57 results were found for WA 0821 7001 0763 (FORTRESS) Pintu Baja Set Kabianggama Yahukimo.

Results:

• 1. Kok_et_al._TFSC_published_2011

  exploratory scenarios (narrative storylines) were developed, in first instance based on a set of existing European scenarios. Results matched expectations; the process produced stories that are complex, integrated, and rich in detail. During the backcasting exercise, four timelines were constructed, each of which took one exploratory scenario as context. The backcasting process established a strong link /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 2. VI_2021_008

  a seismic network (see Figure 2), several stations must identify this signal before an audio alarm is set off. If enough stations within a particular filter vote, a tremor event will be detected in that bandpass filter, and the filter will be put into a triggered state. At this point, the audio alarm will be sounded in the monitoring room, and a new tremor event will be added to the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

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

  addresses the role of AIWM in coping with the impacts of climate change on floods and droughts in four case-studies in three European river basins. The explorative character of this paper intends to identify general patterns in the char- acteristics of AIWM and assumes that regimes with a higher level of AIWM consider and implement more advanced and a more diverse set of structural and non- structural /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 4. 2010_017

  measurements instead of river discharge data. The National Energy Authority has supported this work with contracts on 8 hydrological modelling and groundwater research. The model was then used to make a future projection of runoff for two watersheds in Iceland for the period of 2021–2050 (Einarsson & Jónsson, 2010). The WaSiM model (Jasper et al., 2002; Jasper & Kaufmann, 2003) was first set up /media/ces/2010_017.pdf

• 5. 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

• 6. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 7. Grimsvotn_status_2011-05-30_IES_IMO

  Since Thursday the tremor had been intermittent. Today, Monday 30 May, it has been confirmed by the participants of Iceland Glaciological Society's spring expedition that the eruption has ended. The end of the Grímsvötn eruption is set to 7 UTC Saturday morning 28 May 2011. /media/jar/Grimsvotn_status_2011-05-30_IES_IMO.pdf

• 8. VI_2009_006_tt

  of the subglacial seal at the beginning of the 1996 jökulhlaup and concluded that the high water level reached before the on- set of the 1996 flood could be explained with the traditional theories of Röthlisberger (1972) and Nye (1976) but he did not address the rapid discharge increase following the breaking of the seal. Flowers et al. (2004) concluded that a model fundamentally different from /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 9. Hare-2011-ParticipatoryModelling

  - work. The second half of the article discusses the potential for participatory modelling to progress from being a mainly research-driven activity in the water sector to one being adopted for widespread use by water managers. By widespread adoption I mean that participatory modelling becomes mainstream in the sector and that managers set up their own organizing teams, independent of researchers /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 10. 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