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  • 1. Glacial outburst flood in Múlakvísl

    measured around 580µS/cm and has increased rapidly the last hour.Conductivity is an indicator for the amount of geothermal meltwater in the river. Prior to glacial river surges in the river Múlakvísl conductivity in the river starts rising. This elevation of conductivity can last several days before an actual river surge starts.The glacial outburst flood can be expected to reach its maximum within a few /about-imo/news/glacial-outburst-flood-in-mulakvisl
  • 2. Glacier-outburst flood from Mýrdalsjökull

    with two gauging stations for the glacier river Múlakvísl. The main indicator, located on the bridge on the main road Þjóðvegur 1, began to show increased conduction early evening on 8th July, around the time of peak in the tremor. The water level reached the bridge around midnight, causing damage to the sensors. Contact to the instruments was lost a few hours later. Another gauging station /about-imo/news/nr/2236
  • 3. Space weather predictions

    is considered the most accurate. It can be used as an indicator of the auroral activity for the next few hours. The horizontal time-axis shows the time of day today (UTC), its total length is 24 hours and the time is marked every 6 hours. The prediction is based on measurements of particle flux from the Sun at the ACE-satellite located in the libration point L1 between the Sun and Earth. The data /weather/articles/nr/2550
  • 4. Group4-Pres

    Institutions, Synthesis from other sources, collaboration) Dynamic LIFE CYCLE COSTING & LIFE CYCLE IMPACT (with layering on climate/socio-econ-tech scenarios) Stakeholder Review Process 3rd Party Review Followed by adaption of plan Non Tech Measures (speed, PR) Indicator Creation (internal) Validation (external higher ministry) Updating Out-turn Check – Update Congruency Check Higher Ministry /media/loftslag/Group4-Pres.pdf
  • 5. A jökulhlaup from Grímsvötn

    change their course it must be kept in mind that the water level measured at a fixed location can only be viewed as an indicator of discharge. More extensive and repeated measurements at several places are therefore needed during jökulhlaups to determine the actual size of the flood. The electric conductivity of the river water has increased considerably (see the lowest of the 3 graphs /about-imo/news/nr/2039
  • 6. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

    people in the U.S. alone take the Myers-Brigg Type Indicator (MBTI®) personality test each year, and it has been translated into more than 30 languages. Despite this, Academics in general and natural scientists in particular have been slow to accept the validity of personality type theory and to recognize the value of personality type training as a tool for enhancing communication. In this paper we /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf
  • 7. Group5-Milestones

    on participating for the duration of the stakeholder process? o What are the key milestones of the process? How the milestone can be defined in the first place? In our case, it is the success of the process of involvement. The difficulty is how to measure milestone. One important indicator might be whether each phase has been accomplished within the time prescribed. If the process /media/loftslag/Group5-Milestones.pdf
  • 8. Flood in Grímsvötn

    3.12. at 15:07The icesheet in Grímsvötn started to subside and the water started to drain out from the lake 10 days ago. IMO‘s GPS instruments show that the icesheet has now sunk over 27 meters. This morning, between 10:15 and 12:20, hydrologists from IMO measured a discharge rate of about 1600 m3/s in Gígjukvísl. The electrical conductivity, which is an indicator of the amount of geothermal /about-imo/news/icesheet-in-grimsvotn-subsiding
  • 9. Hofsjökull ice cap gains mass

    - 10th. Fig. 3 indicates how the stakes greeted the expedition team, indicating that much less melting had occurred than during typical conditions over the past 2 decades. Summer ablation was found to be less than 50% of the 1995 - 2014 average. Fig. 3 (enlarge). Ablation stake (white) near the northern margin of Hofsjökull on October 9th 2015 at a height of 980 m. A yellow indicator gives /about-imo/news/nr/3229
  • 10. Grímsvötn 2010

    be viewed as an indicator of discharge. More extensive and repeated measurements at several places are therefore needed during jökulhlaups to determine the actual size of the flood. The electric conductivity of the river water has increased considerably (see the lowest of the 3 graphs). This indicates that geothermal fluids originating in the volcanic system beneath Grímsvötn have mixed /hydrology/articles/nr/2040

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