40 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Fortress Double Door Tiang Pumpung Kepungut Musi Rawas.

Results:

• 11. norsem_begga

  and calculated travel time differences for pairs of closely spaced earthquakes observed at a series of recording stations. Each earthquake is paired with several other earthquakes and the best fitting distances between them as a group are determined. Methods based on this kind of minimization are called double-difference (DD) earthquake location algorithms /media/norsem/norsem_begga.pdf

• 12. norsem_gunnar

  Iceland Seismic Zone. It was implemented in connection with the European REAKT project and lead by Kristin Vogfjörð. We use cross-correlation and double difference methods from Ragnar Slunga. We correlate new single automatic located events with waveforms of events from a high-resolution library (catalog) of active mapped faults in the area and also from a library of well located single events /media/norsem/norsem_gunnar.pdf

• 13. norsem_ingi

  have started applying double-difference method of Waldhauser and Ellsworth (2000), to improve earthquake location accuracy in the area. On spatial resolution scale on the order of the size of the Southern Iceland Lowland (~70 km), we have been able to measure velocity ratios at ~0.04–0.1% significance (1 σ) with the uncorrected SIL catalog data. Preliminary results can be interpreted /media/norsem/norsem_ingi.pdf

• 14. Factsheet_Bardarbunga_20141124

  There is a double pulse cycle, or fluctuation, one takes hours and the other takes between 10 and 20 seconds.  Seismic activity in Bardarbunga continues to be strong. The biggest earthquakes that was detected since noon on Friday, were of magnitude M5,1 on Sunday, 23. November at 09:22 and this morning, 24. November, at 09:03 of magnitude M5,4. In total 36 earthquakes bigger then M4,0 were /media/jar/Factsheet_Bardarbunga_20141124.pdf

• 15. NONAM_1st_workshop_summary_v3

  stages of adaptation policy development (in an adaptive management setting) – the questions are listed below in the textbox and in Annex 1.; 2. to produce a flowchart of an adaptation plan (outline) based on the ideas of adaptive management (as synthesized in the ‘double loop model’) – see figure 1. The first session started with an introduction to the sector / case considered, followed /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 16. 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

• 17. The weather in Iceland 2011

  absolute minimum in Iceland. Precipitation The precipitation was above normal. In Reykjavík it exceeded the 1961 to 1990 mean by about 13%. April was the wettest with more than the double normal amount. June and August were the driest. At Akureyri in the north the precipitation was about 30% above the mean. In the east the exceedance was even larger, up to 45% at Dalatangi, but not an absolute /weather/articles/nr/2439

• 18. ved-eng-2011

  in Iceland. The minimum temperature was -27.8 degrees at Upptyppingar in the northeastern inland on 8 December, close to the average annual absolute minimum in Iceland. Precipitation The precipitation was above normal. In Reykjavík it exceeded the 1961 to 1990 mean by about 13%. April was the wettest with more than the double normal amount. June and August were the driest. At Akureyri /media/vedurstofan/utgafa/skylduskil/ved-eng-2011.pdf

• 19. Group4-Pres

  } } } Single Loop Double Loop Triple Loop /media/loftslag/Group4-Pres.pdf

• 20. The weather in Iceland 2010

  The precipitation in Akureyri was unusually unevenly distributed during the year. There was almost no precipitation in January and June, but double the normal in February. There was also much precipitation in Akureyri in August and November. Largest 24-hr precipitation The largest 24-hr precipitation total was measured at Kvísker in the southeast on September 26, 179.4 mm. The largest 1-hour value /about-imo/news/2011/nr/2112