10 results were found for AG亚游假网黑网19119992299私nbei网.

Results:

• 1. Bakkagerði - weather station - information

  coastal areas(ag) Location65°31.412', 13°49.004' (65.5235, 13.8167) Height above sea-level28.0 m a.s.l. Beginning of weather observations2017 Station owned byVeðurstofa Íslands - Ofanflóð View the observations on a mapStation list /weather/stations/

• 2. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  tg ui da n ce fo rt ra ns bo un da ry w at er s, pr ep ar ed an d P. van der Keur et al. (floo dmanag ement )an d wat er qualit y ag re ed u po n in co m m o n u n de rs ta nd in g, creat ed th e bas is fo rth e formul atio n o f joi nt m ea su re s (Fr ijte rs an d Le en tv aa r 200 3) Mo del s (na tural ,te chnica l an d so ci al sy ste m s): Uncert aint y ha s to be incorp orated : 1: Ep ist /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 3. Hare-2011-ParticipatoryModelling

  stage )Suppor t an d ski lls n ee de d Har e et a l. (2003 ) X X An aly se lin ks be tw ee n participator y structur e an d proces s implementatio n Ba rr et ea u et a l. (2010 ) X X X Pr o vid e cle ar de sc rip tio n o fproces s (m an ag e ex pe ct at io n s); monitorin g an d evaluatio n Bot s an d va n Daale n (2008 ) X X X X X Su pp o rt pr o ce ss de sig n Ad ap te d fra m ew o rk u se d in th /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 4. Refsgaard_2-uncertainty

  Delta Change Method (correction of observed precipitation) Transformation of precipitation cont fut obsfut M M PP = Observeret n dbør 0 5 10 15 20 25 30 1-12-99 11-12-99 21-12-99 31-12-99 Dato N ed bø r (m m /d ag ) Observeret Skal ring af e 5 10 15 20 25 30 35 4 - - - - t N ed bø r (m m /d ag ) Observeret D lta Change Critical assumption: Future dynamics = present dynamics No change in number /media/loftslag/Refsgaard_2-uncertainty.pdf

• 5. IPPC-2007-ar4_syr

  /media/loftslag/IPPC-2007-ar4_syr.pdf

• 6. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  sr el at ed to ag ric ul tu re in D en m ar k Cl im at e ch an ge im pa ct Adaptatio n Typ e o f proble m Conse quenc e Ris k leve l Dom inatin g uncertaint y Optio n Cos t leve l Inten t Actio n Tempora l scop e Spatia l scop e Additiona luncertaint y Sou rc e Natur e Sourc e Natur e In cr ea se d su m m er drought san d highe r w at er re qu ire m en ts caus e by longe rcro p growt h durat io n /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 7. VI_arsskyrsla2020

  meðallagi á árinu. Mikið norðanóveður gekk yfir landið dagana 10. til 11. desember sem olli miklu tjóni. Verst var veðrið á Ströndum, Norðurlandi vestra og Norðurlandi eystra. Mikil ísing og fannfergi fylgdu óveðrinu sem olli því að hundrað hross fennti í kaf, skemmdir urðu á rafmagnslínum með tilheyrandi rafmagnstruflun- um og mikil röskun varð á samgöngum. NÁTTÚRUFAR Hl ut fal l m eð all ag s /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf

• 8. 2013_001_Nawri_et_al

  the average of the (wind speed) distribu- tion is given by m = AG(1+1=k) ; (2) with gamma function, G, defined as usual. Wind power density, a measure of the energy flux through an area perpendicular to the direction of motion, varies not only with the cube of wind 15 Figure 2. Annual modelled distributions (dashed lines) and corresponding Weibull fits (solid lines) of wind speed at 50 mAGL, for two /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 9. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 10. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf