83 results were found for JZMOR Offers Advanced Solutions to Stop Scam in Its Tracks.

Results:

• 31. norsem_janutyte

  Fault plane solutions of the earthquakes in Nordland, Norway Ilma Janutyte(1), Jan Michalek(2), Conrad Lindholm(1), and Lars Ottemoller(2) (1) NORSAR, Kjeller, Norway, (2) University of Bergen, Bergen, Norway This study is a part of the ongoing NEONOR2 project which is carried out in Nordland, norther Norway. This work aims to define the fault plane solutions (FPS) of the earthquakes /media/norsem/norsem_janutyte.pdf

• 32. vonKorff_etal-2010

  Management: Recent Advances in Theory, Practice and Evaluation Designing Participation Processes for Water Management and Beyond Yorck von Korff 1,2, Patrick d'Aquino 3, Katherine A. Daniell 2,4, and Rianne Bijlsma 5 ABSTRACT. This article addresses the question of how to design participation processes in water management and other fields. Despite a lot of work on participation, and especially its /media/loftslag/vonKorff_etal-2010.pdf

• 33. Articles

  April 2010 at 10:43 which advanced at the speed of 5 km per hour. Related topics UNESCO USGS /hydrology/articles/bigimg/2097

• 34. i-frame services

  The Icelandic Meteorological Office offers a service that allows web-masters to show weather information from IMO on their web-sites without effort. This service is free of charge, using the iframe technique. Two versions of iframes have been developed, one for station forecasts, text forecasts or observations, and another for weather elements (wind, temperature and precipitation forecasts /about-imo/the-web/iframes/

• 35. Update on activity in Eyjafjallajökull 2010

  to the southwest at 15-18 m/s. The plume drifted northwest early this morning, but then turned north-northeast, and its colour is gray or light gray. The number of lightning strikes has decreased. Ash has fallen in the south at Flúðir, Fljótshlíð and Rangárþing ytra. Ash has also fallen with rainfall in the north, in Húsavík and Skagafjörður, right before noon. Heavy rainfall caused swelling /earthquakes-and-volcanism/articles/nr/1884

• 36. Bárðarbunga 2014 - September events

  its way parallel to other flows. Therefore, the combined surface area of the lava field is no less than 46 km2. 29 September 2014 11:30 - from the Scientific Advisory Board Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University of Iceland along with representatives from the Icelandic Civil Protection and the Directorate of Health. From the Scientific /earthquakes-and-volcanism/articles/nr/3001

• 37. Bardarbunga-2014_September-events

  but since 26 September an almost 4 km long trail, about 2 square kilometers, has found its way parallel to other flows. Therefore, the combined surface area of the lava field is no less than 46 km2. 29 September 2014 11:30 - from the Scientific Advisory Board Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University of Iceland along with representatives from /media/jar/Bardarbunga-2014_September-events.pdf

• 38. Bárðarbunga 2014 - September events

  its way parallel to other flows. Therefore, the combined surface area of the lava field is no less than 46 km2. 29 September 2014 11:30 - from the Scientific Advisory Board Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University of Iceland along with representatives from the Icelandic Civil Protection and the Directorate of Health. From the Scientific /earthquakes-and-volcanism/articles/nr/3001/

• 39. NONAM_1st_workshop_summary_v3

  are designed and operated (urban and coastal zone management e.g. planning and disaster prevention & relief and rescue) NONAM intends to enhance the following by means of its networking facilities: • the methodological development regarding adaptation assessment with special reference to (common) needs in Nordic countries • the actual application and testing of these methods in co-operation /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 40. Hare-2011-ParticipatoryModelling

  or system dynamics models, provide bene
  ts which go beyond the production of the model itself. The discussions and negotiations between the groupmembers during themodel building, for example, improve the group’s shared understanding of the management problem and its solutions. As such, participatory modelling can be a tool for supporting the type of social learning currently being promoted for water /media/loftslag/Hare-2011-ParticipatoryModelling.pdf