61 results were found for WA 0859 3970 0884 Katalog Harga Pintu Model Korea Godean Sleman.

Results:

1. Bio Energy

and climate scenarios for Finland. Biomass and Bioenergy 32: 934-943. Other international Alam, A., Kilpeläinen, A. and Kellomäki, S. (2010). Climate change and mitigation options in a boreal ecosystem with implication for forest management practices. XXIII IUFRO World Congress - Forests for the Future: Sustaining Society and the Environment. 23.8. ? 28.8.2010, Seoul, Republic of Korea /ces/publications/nr/1939
2. CES_D2.4_VMGO

is the world’s coldest country with its annual mean area averaged temperature of -4.1ºC. Projections with the global climate models provide a physically consistent quantitative picture of climate change through the 21st century. The model projected mean warming will plausibly be accompanied by changes in the extremes that exhibit considerable interregional differences. The extremes at limited /media/ces/CES_D2.4_VMGO.pdf
3. Mid-Latitudes-Agenda1_nov2013EH

Korea Polar Research Institute Korea Agenda L’Heureux, Michelle National Centers for Environmental Protection USA Magnusdottir, Gudrun University of California - Irvine USA Mote, Tom University of Georgia USA Nawri, Nikolai International Maritime Organization UK Ólafsson, Haraldur Icelandic Met Office Iceland Overland, James NOAA/Seattle USA Petersen, Guðrun Nina Icelandic Met Office Iceland /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf
4. 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
5. 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
6. 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
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. 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
9. 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
10. VI_2009_006_tt

–conduit model for subglacial water flow was used to simulate the jökulhlaup. The model was forced with the estimated outflow from the subglacial lake. The simulations were not successful as a realistic subglacial pressure field could not be obtained for a reasonable fit of the jökulhlaup discharge at the glacier terminus. This indicates that the physical basis of the model is insufficient to provide /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf