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Results:

• 1. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  la tio ns hi ps be tw ee n di ffe re nt dis cipline s = > bro ad inte grate d outp ut (bu tn o tq ua nt ita tiv e) Pr ogres s towa rd sIWR M measu re s Ind icator s o fe ffec to f measu res , invo lvin g m o n ito rin g M ul tip le fra m es (so cia l sy st em ):w at er u se s su ch as n av ig at io n , hy dr o ele ct ric po w er ge n er at io n , flo o d pr o te ct io n m u st be ha rm o n ize d w /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 2. Alam_Ashraful_CES_2010

  (ECT) Working paths and machinery transportation + C Rotation period Plant production and transportation Site preparation a r b o n Planting E n e r d i o Thinnings/ harvesting operations h di g y i x i d e Emission parametersEcosystem model S ort stance transportation Long distance n p u t E m i s Emission calculation tool transportation Chipping s i o n CO2 balance 14 Energy wood /media/ces/Alam_Ashraful_CES_2010.pdf

• 3. IPPC-2007-ar4_syr

  and their interactions with sustainable develop- Figure I.1. Schematic framework representing anthropogenic drivers, impacts of and responses to climate change, and their linkages. Schematic framework of anthropogenic climate change drivers, impacts and responses ment. Topic 5 assesses the relationship between adaptation and mitigation on a more conceptual basis and takes a longer-term per- spective. Topic 6 /media/loftslag/IPPC-2007-ar4_syr.pdf

• 4. Hare-2011-ParticipatoryModelling

  Simulatio n mode l (scientific ) Im pr o ve m o de l (quality ) Fa rm er s, Fa rm busines s advisor sNO P IN D Interview s NO P IN D Qu es tio n n ai re – verificatio n NO P OT :Researcher s M KA/ M M (re nements ) KA M Has e I Simulatio n mode l (scientific ; discussio n su pp o rt ) Im pr o ve m o de l (quality , acceptance ) Farmers ,loca l authorities , association s IN D Reques t fo rdat a N /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 5. IMO_AnnualReport2014

  The map shows the likelihood at a specific location, that the hourly ground concentration of SO2 will exceed a threshold of 2600 µg/m3 dur- ing summer season. The colour scale shows di?rent values (likelihood smaller than 1% has no colour associated). I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 7 In the evening of 21 July 2014 a large rockslide oc- curred in Askja /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 6. VI_2014_001

  at each site i with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D (see Crochet, 2012c). The index flood µi(D), is modeled at each site i as a continuous function of D, as follows: µi(D) = µi 1+(D=Di)li ; (5) where µi, Di /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 7. Group5-Stakeholders_involvement

  /EPP 2 Stakeholders analysis 26 August 2011 PM/YZ/EPP 3 Stake h o l d e r s P u b l i c / p r i v at e P o w e r l e v e l (“ n u i s an ce” ca p a c i t y ) O r i e n tat i o n H or s t e n s m uni c ipal i t y ( c o m pe t e n t a u t h ori t y ) P u b l i c S t ron g Go v ernanc e N eighbour mun i c i p ali t y P u b l i c S t ron g Go v ernanc e Poli c y /media/loftslag/Group5-Stakeholders_involvement.pdf

• 8. TAF - Iceland

  TAF - Iceland Last updated 01.05.2023 - at. 13:04 SIGMET for the last six hours No SIGMET messages last 6 hours. TAF TAFBIAR011047Z01121234008KT 9999 SCT015 BKN028 TX05/0212Z TNM02/0204Z TEMPO 0112/0121 2500 -SHSN /weather/aviation/taf/

• 9. Guidelines2-for-rapporteurs

  ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 10. VI_2015_007

  with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D. The index flood, µi(D), is modelled at each site i as a continuous function of D, as follows: 12 µi(D) = µi 1+(D=Di)li ; (6) where µi, Di and li are basin dependent parameters /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf