97 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja 240 Cm Ngimbang Lamongan.

Results:

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

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

• 22. 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

• 23. 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

• 24. 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

• 25. New article on glacier changes in

  cubic kilometers of water), or a total of 540 ± 130 Gt. This corresponds to 16 ± 4% of the volume of the glaciers around 1890. About half of this mass was lost from 1994 to 2019 or 240 ± 20 Gt, which is about 9.6 ± 0.8 Gt / year on average during that period. Vatnajökull has thinned by 45 m on average in the period 1890–2019, Langjökull by 66 m and Hofsjökull by 56 m. This corresponds /about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years

• 26. Reykholt-abstracts

  in July 2016 on a Delta II rocket from Vandenberg Air Force Base in California. ICESat-2 will carry the Advanced Topographic Laser Altimeter System (ATLAS) and collect data to a latitudinal limit of 88 degrees. In contrast to Geoscience Laser Altimeter System (GLAS) on ICESat, ATLAS employs a 6-beam micro-pulse laser photon-counting approach. It uses a high repetition rate (10 kHz; 70 cm /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 27. VI_2014_005

  reanalysis project is 37h1.2. The simulations were run on the c2a supercomputer at the European Centre for Medium Range Weather Forecasts (ECMWF). The model domain is the same as the one used for the IMO operational forecast runs (DOMAIN=ICELAND)2, with 300 240 horizontal grid points, and a horizontal grid-point spacing of about 2.5 km in both directions. HARMONIE uses a terrain-following sigma /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 28. VI_2015_006

  Meteorological Office (IMO) between 2011 and 2014. The model do- main is also the same as for the IMO operational runs, with 300 240 horizontal grid points cov- ering the whole of Iceland and parts of the surrounding ocean, and with a horizontal grid-point spacing of about 2.5 km in both directions. The model is run with the standard 65 vertical levels, and with a non-hydrostatic dynamic core /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 29. 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

• 30. Markarfljót outwash plain and Öræfajökull

  destruction of the road network; In Öræfi, up to 130 lives could be lost and 240–250 people isolated. Chapter VII. Öræfajökull: Evacuation time modelling of areas prone to volcanogenic floods (pdf 2.96 Mb) Pages 141–164 Emmanuel Pagneux Short summary A model of evacuation routes and timing for areas exposed to floods due to eruptive activity of Öræfajökull Volcano is presented. Estimates /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/