Note
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27 results were found for WA 0821 7001 0763 (FORTRESS) Ukuran Pintu Rumah Ideal Teminabuan Sorong Selatan.

Results:

11. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
12. vonKorff_etal-2010

/media/loftslag/vonKorff_etal-2010.pdf
13. IPPC-2007-ar4_syr

/media/loftslag/IPPC-2007-ar4_syr.pdf
14. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

and policymakers when analyzing, assessing and managing risk/uncertainty? In many cases where uncertainty and risk is involved, acts and regulations prescribe different methods of analyses and/or assessments to be carried out before the decision is made. The ideal is that researchers provide objective, neutral facts to the policymakers or politicians. However, research and policy are often closely /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
15. 2010_017

m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf
16. Journal_of_Hydrology_Veijalainen_etal

The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
17. 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
18. VI_2009_006_tt

than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
19. Bárðarbunga 2014 - August events

/earthquakes-and-volcanism/articles/nr/3000
20. Bardarbunga-2014_August-events

/media/jar/Bardarbunga-2014_August-events.pdf