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27 results were found for WA 0859 3970 0884 Kontraktor Partisi Kaca Es Matesih Karanganyar.


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  • 1. IPPC-2007-ar4_syr

    of Europe, and earlier onset of and increases in seasonal production of allergenic pollen in Northern Hemisphere high and mid-latitudes {WGII 1.3, 8.2, 8.ES, SPM}  some human activities in the Arctic (e.g. hunting and shorter travel seasons over snow and ice) and in lower-elevation alpine areas (such as limitations in mountain sports). {WGII 1.3, SPM} Sea level rise and human development /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 2. 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
  • 3. Kriauciuniene_Jurate_CES_2010

    periods (1922-1980 and 1981-2007) -80 -40 0 40 80 120 1922-1980 1981-2007 % Average temperature anomaly (ºC) of 1931-1960 and 1991-2007 compared with reference period LT- W LT- C LT- SE LV- SE LV- NE LV- C LV- W ES- N ES- E ES- W 1931- 1960 -0.2 -0.1 0.0 -0.1 -0.2 -0.1 -0.1 0.0 0.1 0.1 1991- 2007 0.9 0.9 0.9 0.8 0.9 0.9 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf
  • 4. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    requires an appropriate monitoring system and the use of integrated or more simple models for the prediction of future scenarios including effects of implemented measures. Such integrated models should also include socio-economic aspects. In the Netherlands for the Major sources of uncertainty in current IWRM practice Tabl e 1 St ep 1: Es ta bl ish st at us an d go al s Pr oces s in Ste p 1 Es tablis /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 5. ces_risk_flyer

    applied in various case studies, the Risk Assessment Framework and its tools have been shown to aid visualisation of the risks and i i i d i h li h i h Supporting decision‐making t e g g te r s s an opportun t es n re at on to the likelihood of the examined scenarios and the likelihood of the risks and opportunities identified. The different quadrants of the table (act, prepare and monitor) guide /media/ces/ces_risk_flyer.pdf
  • 6. Keranen_Jaana_CES_2010

    erations which will be done to protect against th e phenome na a nd its conse quenc es The consequenc es of the phenom ena to the distribution network T he con seque nc es of the phe nom ena to the pow er plant The conse quence s of the phe nomena to e nerg y sourc e and its usability Probability according to IP CC 2007 Phe nom ena acco rding to regional scena rio /media/ces/Keranen_Jaana_CES_2010.pdf
  • 7. Wind Energy

  • 8. Group5-Stakeholders_involvement

    E . g . 8 0 % qu e s t i onn a i r es to pu b l i c re t urne d a n d p r o c e s s ed a t t h e e nd o f t h e phase Initial proposal 12 Catalogue of measures Testing & revision 12 Revised catalogue of measures Decision-making 2 Published catalogue of measures *Objective Verifiable Indicators: the quantitative, qualitative, and time-bound measures that constitute evidence /media/loftslag/Group5-Stakeholders_involvement.pdf
  • 9. Group-1_Scenarios-for-AWM

    example can be given by the low cost still flood risk adaptation by implementing early warning system. But there is one more suggestion dfor stakeholders to restrict infrastructure in the cities of Horsens. Fiva PhD Courses : Adaptive management in relation to climate change (august 22 2011 - august 26 2011) 2 / 3 R es e a r c h Flood f r equenc y a n d i n t ensi t y c o m m un i c a t /media/loftslag/Group-1_Scenarios-for-AWM.pdf
  • 10. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

    e in relatio n to climat echang eadapt ation .X ,X X ,XX X is a ge n era lguid eo n th e relativ e imp ortanc e leve lo fth e sourc es , alth oug h it mus tb e em phasise d tha tth e imp ortanc e o fth e indi vidua lsou rce s o fun certaint y is co n tex tspe cifi c St ep si n cl im at e ch an ge ad ap tat io n an al ys es (ch ain in u n ce rta in ty ca sc ad e, Fi g. 2) So ur ce s o fu n ce rta /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

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