80 results were found for WA 0821 7001 0763 (MEVVAH) model marmer dinding P. Haruku Kabupaten Maluku Tengah Maluku.

Results:

• 1. Milly_etal-2008-Stationarity-dead-Science

  appears to be driving a poleward expansion of the subtropical dry zone (8), thereby reducing runoff in some regions. Together, circulatory and thermodynamic responses largely explain the picture of regional gainers and losers of sustainable freshwater availability that has emerged from climate models (see figure, p. 574). Why now? That anthropogenic climate change affects the water cycle (9 /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 2. Hare-2011-ParticipatoryModelling

  the system works’ ( Q3Mulligan and Wainwright, 2005, p. 14). This might include paper- or computer-based representa- tions of a system’s ontological model (i.e. key system components and their structural relationships). A common representation is a directed graph in which components are visualized by nodes and relationships by directed arrows between nodes (e.g. causal diagrams or inuence diagrams /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 3. 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

• 4. CES_D2.4_task1

  model-simulated climate changes and observed global mean temperature changes are used to extrapolate past observations forward in time, to make them representative of present or future climate conditions. By using this method, we estimate the probability distributions that characterize the interannual variability of temperature and precipitation in the present (year 2010) climate and later /media/ces/CES_D2.4_task1.pdf

• 5. TietavainenHanna_CES_2010

  the observed data sets are smaller in SW than in NE • MMM overestimates precipitation, but is closer to observations in SW than NE barb2right Better observational coverage in SW SW NE p r e c i p i t a t i o n s u m ( m m ) CES Conference, Oslo 31.5.-2.6.2010 SWNE • Precipitation trends (mm / 10 yr) in 1961-2000 according to observations and model simulations (MMM) • Including the range /media/ces/TietavainenHanna_CES_2010.pdf

• 6. Hydropower - Glacier, Snow and Ice

  ). Distribution of snow accumulation on the Svartisen ice cap, Norway, assessed by a model of orographic precipitation. Hydrological Processes, 22(19), 3998-400. Other international Crochet, P., Jóhannesson, T., Sigurðsson, O., Björnsson, H. & Pálsson, F. (2008). Modeling precipitation over complex terrain in Iceland. In: Sveinsson, Ó. G. B., S. M. Garðarsson and S. Gunnlaugsdóttir (eds.), Northern /ces/publications/nr/1940

• 7. 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

• 8. 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

• 9. 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

• 10. program17012012

  Airborne Measurements of Volcanic Ash - results from Eyja and the new Met Office Civil Contingency Aircraft Jonathan P. Taylor, UK Met Office 11:15 Observational systems for monitoring of volcanic ash Sibylle von Löwis, Geirfinnur S. Sigurðarson, IMO 11:45 NAME dispersion model, an introduction Jonathan P. Taylor, UK Met Office 12:15 – 13:30 Lunch break The volcanic ash problem /media/vedurstofan/utgafa/hlidarefni/program17012012.pdf