95 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja 230 Cm Taliabu Barat Laut Pulau Taliabu.

Results:

• 21. 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

• 22. 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

• 23. VI_2020_005

  2000-3000 years with variations of 25 cm at most over timescales of several centuries. The few pre-1900 tide gauge records, evidence from paleo coastal sediments and reconstructed mean sea levels modelled using combined tide gauge data and satellite altimetry suggest an acceleration in global mean sea level rise in the late 19th and early 20th century (figure 4) (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 24. The crust has changed

  network used for monitoring crustal movement. The network is run by IMO in co-operation with other institutes, in Iceland and overseas. At Selfoss, lateral displacement was 20 cm to the southeast and at Hveragerði 17 cm to the northwest. Landrise was 5 cm and 3.5 cm, respectively. These tectonic changes are permanent and in concordance with a dextral fault through the mountain Ingólfsfjall /about-imo/news/nr/1326

• 25. askja_minnisblad_ens

  the lower frequency content of the wave, with main frequency around 0.05 Hz. This low frequency was even measured in the southwestern part of Iceland at a roughly 230 km distance. It probably indicates the main mass movement in the landslide. Drawing: Kristín S. Vogfjörð /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 26. Bárðarbunga 2014 - September events

  85 earthquakes have been detected since midnight, thereof 36 occurred in Bárðarbunga. The largest earthquake was of magnitude 5.5 at the southeastern rim of the caldera at 10:51. A recently mounted GPS station within the caldera showed about 20 cm subsidence at the same time. The second largest earthquake was of magnitude 4.8 at the northern rim of the caldera at 00:57. Two other earthquakes /earthquakes-and-volcanism/articles/nr/3001

• 27. Bardarbunga-2014_September-events

  on webcam observations this morning. 21 September 2014 19:00 - from geoscientist on duty About 85 earthquakes have been detected since midnight, thereof 36 occurred in Bárðarbunga. The largest earthquake was of magnitude 5.5 at the southeastern rim of the caldera at 10:51. A recently mounted GPS station within the caldera showed about 20 cm subsidence at the same time. The second largest /media/jar/Bardarbunga-2014_September-events.pdf

• 28. Bárðarbunga 2014 - September events

  85 earthquakes have been detected since midnight, thereof 36 occurred in Bárðarbunga. The largest earthquake was of magnitude 5.5 at the southeastern rim of the caldera at 10:51. A recently mounted GPS station within the caldera showed about 20 cm subsidence at the same time. The second largest earthquake was of magnitude 4.8 at the northern rim of the caldera at 00:57. Two other earthquakes /earthquakes-and-volcanism/articles/nr/3001/

• 29. News

  the surface of the glacier, a few tens of cm in size. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 2012 2011 2010 2009 2008 2007 2006 /about-imo/news/bigimg/3214

• 30. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  was even measured in the southwestern part of Iceland at a roughly 230 km distance. It probably indicates the main mass movement in the landslide. Drawing: Kristín S. Vogfjörð. Fig. 16 Figure 16. Thermal image (upper) and photograph (lower) of the rockslide area taken near Víti at the north side of Öskjuvatn. The thermal image was taken with a FLIR P660 infrared camera. Hot patches /avalanches/articles/nr/2929