WMS A compliant implementation of WMS plus most of the SLD extension (dynamic styling). Can also generate PDF, SVG, KML, GeoRSS WFS WMS GEOSERVER Ragnar Heiðar Þrastarson Icelandic Met Office Work

Reykjavík Iceland fyrirspurnir@vedur.is NONE NONE text/xml image/png application/atom+xml application/json;type=utfgrid application/pdf application/rss+xml application/vnd.google-earth.kml+xml application/vnd.google-earth.kml+xml;mode=networklink application/vnd.google-earth.kmz image/geotiff image/geotiff8 image/gif image/jpeg image/png; mode=8bit image/svg+xml image/tiff image/tiff8 image/vnd.jpeg-png image/vnd.jpeg-png8 text/html; subtype=openlayers text/html; subtype=openlayers2 text/html; subtype=openlayers3 text/plain application/vnd.ogc.gml text/xml application/vnd.ogc.gml/3.1.1 text/xml; subtype=gml/3.1.1 text/html application/json XML INIMAGE BLANK JSON A compliant implementation of WMS plus most of the SLD extension (dynamic styling). Can also generate PDF, SVG, KML, GeoRSS EPSG:4326 EPSG:3857 EPSG:3057 EPSG:900913 CRS:84 -29.128833642016 -9.51699342356888 62.18165769647678 67.24187007298997 glaciology:glacier_outline_group A single layer for all the glacier outlines available. For details, check description for each layer. EPSG:4326 -23.9 -13.7 63.4 66.5 geology:HEK_1980_10kg_m2_depositprob Probability (%) to exceed 10 kg/m2 of tephra ground loading for a 1980-like eruption at Hekla using the VOL-CALPUFF model (EPOS service). HEK_1980_10kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -26.02326845113788 -9.961000432726575 62.56528332346246 67.24187007298997 geology:HEK_1980_1kg_m2_depositprob Probability (%) to exceed 1 kg/m2 of tephra ground loading for a 1980-like eruption at Hekla using the VOL-CALPUFF model (EPOS service). HEK_1980_1kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -26.02326845113788 -9.961000432726575 62.56528332346246 67.24187007298997 geology:HEK_1980_3kg_m2_depositprob Probability (%) to exceed 3 kg/m2 of tephra ground loading for a 1980-like eruption at Hekla using the VOL-CALPUFF model (EPOS service). HEK_1980_3kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -26.02326845113788 -9.961000432726575 62.56528332346246 67.24187007298997 meteorology:IcelandicMetOffice_CAP_areas Weather forecast areas on land of The Icelandic Met Office. These areas are also used when CAP weather warnings are issued. features IcelandicMetOffice_CAP_areas EPSG:4326 CRS:84 -24.579999999999927 -13.439999999999927 63.37000000000006 66.57000000000006 geology:KAT_1918_10kg_m2_depositprob Probability (%) to exceed 10 kg/m2 of tephra ground loading for a 1918-like eruption at Katla using the VOL-CALPUFF model (EPOS service). KAT_1918_10kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -25.34455125065649 -9.51699342356888 62.18165769647678 66.87939308836444 geology:KAT_1918_1kg_m2_depositprob Probability (%) to exceed 1 kg/m2 of tephra ground loading for a 1918-like eruption at Katla using the VOL-CALPUFF model (EPOS service). KAT_1918_1kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -25.34455125065649 -9.51699342356888 62.18165769647678 66.87939308836444 geology:KAT_1918_3kg_m2_depositprob Probability (%) to exceed 3 kg/m2 of tephra ground loading for a 1918-like eruption at Katla using the VOL-CALPUFF model KAT_1918_3kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -25.34455125065649 -9.51699342356888 62.18165769647678 66.87939308836444 geology:ORA_1362_100kg_m2_depositprob Probability (%) to exceed 100 kg/m2 of tephra ground loading for a 1362-like eruption at Öræfajökull using the VOL-CALPUFF model (EPOS service). ORA_1362_100kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -26.02326845113788 -9.961000432726575 62.56528332346246 67.24187007298997 geology:ORA_1362_1kg_m2_depositprob Probability (%) to exceed 1 kg/m2 of tephra ground loading for a 1362-like eruption at Öræfajökull using the VOL-CALPUFF model (EPOS service). ORA_1362_1kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -26.02326845113788 -9.961000432726575 62.56528332346246 67.24187007298997 geology:ORA_1362_3kg_m2_depositprob Probability (%) to exceed 3 kg/m2 of tephra ground loading for a 1362-like eruption at Öræfajökull using the VOL-CALPUFF model (EPOS service). ORA_1362_3kg_m2_depositprob WCS GeoTIFF EPSG:3057 CRS:84 -26.02326845113788 -9.961000432726575 62.56528332346246 67.24187007298997 geography:Reykjanes_hillshade Hillshade around the eruption area near Svartsengi and Grindavík hillshade_5m_fag_sva_v20250807 WCS GeoTIFF EPSG:3057 CRS:84 -22.6 -22.11 63.7 64.1 glaciology:glaciercauldronv Known glacier cauldrons. Based on observations by the Institute of Earth Sciences at The University of Iceland and The Icelandic Met Office. glaciercauldronv features EPSG:4326 CRS:84 -22.0 -15.5 62.4 65.9 glaciology:glacieroutline_ams The US Army Map Service (AMS) created topographic maps of Iceland at a scale of 1:50,000. These were based on aerial photographs taken in 1945 and 1946 and had contour lines drawn at 20 m intervals. During recent years, the original AMS aerial photographs, that are now stored at the National Land Survey of Iceland (NLS), have been scanned, georectified and processed to create DEMs and orthoimages utilizing the 60% acquisition overlap (Magnússon et al., 2016; Belart et al., 2019). These DEMs have been used to digitize glacier outlines more accurately than those displayed on the original topographic maps (see for example Belart et al., 2019, and Andreassen et al., 2020). In Table 2, a distinction is made between 1945/1946 glacier outlines digitized from the original maps and outlines derived more recently from the scanned aerial photographs. Two-thirds of the 1945/1946 outline for Vatnajökull (from Skeiðarárjökull to the west and north to Lambatungnajökull, except Öræfajökull for which the aerial images have been scanned and re-processed) is based on the AMS maps with some corrections; by georeferencing the scanned maps individually, and fitting each map segment to the surrounding valley walls, using lidar DEMs as reference topography (for more details see Pálsson et al., 2012, and Hannesdóttir et al., 2015b). Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacieroutline_ams EPSG:4326 CRS:84 -21.1 -14.7 63.4 65.8 glaciology:glacieroutline_ca_2000 Multiple imagery sources were used to delineate the glacier margin for ∼2000. These included orthorectified aerial images from the company Loftmyndir ehf. (GSD of 1×1 m), satellite images from both Landsat 7 (GSD of 15×15 m) and SPOT-5 (GSD of 2.5×2.5 m and 5×5 m) and georeferenced oblique images taken from an airplane. The year of acquisition varies between sources from 1998 to 2004. The orthoimages (airborne and spaceborne) also have different GSD. For information relating to each glacier or glacierized area see Table 2. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacieroutline_ca_2000 EPSG:4326 CRS:84 -23.3 -13.8 63.4 66.3 glaciology:glacieroutline_ipy During 2008–2012, starting during the International Polar Year, accurate and detailed DEMs of the glaciers in Iceland were produced with airborne lidar. The lidar DEMs have a GSD of 5×5 m and hillshades were created from them for delineation of glacier outlines (Jóhannesson et al., 2011, 2013). More than 90% of the glaciers were surveyed in this effort, including Vatnajökull, Hofsjökull, Mýrdalsjökull, Drangajökull, Eyjafjallajökull and several smaller glaciers. Approximately 70% of Langjökull was surveyed by the Scott Polar Research Institute (SPRI) in late summer 2007, and almost the whole glacier again in 2013, including Þórisjökull (Pope et al., 2013). Hofsjökull was also resurveyed by lidar in 2013. The lidar mapping generally includes a 500–1000 m wide ice-free buffer zone around the ice margins which contains many glacial geomorphological features, and therefore the new DEMs have proved to be useful in geological investigations of proglacial areas. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacieroutline_ipy EPSG:4326 CRS:84 -21.1 -14.7 63.4 65.1 glaciology:glacieroutline_lia Outlines based on the mapping of glacier morains and other glacio-geomorphological landforms. Information about the maximum LIA glacier extent has also been obtained from historical documents, from travellers and local farmers and other inhabitants in areas near the glaciers, photograps, maps and other available sources. These outlines have been provided by many research groups. features glacieroutline_lia EPSG:4326 CRS:84 -23.5 -13.7 63.4 66.5 glaciology:glacieroutline_lm_2014 Glacier outlines of 2014 based on aerial images from Loftmyndir ehf. and Landsat 8 satellite images are part of the glacier inventory presented here and submitted to GLIMS. Many of the smaller glaciers, particularly on Tröllaskagi, were snow-covered in late summer in 2014, and the glacier margin is hard to delineate in some areas for this reason. The outlines from 2014 are not shown on the maps in this paper for clarity because they are hard to distinguish from the outlines from ∼2010 and 2019. Data from 2014 are, however, included in the time series of glacier area shown in the Results section. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacieroutline_lm_2014 EPSG:4326 CRS:84 -22.6 -13.8 63.4 66.4 glaciology:glacieroutline_misc_1970s Glacier outlines for the decade 1970–1980 have been digitized from early Landsat 1 (previously known as ERTS-1) images acquired in the summer of 1973, with a Ground Sampling Distance (GSD) 60×60 m and aerial images from the National Land Survey of Iceland from the 1970s (with a GSD of 0.7×0.7 m). The aerial images have been processed for creation of orthoimages and DEMs, and they were used to create additional glacier outlines in areas not covered by the 1973 Landsat imagery, and improve outlines in a few areas. This includes glacier margins for the smaller ice caps and glaciers (see Table 2 for details). The outlines of a few glaciers are based on declassified Hexagon KH9 satellite images aquired in 1980 (Belart et al., 2019, 2020). Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacieroutline_misc_1970s EPSG:4326 CRS:84 -23.9 -14.7 63.4 65.1 glaciology:glacieroutline_sent2_2017 During the summer and autumn of 2017, Sentinel-2 satellites acquired images (GSD of 10×10 m) of all the major glaciers in Iceland. To fill in the missing patches a mix of Landsat 8 and orthorectified aerial images from the company Loftmyndir ehf. were used. Kääb et al. (2016) noted lateral offsets in the geolocation of Sentinel-2 data. We found this offset to be quite small for the Icelandic glaciers and it is neglected here for simplicity since it does not affect calculations of glacier area. The outlines from 2017 are not shown on the maps in this paper for clarity because they are hard to distinguish from the outlines from ∼2010 and 2019. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacieroutline_sent2_2017 EPSG:4326 CRS:84 -23.3 -13.8 63.4 66.4 glaciology:glacieroutline_sent2_2019 During the summer and autumn of 2019, Sentinel-2 satellites acquired images (GSD of 10×10 m) of all the major glaciers in Iceland. The warm spring and summer of 2019 enhanced melting of seasonal snow, exposing glacier margins, and enabled the delineation of the actual ice margin for the first time in several years at many locations. Orthorectified aerial images from the company Loftmyndir ehf. were also used in some areas. The smallest glaciers (< 3 km2 , shown in blue in Figure 1) and the groups listed in Table 1 were not digitized from those images and changes in their extent were assumed to be negligible compared with 2017. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacieroutline_sent2_2019 EPSG:4326 CRS:84 -23.3 -13.8 63.4 66.4 glaciology:glacieroutline_sent2_2021 Outlines digitized from orthorectified Sentinel-2 satellite images and Pleiades imagery. Orthorectified aerial images from Loftmyndir ehf. were also used in a few places. features glacieroutline_sent2_2021 EPSG:4326 CRS:84 -24.7 -13.2 63.1 66.6 glaciology:glacieroutline_sent2_2023 Outlines digitized from orthorectified Sentinel-2 satellite images and Pleiades imagery. Orthorectified aerial images from Loftmyndir ehf. were also used in a few places. features glacieroutline_sent2_2023 EPSG:4326 CRS:84 -24.7 -13.2 63.1 66.6 glaciology:glacieroutline_sent2_2025 Outlines digitized from orthorectified Sentinel-2 satellite images and Pleiades imagery. Orthorectified aerial images from Loftmyndir ehf. were also used in a few places. features glacieroutline_sent2_2025 EPSG:4326 CRS:84 -24.7 -13.2 63.1 66.6 glaciology:glacierphotolocv Location of photos (camera location) avilable in the Icelandic glacier web portal. features glacierphotolocv EPSG:4326 CRS:84 -23.8 -14.8 63.4 66.2 glaciology:glacierpolygon_ams The US Army Map Service (AMS) created topographic maps of Iceland at a scale of 1:50,000. These were based on aerial photographs taken in 1945 and 1946 and had contour lines drawn at 20 m intervals. During recent years, the original AMS aerial photographs, that are now stored at the National Land Survey of Iceland (NLS), have been scanned, georectified and processed to create DEMs and orthoimages utilizing the 60% acquisition overlap (Magnússon et al., 2016; Belart et al., 2019). These DEMs have been used to digitize glacier outlines more accurately than those displayed on the original topographic maps (see for example Belart et al., 2019, and Andreassen et al., 2020). In Table 2, a distinction is made between 1945/1946 glacier outlines digitized from the original maps and outlines derived more recently from the scanned aerial photographs. Two-thirds of the 1945/1946 outline for Vatnajökull (from Skeiðarárjökull to the west and north to Lambatungnajökull, except Öræfajökull for which the aerial images have been scanned and re-processed) is based on the AMS maps with some corrections; by georeferencing the scanned maps individually, and fitting each map segment to the surrounding valley walls, using lidar DEMs as reference topography (for more details see Pálsson et al., 2012, and Hannesdóttir et al., 2015b). Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacierpolygon_ams EPSG:4326 CRS:84 -23.9 -14.7 63.4 66.3 glaciology:glacierpolygon_ca_2000 Multiple imagery sources were used to delineate the glacier margin for ∼2000. These included orthorectified aerial images from the company Loftmyndir ehf. (GSD of 1×1 m), satellite images from both Landsat 7 (GSD of 15×15 m) and SPOT-5 (GSD of 2.5×2.5 m and 5×5 m) and georeferenced oblique images taken from an airplane. The year of acquisition varies between sources from 1998 to 2004. The orthoimages (airborne and spaceborne) also have different GSD. For information relating to each glacier or glacierized area see Table 2. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacierpolygon_ca_2000 EPSG:4326 CRS:84 -23.9 -13.7 63.4 66.4 glaciology:glacierpolygon_ipy During 2008–2012, starting during the International Polar Year, accurate and detailed DEMs of the glaciers in Iceland were produced with airborne lidar. The lidar DEMs have a GSD of 5×5 m and hillshades were created from them for delineation of glacier outlines (Jóhannesson et al., 2011, 2013). More than 90% of the glaciers were surveyed in this effort, including Vatnajökull, Hofsjökull, Mýrdalsjökull, Drangajökull, Eyjafjallajökull and several smaller glaciers. Approximately 70% of Langjökull was surveyed by the Scott Polar Research Institute (SPRI) in late summer 2007, and almost the whole glacier again in 2013, including Þórisjökull (Pope et al., 2013). Hofsjökull was also resurveyed by lidar in 2013. The lidar mapping generally includes a 500–1000 m wide ice-free buffer zone around the ice margins which contains many glacial geomorphological features, and therefore the new DEMs have proved to be useful in geological investigations of proglacial areas. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacierpolygon_ipy EPSG:4326 CRS:84 -23.9 -14.7 63.4 65.1 glaciology:glacierpolygon_lia Outlines based on the mapping of glacier morains and other glacio-geomorphological landforms. Information about the maximum LIA glacier extent has also been obtained from historical documents, from travellers and local farmers and other inhabitants in areas near the glaciers, photograps, maps and other available sources. These outlines have been provided by many research groups. features glacierpolygon_lia EPSG:4326 CRS:84 -23.9 -13.7 63.4 66.5 glaciology:glacierpolygon_lm_2014 Glacier outlines of 2014 based on aerial images from Loftmyndir ehf. and Landsat 8 satellite images are part of the glacier inventory presented here and submitted to GLIMS. Many of the smaller glaciers, particularly on Tröllaskagi, were snow-covered in late summer in 2014, and the glacier margin is hard to delineate in some areas for this reason. The outlines from 2014 are not shown on the maps in this paper for clarity because they are hard to distinguish from the outlines from ∼2010 and 2019. Data from 2014 are, however, included in the time series of glacier area shown in the Results section. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacierpolygon_lm_2014 EPSG:4326 CRS:84 -23.3 -13.7 63.4 66.4 glaciology:glacierpolygon_misc_1970s Glacier outlines for the decade 1970–1980 have been digitized from early Landsat 1 (previously known as ERTS-1) images acquired in the summer of 1973, with a Ground Sampling Distance (GSD) 60×60 m and aerial images from the National Land Survey of Iceland from the 1970s (with a GSD of 0.7×0.7 m). The aerial images have been processed for creation of orthoimages and DEMs, and they were used to create additional glacier outlines in areas not covered by the 1973 Landsat imagery, and improve outlines in a few areas. This includes glacier margins for the smaller ice caps and glaciers (see Table 2 for details). The outlines of a few glaciers are based on declassified Hexagon KH9 satellite images aquired in 1980 (Belart et al., 2019, 2020). Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacierpolygon_misc_1970s EPSG:4326 CRS:84 -23.9 -14.7 63.4 66.3 glaciology:glacierpolygon_sent2_2017 During the summer and autumn of 2017, Sentinel-2 satellites acquired images (GSD of 10×10 m) of all the major glaciers in Iceland. To fill in the missing patches a mix of Landsat 8 and orthorectified aerial images from the company Loftmyndir ehf. were used. Kääb et al. (2016) noted lateral offsets in the geolocation of Sentinel-2 data. We found this offset to be quite small for the Icelandic glaciers and it is neglected here for simplicity since it does not affect calculations of glacier area. The outlines from 2017 are not shown on the maps in this paper for clarity because they are hard to distinguish from the outlines from ∼2010 and 2019. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. glacierpolygon_sent2_2017 features EPSG:4326 CRS:84 -23.3 -13.7 63.4 66.4 glaciology:glacierpolygon_sent2_2019 During the summer and autumn of 2019, Sentinel-2 satellites acquired images (GSD of 10×10 m) of all the major glaciers in Iceland. The warm spring and summer of 2019 enhanced melting of seasonal snow, exposing glacier margins, and enabled the delineation of the actual ice margin for the first time in several years at many locations. Orthorectified aerial images from the company Loftmyndir ehf. were also used in some areas. The smallest glaciers (< 3 km2 , shown in blue in Figure 1) and the groups listed in Table 1 were not digitized from those images and changes in their extent were assumed to be negligible compared with 2017. Taken from: Hannesdóttir, Hrafnhildur, et al. "A national glacier inventory and variations in glacier extent in Iceland from the Little Ice Age maximum to 2019." JOKULL 70 (2020): 1-34. features glacierpolygon_sent2_2019 EPSG:4326 CRS:84 -23.9 -13.7 63.4 66.4 glaciology:glacierpolygon_sent2_2021 Outlines digitized from orthorectified Sentinel-2 satellite images and Pleiades imagery. Orthorectified aerial images from Loftmyndir ehf. were also used in a few places. features glacierpolygon_sent2_2021 EPSG:4326 CRS:84 -24.7 -13.2 63.1 66.6 glaciology:glacierpolygon_sent2_2023 Outlines digitized from orthorectified Sentinel-2 satellite images and Pleiades imagery. Orthorectified aerial images from Loftmyndir ehf. were also used in a few places. features glacierpolygon_sent2_2023 EPSG:4326 CRS:84 -24.7 -13.2 63.1 66.6 glaciology:glacierpolygon_sent2_2025 Outlines digitized from orthorectified Sentinel-2 satellite images and Pleiades imagery. Orthorectified aerial images from Loftmyndir ehf. were also used in a few places. features glacierpolygon_sent2_2025 EPSG:4326 CRS:84 -24.7 -13.2 63.1 66.6 glaciology:glacierv A point for each glacier in Iceland. features glacierv EPSG:4326 CRS:84 -23.8 -14.0 63.5 66.2 geology:lava_model_fagradalsfjall_large_weighted_epsg3857 lava_model_fagradalsfjall_large_weighted_epsg3857 WCS GeoTIFF EPSG:3857 CRS:84 -22.8131977710896 -20.525481242209587 63.70626214475532 64.408100601944 geology:lava_model_fagradalsfjall_med_weighted_epsg3857 lava_model_fagradalsfjall_med_weighted_epsg3857 WCS GeoTIFF EPSG:3857 CRS:84 -22.8131977710896 -20.525481242209587 63.70626214475532 64.408100601944 geology:lava_model_svartsengi_med_weighted_epsg3857 lava_model_svartsengi_med_weighted_epsg3857 WCS GeoTIFF EPSG:3857 CRS:84 -22.8131977710896 -20.525481242209587 63.70626214475532 64.408100601944 geology:lava_model_svartsengi_small_weighted_epsg3857 lava_model_svartsengi_small_weighted_epsg3857 WCS GeoTIFF EPSG:3857 CRS:84 -22.8131977710896 -20.525481242209587 63.70626214475532 64.408100601944 glaciology:stakembvv features stakembvv EPSG:4326 CRS:84 -20.6 -18.4 63.4 65.1 glaciology:stakev features stakev EPSG:4326 CRS:84 -20.6 -15.4 63.4 65.1 glaciology:terminusobslocvv terminusobslocvv features EPSG:4326 CRS:84 -23.9 -15.2 63.4 66.3 tos:v_stations_wgs84 Survey stations and observation locations of The Icelandic Met Office. This includes stations used for observing and monitoring weather, geophysical and hydrological parameters. features v_stations_wgs84 EPSG:4326 CRS:84 -29.128833642016 -13.517 63.0016553077381 66.54378