63 results were found for WA 0821 1305 0400 RAB Bangunan Plafon Model Granit Terpercaya Cisarua Kab Bogor.

Results:

• 1. Isskyrsla_20101212

  örugt að fara fyrir Horn í um 10 sml frá landi en það yrði að hafa góðan útvörð. Kl.1341, kalla TFB og spyr um ETA í RVK, ETA um kl 1440. Kl 1305, AIS umferð fyrir N- Horn. Vegna bilunnar í WS 1 var megináhersla lögð á ískönnun í þessu flugi. Flugskýrsla TF-SIF 12. desember 2010 Flug nr. 117410.025 Ískönnun. Meginröndin lá um eftirtalda staði. 1. 67°47.0N 023 /media/hafis/skyrslur_lhg/Isskyrsla_20101212.pdf

• 2. 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

• 3. Kok_and_Veldkamp_editorial_ES-2011-4160

  van Apeldoorn et al. 2011, van Lieshout et al. 2011) and two with governance (Mandemaker et al. 2011, van der Veen and Tagel 2011). The papers show the application of a wide variety of methods, thus also spawning multiple disciplines and theoretical starting points. Methods range from model development and application and a statistical empirical analysis to semistructured interviews. The case /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 4. 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

• 5. 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

• 6. Kok_JGEC658_2009

  in the models, while on the other hand, models require quantitative information on a wealth of parameters that is often difficult to extract from storylines. In other words, there is a mismatch between storylines and model parameters (Steps 3–4 in Fig. 1), as well as between model output and revised stories (Steps 5–6). In practice, particularly the translation of stories into quantified model /media/loftslag/Kok_JGEC658_2009.pdf

• 7. 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

• 8. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

• 9. 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

• 10. 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