68 results were found for WA 0821 7001 0763 (FORTRESS) Model Pintu Rumah Cluster Terbaru Maro Sebo Ilir Batang Hari Jambi.

Results:

21. Further information on the seismicity in Northern Iceland

were M 3.6 at 03:42 and M 3.2 at 07:47. Since the afternoon of 23 October, a new cluster of earthquakes has occurred about 5 km north-northwest of Gjögurtá on the intersection of the eastern end of Eyjafjarðaráll and the Húsavík-Flatey Fault (HFF). The largest events in this region were M 3.1 at 23:38 on 23 October and 3.2 at 22:20 on 24 October (see the map). Movements on the fault of the M /about-imo/news/nr/2561
22. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

their audience. Climatic Change (2012) 112:233–242 DOI 10.1007/s10584-011-0205-7 C. S. Weiler (*) Office for Earth System Studies, Whitman College, Walla Walla, WA 99362, USA e-mail: weiler@whitman.edu J. K. Keller School of Earth and Environmental Sciences, Chapman University, Orange, CA 92866, USA C. Olex The Point, 121 Jewett Street, Newton, MA 02458, USA 1 Introduction Of all the applications /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf
23. IPPC-2007-ar4_syr

judgment and statistical analysis of a body of evidence (e.g. observations or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%; extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very unlikely <10%; extremely unlikely <5 /media/loftslag/IPPC-2007-ar4_syr.pdf
24. 2010_017

Improving groundwater representation and the parameterization of glacial melting and evapotranspiration in applications of the WaSiM hydrological model within Iceland Bergur Einarsson Sveinbjörn Jónsson VÍ 2010-017 Report Improving groundwater representation and the parameterization of glacial melting and evapotranspiration in applications of the WaSiM hydrological model within /media/ces/2010_017.pdf
25. PhD Workshop 2012

structure, analysis or interpretation of their study). Small clusters of 3 or 4 related dissertation projects will be discussed and reviewed with the aid of experts in parallel sessions. Following acceptance and registration for the Workshop, every PhD student will be allocated a mentor from the pool of experts. Each cluster will receive several assignments for group work. The Workshop will also include 2 /nonam/adaption/phd-workshop-2012/
26. norsem_begga

earthquake locations significantly. Our first step is to test the algorithm on a small subset of 215 earthquakes in year 2001, as reported in the SIL catalog, the earthquakes being located in and around the Geysir region in Southern Iceland. Three small areas were active during the year of 2001, although only one of them was recorded to be active as an earthquake sequence (western cluster; main /media/norsem/norsem_begga.pdf
27. 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 ied .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
28. Journal_of_Hydrology_Veijalainen_etal

in flooding were evaluated at 67 sites in Finland with var- iable sizes of runoff areas using a conceptual hydrological model and 20 climate scenarios from both glo- bal and regional climate models with the delta change approach. Floods with a 100-year return period were estimated with frequency analysis using the Gumbel distribution. At four study sites depicting dif- ferent watershed types /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
29. VI_2013_006

with a gray cross at the origin (0,0), the median location of the lightning with a blue circle. Individual lightning are red and brown dots, the closest half of the dots to the median are brown. A backtraced wind correction of the median is shown by the line and blue square. The wind at the 500 hPa level of a weather model was used and this wind backtraced for 500 s. The best available data /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
30. 2010_003rs

plate spreading motion, according to the NUVEL-1A plate motion model (DeMets et al., 1990, 1994). Using a simple screw dislocation model to interpret GPS campaign measurements on the RP from 1993 and 1998, Hreinsdóttir et al. (2001) suggested that rifting on the peninsula occurred in pulses, since their research indicated present accumulation of left-lateral shear strain parallel to the peninsula /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf