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• 41. Gauging stations

  and transmits data to the IMO centre at least once a day. The information mainly concerns water-flow, water-level and ground water, and in some cases other environmental factors are being measured. The network includes about 200 gauging stations. They are to a large extent operated for the Ministry of Industry and the National Energy Authority, or for some of the largest energy firms in the country /hydrology/stations/

• 42. Solar eclipse on 1st August

  In Akureyri the eclipse begins at 08:17 GMT. and ends at 10:14 GMT. At its peak, the eclipse will cover 62% of the sun's diameter. People should avoid looking directly into the sun without using very dark glasses or film. The safest way to watch the eclipse is to let a binocular or monocular project the sun's image onto white cardboard, and then adjust the focus for sharpness. For further /about-imo/news/nr/1363

• 43. Program

  to investigate glacier geomorphic processes Rudolf Sailer, Erik Bollmann, Veronika Ebe, Anna Girstmair, Christoph Klug, Lorenzo Rieg, Maximilian Spross and Johann Stötter, Institute of Geography, University of Innsbruck, Austria. Potentials of ALS in the analysis of geomorphodynamic processes in high alpine regions Coffey 15:00–15:30 Thursday 15:30–17:30 ‒ Lidar measurements from space Beata Csatho /lidar/lidar-2013/program/

• 44. Prohibited area around the Holuhraun lava field

  and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge. Preliminary flood risk assessment Preliminary flood risk assessment for Jökulsá á Fjöllum gives flood travel times in minutes. The assigned locations (dots) are colour coded: Red location (dot) is half an hour from the source, orange is an hour, dark yellow one and a half hours, bright yellow two hours, light green two and a half /hydrology/articles/nr/2963

• 45. Monitoring flow

  floods originating in sub-glacial volcano and geothermal systems, or melt water, heavy rain and ice blockage of river-flow. The development of the network began in 1996, following jökulhlaup in Skeiðará, and has in the last decade been extended to the areas south and north of Vatnajökull, south of Mýrdalsjökull, the South Iceland lowland and to Borgarfjörður. Each monitoring station has /hydrology/flow/

• 46. Measuring glaciers

  released, e.g. by World Glacier Monitoring Service in Zürich and Global Land Ice Measurements from Space (GLIMS) in Flagstaff, Arizona. Bird's eye view Snæfellsjökull, western Iceland, 18 October 2001. At that time, the ice-cap had already been observed to retreat and thin in the preceding years and decades, as confirmed by annual measurements in a single location since 1931. This was further /hydrology/glaciers/

• 47. Ice subsidence above eastern Skaftá cauldron

  This graph shows the ice-surface lowering (subsidence) of the eastern Skaftá ice-cauldron in Vatnajökull ice cap in October 2015. Vertical displacement (m) was monitored by near real time presentation of data from a GPS station, mounted in the middle of the cauldron. The maximum elevation above sea level, top left (hæð), refers to the zero value on the y-axis; while such value top right /hydrology/research/skafta-cauldron/

• 48. Prohibited area around the Holuhraun lava field

  and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge. Preliminary flood risk assessment Preliminary flood risk assessment for Jökulsá á Fjöllum gives flood travel times in minutes. The assigned locations (dots) are colour coded: Red location (dot) is half an hour from the source, orange is an hour, dark yellow one and a half hours, bright yellow two hours, light green two and a half /hydrology/articles/nr/2963/

• 49. Reykholt-abstracts

  in July 2016 on a Delta II rocket from Vandenberg Air Force Base in California. ICESat-2 will carry the Advanced Topographic Laser Altimeter System (ATLAS) and collect data to a latitudinal limit of 88 degrees. In contrast to Geoscience Laser Altimeter System (GLAS) on ICESat, ATLAS employs a 6-beam micro-pulse laser photon-counting approach. It uses a high repetition rate (10 kHz; 70 cm /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 50. Icelandic climate in general

  than its name and location adjacent to the Arctic circle would imply. A branch of the Gulf Stream flows along the southern and the western coast greatly moderating the climate. However, this brings mild Atlantic air in contact with colder Arctic air resulting in a climate that is marked by frequent changes in weather and storminess. Furthermore this leads to more rainfall in the southern and western /climatology/iceland/nr/1268