72 results were found for WA 0821 7001 0763 (FORTRESS) pintu motif kayu solid modern Heram Kota Jayapura Papua.

Results:

• 31. Supporting structures stopped most of an avalanche

  slab had started to break up but was nevertheless moving as a more or less solid block when it was stopped by the supporting structures. It may be assumed that the avalanche would have been many times larger, and that it might have reached the health care centre, if the supporting structures had not reduced the released snow volume by an order of magnitude. This is the first example /about-imo/news/nr/2476/

• 32. Supporting structures stopped most of an avalanche

  that the avalanche slab had started to break up but was nevertheless moving as a more or less solid block when it was stopped by the supporting structures. It may be assumed that the avalanche would have been many times larger, and that it might have reached the health care centre, if the supporting structures had not reduced the released snow volume by an order of magnitude. This is the first example /avalanches/articles/nr/2475/

• 33. 2013_001_Nawri_et_al

  the average of the (wind speed) distribu- tion is given by m = AG(1+1=k) ; (2) with gamma function, G, defined as usual. Wind power density, a measure of the energy flux through an area perpendicular to the direction of motion, varies not only with the cube of wind 15 Figure 2. Annual modelled distributions (dashed lines) and corresponding Weibull fits (solid lines) of wind speed at 50 mAGL, for two /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 34. 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

• 35. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 36. Markarfljót outwash plain and Öræfajökull

  Öræfajökull Volcano: Geology and historical floods (pdf 5.43 Mb) Pages 17–44 Matthew J. Roberts og Magnús T. Gudmundsson Short summary Despite the documented severity and lasting geomorphic imprint of the 1362 and 1727 jökulhlaups from Öræfajökull, there is scant information about the routing and extent of these floods. Using field observations, aerial photographs, and modern-day analogues /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 37. 2011_005

  network on the north coast of Iceland. According to the number of 4000 – 5700 Trimble receivers, the total network is relatively modern. Trimble NetRS receivers have an ethernet and serial interface, but the older models have serial interfaces only, making data transfer more cumbersome with modern communication technology such as GPRS and 3G. In general the receivers have been reliable. The NetRS /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 38. Paper-Olafur-Rognvaldsson_91

  ice cap is in good agree- ment with observations (cf. Fig. 3) over the northern part of the ice cap (HN, Figure 3: Estimated mean accumulated winter precipitation [mm] along profiles HN (N-part), HSA (SE-part) and HSV (SW-part) at altitudes between 1450 and 1650 metres (solid line, Jóhannesson et al., 2006). Dashed line represents simulated precipitation by MM5 (nine point average) at Hofsjökull /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 39. A glimpse into the field

  fountains whereas this morning it had a solid wall of fire. These are signs of temporary narrowing in the eruptive vent. Baugsbörn (i.e. Baugur's babies, three or four small vents north of Baugur) do have lava lakes that are boiling. Suðri's activity has increased, probably because the position of its rims has changed. Lava flows towards south from Suðri. These changes in the craters /about-imo/news/nr/2985

• 40. A glimpse into the field

  fountains whereas this morning it had a solid wall of fire. These are signs of temporary narrowing in the eruptive vent. Baugsbörn (i.e. Baugur's babies, three or four small vents north of Baugur) do have lava lakes that are boiling. Suðri's activity has increased, probably because the position of its rims has changed. Lava flows towards south from Suðri. These changes in the craters /about-imo/news/nr/2985/