49 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Rumah Cluster Depan Kokoh Merek Karo Sumatera Utara.

Results:

• 41. Bárðarbunga 2014 - September events

  2 3 1 1 M4.0-4.9 43 7 34 1 1 0 0 0 M>5.0 23 0 23 0 0 0 0 0 HB/HBT: Herðubreið and Herðubreiðartögl TFJ: Tungnafellsjökull Kverkfj.: Kverkfjöll Kistufell: Cluster north of Bárðarbunga that was active during the first days automatic: Automatically detected events in the whole country, number of events outside the Vatnajökull are comparably /earthquakes-and-volcanism/articles/nr/3001

• 42. Bardarbunga-2014_September-events

  - - - - - - - checked ~ 5.900 ~ 4.100 ~ 760 ~ 120 ~ 250 ~ 680 ~ 70 ~10 M3.0-3.9 186 99 74 6 2 3 1 1 M4.0-4.9 43 7 34 1 1 0 0 0 M>5.0 23 0 23 0 0 0 0 0  HB/HBT: Herðubreið and Herðubreiðartögl  TFJ: Tungnafellsjökull  Kverkfj.: Kverkfjöll  Kistufell: Cluster north of Bárðarbunga that was active during the first days  automatic: Automatically detected /media/jar/Bardarbunga-2014_September-events.pdf

• 43. Bárðarbunga 2014 - September events

  2 3 1 1 M4.0-4.9 43 7 34 1 1 0 0 0 M>5.0 23 0 23 0 0 0 0 0 HB/HBT: Herðubreið and Herðubreiðartögl TFJ: Tungnafellsjökull Kverkfj.: Kverkfjöll Kistufell: Cluster north of Bárðarbunga that was active during the first days automatic: Automatically detected events in the whole country, number of events outside the Vatnajökull are comparably /earthquakes-and-volcanism/articles/nr/3001/

• 44. VI_2009_012

  in the SISZ are mostly from the year- 2000 seismic sequence, which also contains the three largest events in the data set (Jakobsdóttir et al., 2002; Hjaltadóttir and Vogfjörd, 2005). Figure 1. Map of SW Iceland showing the epicenters of the 46 earthquakes used in the study, color coded according to origin time. The time scale is shown on the left. Most of the events cluster in the Hengill region /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 45. VI_2015_005

  intense than over land. 17 Figure 8. Occurrence of low-pressure centres, as a function of centre depression, per win- ter (blue bars) and summer (red bars) season over the entire ocean or land area within the study domain. As shown in Figure 7, increasingly with longer time-scales, cyclones tend to cluster in three pre- ferred regions within the study domain, with a low occurrence of MSLP minima /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 46. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 47. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 48. VI_2014_001

  frequency curve at each site of interest. Different techniques can be used to identify homogeneous groups of watersheds such as ge- ographic proximity, or more objective methods relying on the use of catchments climatic and physiographic characteristics such as cluster analysis or the region of influence approach (Burn 1990) (see Crochet 2012b). The regional estimation method transfers a dimensionless /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 49. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf