88 results were found for WA 0821 7001 0763 (FORTRESS) pintu baja single Kaliwungu Kabupaten Kudus Jawa Tengah.

Results:

• 21. Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull

  indicates that about 60 million cubic metres of material are in motion. It is possible that the entire mass may be released as a single rockslide, it is also possible that the material may be released as several smaller rockslides. The age of these fractures is not well known. They are not visible on aerial imagery from the year 2003 but they are evident in an elevation model from 2011, indicating /about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull

• 22. Station forecasts, text forecasts or observations

  but in most cases removing the Modernus measuring code from a single web-page is a simple task. As for now, our frames are large and constitute the main topic of the relevant page. In such circumstances, each visit counts. Later, the Icelandic Meteorological Office will offer small iframes which will not contain a Modernus measuring code and therefore not conflict in any way with Coordinated /about-imo/the-web/iframes/wst-txt-obs/

• 23. Bárðarbunga - decay of seismic activity

  that the plot is logarithmic, one tick on the y-scale corresponds to a factor of 10. Further, the general trend of the curve should be interpreted, and not single points, as they might be outliers. In both clusters, the moment release was largest shortly before the onset of the fissure eruption in Holuhraun and has decayed ever since. Seismic activity on the caldera rim has constantly decreased /earthquakes-and-volcanism/articles/nr/3083

• 24. Eyjafjallajokull_status_2010-04-28_IES_IMO

  is similar to the five preceding days. Other remarks: Gas emissions from meltwater leaving Gígjökull represents a localised hazard, especially within the moraines of the glacier. The main gasses are CO2 and probably SO2. These gases are heavier than air, and could linger in front of Gígjökull if light winds prevail. Despite a single earthquake occurring, there are no signs of untoward changes /media/jar/Eyjafjallajokull_status_2010-04-28_IES_IMO.pdf

• 25. Milly_etal-2008-Stationarity-dead-Science

  6University of Washington, Seattle, WA 98195, USA. 7NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA. *Author for correspondence. E-mail: cmilly@usgs.gov. An uncertain future challenges water planners. Published by AAAS on July 12, 201 1 www.sciencemag.or g Downloaded from 1 FEBRUARY 2008 VOL 319 SCIENCE www.sciencemag.org574 POLICYFORUM combined with opera- tions /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 26. Avalanche danger scale

  / snowboarders etc. without good spacing (or without intervals); snowmachine; explosives; single hiker/climber The table and icons above are from EAWS Selected areas Maps are presented for three selected areas: Northern Westfjords from southern Dýrafjörður north to Ísafjarðardjúp and to the mountains east of Álftafjörður. Northern Tröllaskagi marked by the mountains west of Siglufjörður, towards /avalanches/articles/nr/2619

• 27. bb100days_ens

  that a tectonic earthquake like the 1912 earthquake in the eastern South Icelandic Seismic Zone or 1963 in Skagafjörður (both were around magnitude 7) can easily outnumber the recent activity around Bárðarbunga in just one event, by means of moment release. The cumulative moment release during the migration of the dyke intrusion between 16 August and 1 September corresponds to a single /media/jar/bb100days_ens.pdf

• 28. Eyjafjallajokull_SK_20101214_1

  height information Plume height estimation is currently the most important real- time input data into dispersion models. Primary instrument is a single C-band Doppler weather radar located in Keflavik, surveillance flights and pilot reports (PiReps), and other methods include theodolite estimation. Web-cams Satellite images Some difficulties Inconvenient positioning of radar. Cloudy conditions /media/vedurstofan/myndasafn/Eyjafjallajokull_SK_20101214_1.pdf

• 29. Notes on the 2010 eruptions

  trace the timing of a single flood event from Gígjökull lagoon early this morning, to the new bridge across Markarfljót river at noon, and to the old bridge in the late afternoon. 15.04.2010 Sampling of ash is encouraged, instructions provided (pdf), both for the public and weather observers around the country. IMO‘s web-site now provides a fill-in-form for observations of ashfall and other related /earthquakes-and-volcanism/articles/nr/2467

• 30. ces-glacier-scaling-memo2009-01

  in this figure. ume v = csg rather than area s, in case the distribution function is approximated by a continuous differentiable function. If the watershed contains both ice caps and valley glaciers, it is possible to use two area distribution curves, one for ice caps and another for valley glaciers. It is also possible to use a single area distribution function in this case and choose a weighted /media/ces/ces-glacier-scaling-memo2009-01.pdf