93 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Tinggi 220 Cm Patamuan Padang Pariaman.

Results:

• 21. On the weather forecast and the flood conditions

  streams close to the capital region have risen sharply.Hvítá, Ölfusá, SogThe level of Hvítá and Ölfusá has not increased significantly yet, although further intense rainfall is expected in the region until late on Thursday. The discharge of Sog, which drains from Þingvallavatn, is presently 220 m³/s, which is twice the river's typical level. Flooding in Sog will most likely peak on Thursday afternoon /about-imo/news/on-the-weather-forecast-and-the-flood-conditions

• 22. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 23. VI_2016_006_rs

  width of 15–20 cm and a maximum vertical displacement of the lower with respect to the upper edge of 10 cm. After a long wet period in August–October 2001, with several heavy rainstorms, additional cracks, the largest of which ca. 100 m long, were discovered close to the rim of Þófi near Hæðarlækur. The movement of the surface slowed down and essentially stopped without a catastrophic failure /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 24. Bardarbunga_kafli20140825

  eruptions. Inflation expected 2 Current activity Heightened unrest from 16 August 2014. See http://vedur.is for live information Distance to international airports: Keflavík 260 km, Reykjavík 220 km, Akureyri 115 km, Egilsstaðir 155 km Principal hazards: Tephra fallout, jökulhlaups _________________________________________________________________________ Fissure swarm: Exists Yes Length /media/jar/Bardarbunga_kafli20140825.pdf

• 25. Traffc-maintenance_expenditures

  602 1985 69 162 268 854 21 519 287 550 - 8 390 17 755 26 574 8 767 - - - 708 572 1 444 484 1984 63 220 239 096 17 569 274 379 - 6 561 17 510 21 630 7 314 - - - 646 775 1 373 444 1983 58 155 225 692 22 930 273 852 - 7 658 15 811 17 982 7 433 - - - 629 513 1 410 203 1982 52 712 189 383 15 822 262 412 - 8 974 15 974 17 509 10 038 - - - 572 824 1 385 993 1981 48 251 172 997 14 874 234 817 - 6 526 20 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 26. Hare-2011-ParticipatoryModelling

  ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec i
  ed .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 27. Seismic signal associated with the Askja rockslide

  be seen on all seismometers around Askja, while the low frequency signal can be seen on broadband seismometers throughout the whole country. The traveltime of the signal from Mókollar (mko) close to Askja to station Ásbjarnarstaðir (asb) in Borgarfjörður is about 55 s; the distance between both stations is about 220 km. This gives the signal an apparent velocity of around 4 km/s, which /earthquakes-and-volcanism/articles/nr/2921

• 28. Eyjafjallajokull_SK_20101214_1

  on volcanic activity Earth science Seismic monitoring (SIL network) GPS measurements Strain measurements Hydrology Water level gauges Heat and conductivity measurements Show early signs of volcanic activity under the ice caps. Atmosphere ~220 weather stations (~120 automatic and ~100 manned stations) Weather radar Direct and indirect plume measurements lightning sensors radiosondes SO2 measurements /media/vedurstofan/myndasafn/Eyjafjallajokull_SK_20101214_1.pdf

• 29. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 30. VI_2020_004

  49 Probabilistic hazard map for a load ≥1000 kg/m2 (Öræfajökull) ............................ 78 Figure 50 Seasonal analysis for 1 kg/m2 (~1mm) tephra ground load (Öræfajökull). ............ 79 Figure 51 Seasonal analysis for 10 kg/m2 (~1 cm) tephra ground load (Öræfajökull). ........... 80 Figure 52 Impact map for roads in case of an eruption like 1362 at Öræfajökull ................... 81 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf