á Kili og hamfarahlaup í Hvítá í Árnessýslu. Nátt. 1993 62 (1.-2. hefti) bls. 77-98. - Helgi Torfason 2010. The great Geysir. Geysisnefnd, Reykjavík. (bæklingur) - Ingvar Birgir Friðleifsson 1979. Honours Research Essay, St. Andrews, 1970 (Stóra Laxá). Í safni ÍSOR nr. 12473 í kassa 1290 í safni ÍSOR 2. Hæð - Jones, J.G. 1969. Intraglacial volcanoes of the Laugarvatn region, south-west Iceland-I. Quart J Geol Soc Lond 124:197–211. - Jones, J.G. 1970. Intraglacial volcanoes of the Laugarvatn region, south-west Iceland-II. J Geol 78:127–140. - Kristján Sæmundsson og Noll, H. 1974. K/Ar ages of rocks from Husafell, Western Iceland, and the developement ot the Husafell central volcano. Jökull 24, 40-59. - Kristján Sæmundsson 2002. Jarðfræði Þingvallavatns og vatnasviðs þess. Í: Pétur. M. Jónasson og Páll Hersteinsson (ritstjórar). Þingvallavatn. Undraheimur í mótun. Mál og menning, Reykjavík, s. 40-63. - Magnús Tumi Guðmundsson, Þórdís Högnadóttir, Sveinn P. Jakobsson 2000. Hraun og móbergsmyndanir sunnan Langjökuls. Niðurstöður Þyngdarmælinga. Raunvísindastofnun Háskólans, RH-28-2000, Reykjavík, 37 s. - McDougall, I., Kristján Sæmundsson, Haukur Jóhannesson, Watkins, N.D. og Leó Kristjánsson 1977. Extension of the geomagnetic polarity time scale to 6.5 m.y.: K-Ar dating, geological and paleomagnetic study of a 3,500-m lava succession in western Iceland. Geological Society of America Bulletin 88, 1-15. - McGarvie, D.W., Stevenson, J.A., Burgess, R., Tuffen, H. and Tindle, A.G. 2007. Volcano-Ice interactions at Prestahnúkur, Iceland: rhyolite eruption during the last interglacial-glacial transition. Annals of Glaciology 45, 38-47. - Sinton, J., Karl Grönvold og Kristján Sæmundsson 2005. Postglacial eruptive history of the Western Volcanic Zone, Iceland. Geochemistry, Geophysics, Geosystems 6, 1-34. - Skilling, I.P. 2009. Subglacial to emergent basaltic volcanism at Hlöðufell, south-west Iceland: a history of ice-confinement. J Volcanol Geotherm Res 185:276–289. - Sveinn P. Jakobsson 2013. Vesturgosbelti. Í Júlíus Sólnes, Freysteinn Sigmundsson og Bjarni Bessason (ritstjórar), Náttúruvá á Íslandi – Eldgos og jarðskjálftar (358 - 365). Reykjavík: Viðlagatrygging Íslands/Háskólaútgáfan. - Sveinn P. Jakobsson og Johnson, G.L. 2012. Intraglacial volcanism in the Western Volcanic Zone, Iceland. Bulletin of Volcanology 74, 1141-1160. - Tómas Tryggvason 1943. Das Skjaldbreid-Gebiet auf Island – Bull. Geol. Inst. Uppsala 30. 273-320. - Trausti Einarsson 1957. Magneto-geological mapping in Iceland with the use of a compass. Advances in Physics, 6(22), pp.232–239. - Þorleifur Einarsson 1982. Saga Hvítárgljúfurs og Gullfoss í ljósi öskulagarannsókna. Eldur er í Norðri bls. 44-451. - Þorleifur Einarsson 1965. Greinargerð um jarðfræði Tungufellssvæðisins. Rvk. Raforkumálastj. 1965. Kortalisti: - Árni Hjartarson og Kristján Sæmundsson 2014. Berggrunnskort af Íslandi. 1:600 000. Íslenskar orkurannsóknir, Reykjavík. - Árni Hjartarson og Magnús Ólafsson 2005. Hveravellir : könnun og kortlagning háhitasvæðis. Íslenskar orkurannsóknir, Reykjavík - Guðmundur Kjartansson 1965. Jarðfræðikort af Íslandi (1:250 000), blað 5, Mið-Ísland. Menningarsjóður, Reykjavík. - Haukur Jóhannesson, Sveinn P. Jakobsson og Kristján Sæmundsson 1990. Jarðfræðikort af Íslandi, blað 6, Miðsuðurland (3. útgáfa). Náttúrufræðistofnun Íslands, Náttúrufræðistofnun, Reykjavík. - Haukur Jóhannesson 1994. Jarðfræðikort af Íslandi, blað 2. Miðvesturland (1:250 000), önnur útgáfa. Náttúrufræðistofnun Íslands og Náttúrufræðistofnun, Reykjavík. - Haukur Jóhannesson og Kristján Sæmundsson 1998. Jarðfræðikort af Íslandi, 1:500 000. Berggrunnur (2. útgáfa). Náttúrufræðistofnun Íslands, Reykjavík. - Haukur Jóhannesson og Kristján Sæmundsson 1998. Jarðfræðikort af Íslandi, 1:500 000. Höggun (1. útgáfa). Náttúrufræðistofnun Íslands, Reykjavík. - Haukur Jóhannesson og Kristján Sæmundsson 2009. Jarðfræðikort af Íslandi. 1:600 000. Höggun. Náttúrufræðistofnun Íslands, Reykjavík. - Hjalti Franzson. Geological Map of Vörðufell and the Surrounding Area. 1:20 000. ÍSOR. Óbirt kort - Ingibjörg Kaldal 2005. Umhverfi og orkuöflun : jöklalandslag : Þórisjökull og suðurhluti Langjökuls, 1:120 000. Staða gagnasafns í október 2005. Íslenskra orkurannsókna ÍSOR-05180. - Ingibjörg Kaldal og Skúli Víkingsson 2009. Umhverfi og orkuöflun kort 1 : jöklalandslag : norðurhluti Langjökuls og Kjölur. Íslenskra orkurannsókna ÍSOR-2009/062. - Kristján Sæmundsson 1995. Hengill. Jarðfræðikort (berggrunnur). 1:50 000. Orkustofnun, Hitaveita Reykjavíkur, Náttúrufræðistofnun. Reykjavík. - Kristján Sæmundsson, Jónas Þór Ingólfsson og Guðjón Eyjólfur Ólafsson 2014. Stóra-Laxá – Illagil. Berggrunnskort 1.10.000. Unnið fyrir Eflu. ÍSOR 2014/019 Kristján Sæmundsson og Ingibjörg Kaldal 2004. Vatnssvið Þinvallarvatns - jarðfræðikort. ÍSOR. Óbirt kort - Náttúrufræðistofnun Íslands 2017. NÍ-Kortasjá ‚Sérstök vernd náttúrufyrirbæra‘. Eldhraun á nútíma. 1. útg. mars 2017 - Sveinn P. Jakobsson 2019. Geological map of the western volcanic zone, Iceland.
The Yukon Geological Survey (YGS) has compiled over 195 surficial geology maps into a standardized GIS format, providing approximately 80% coverage of the territory. The maps range in scales from 1:250,000 to 1:10,000 with spatial overlap between scales. The original maps were produced by various agencies, including the Geological Survey of Canada, YGS, Yukon Government, universities, and the City of Whitehorse. All original feature descriptions have been preserved and also converted to standardized values using the Yukon terrain classification system. The compilation includes 4 GIS datasets and supporting documents available for download via [YGS integrated data system](https://data.geology.gov.yk.ca/Compilation/33) (YGSIDS) or GeoYukon. A .lyr file is [provided](https://data.geology.gov.yk.ca/Compilation/33) to symbolize feature classes and differentiate overlapping maps at different scales. Additionally, there is a surficial geology map index. The polygon attributes captured include surficial material, texture, age, surface expression, and geomorphological processes. Line features include geological contacts, glacial limits, glacial landforms (cirques, arêtes, eskers, meltwater channels, moraines), and non-glacial landforms (faults, lineaments, landslides, escarpments). Point features include field station, fossil and sample locations, glacial landforms (erratics, kames, kettles, drumlins, flutings), permafrost features (pingos, palsas, patterned ground, thermokarst depressions), and other non-glacial landforms (landslides, tors). The map index provides information on each map publication such as author, map title, map scale, publisher. These data are valuable for land-use applications in the territory, including: mineral and placer exploration, geotechnical engineering, infrastructure planning, granular resource assessments, permafrost modeling, agricultural assessments, forest management, and biophysical or ecological land classification. Distributed from [GeoYukon](https://yukon.ca/geoyukon) by the [Government of Yukon](https://yukon.ca/maps) . Discover more digital map data and interactive maps from Yukon's digital map data collection. For more information: [geomatics.help@yukon.ca](mailto:geomatics.help@yukon.ca)
Historical Ambient Air Quality Validated - Estevan
The Ministry of Environment operates a network of continuous ambient air monitoring stations to measure the concentration of air pollutants across Saskatchewan. This is considered validated data that has undergone quality control and quality assurance. For best results download the entire dataset without filtering as a CSV. ‘Date and time’ as displayed is your local time. However, downloaded data is in UTC for ‘Date and time’. Any values of -9999, -999, or 9980 are invalid data. Download zip file. The Ministry of Environment operates a network of continuous ambient air monitoring stations. These stations are part of the National Air Pollution Surveillance (NAPS) network. Continuous ambient air monitoring stations measure the concentration of air pollutants across Saskatchewan. The data is used to: • track and report on progress for achieving air quality objectives • measure representative pollutant concentrations and determine long-term trends and • provide air quality information to the public Air pollutants typically come from various industrial activity and natural sources, such as mining, oil and gas, agriculture, forest fires, electrical generation, and the transportation sector. Disclaimer: Hourly data from the Saskatchewan Ministry of Environment monitoring stations is validated and updated every quarter. This is the most up-to-date and accurate information available. A final annual review occurs in spring where data are subject to change. For more information please visit the ministry's Air Quality Monitoring page or contact the Ministry of Environment Inquiry Centre: centre.inquiry@gov.sk.ca 1-800-567-4224
By_sea_regions/Baltic_Sea/Water_body_dissolved_oxygen_concentration.4Danl.nc*Water body dissolved oxygen concentration_L1
Íslenskt fitjuskrá '600 Jarðmyndun og landmótun' sem tengjast staðlinum ÍST 120 (PDF)
Original metadata (https://open.yukon.ca)
original metadata (http://geohub.saskatchewan.ca)
Swedish Meteorological and Hydrological Institute
Aarhus University, Department of Bioscience, Marine Ecology Roskilde
Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research
All-Russia Research Institute of Hydrometeorological Information, World Data Centre, National Oceanographic Data Centre (NODC)
Arctic and Antarctic Research Institute, Roshydromet (Saint-Petersburg)
Baltic Research Institute of Fishery of Latvia
Blekingekusten Coalition of Water Conservation
Carl von Ossietzky University of Oldenburg, Institute for Chemistry and Biology of the Marine Environment
Chief Inspectorate for Environmental Protection
Committee of North Eastern Halsingland Coordinated Recipient Monitoring
County Administration Board of Norrbottens lan
County Administration Board of Stockholm lan
County Administration Board of Uppsala lan
County Administration Board of Vasternorrlands lan
County Administrative Board of Vasterbotten
DTU Aqua, National Institute of Aquatic Resources, Technical University of Denmark
Department of Marine Systems at Tallinn University of Technology
Federal Maritime and Hydrographic Agency
Federal Maritime and Hydrographic Agency, Dept. Oceanography
Helmholtz Centre for Ocean Research Kiel
Institute of Meteorology and Water Management National Research Institute, Poland
Krondshtadt Hydrometeorological Observatory, North-West HMS
Leibniz Institute for Baltic Sea Research Warnemünde
Lithuanian Hydrometeorological Service under the Ministry of Environment
Ljusnan-Voxnans Water Conservation Association
Ministry of Environmental Protection and Regional Development
Motala strom Coalition of Water Conservation
North-Western Regional Administration of Hydrometeorology of Roshydromet
Odessa Branch of State Oceanographic Institute
Royal Netherlands Institute for Sea Research
Russian State Hydrometeorological University, St-Petersburg
South Coast Water Conservation Association
State Agency for Environment, Nature and Geology, Mecklenburg-Vorpommern
State Agency for Nature and Environment of Schleswig Holstein
State Office for Agriculture, Environment and Rural Areas of Schleswig Holstein
The Swedish Agency for Marine and Water Management
Ume- and Vindelälven Coalition of Water Conservation
Vastra Hanobukten Coalition of Water Conservation
Náttúrufræðistofnun – Natural Science Institute of Iceland
Government of Yukon; Government of Yukon; Geomatics Yukon
Government of Saskatchewan; Government of Saskatchewan; Air Quality, Saskatchewan Ministry of Environment