86 results were found for u 서귀업소┫『dm080.com〕 서귀유흥 서귀주점 서귀안마♨서귀안마 서귀타이.

Results:

• 51. PhD_course-Programme_26Aug2011-final

  for widespread adoption in the water sector. Environmental Policy and Governance. DOI: 10.1002/eet.590 Kaner S (2007) Facilitator’s Guide to Participatory Decision-Making. Jossey-Bass: San Francisco. Cooke B, Kothari U (2007) Participation: the new tyranny? (4th edition) Zed Books: New York. Daniell KA, White I, Ferrand N, Ribarova IS, Coad P, Rougier J-E, Hare MP, Jones NA, Popova A, Rollin D /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 52. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 53. Traffc-maintenance_expenditures

  Manage- Basic Purchase Road Road net- Const- Acquisi- Govern- Com- Participati- Value Miscel- Total 2009 ment and road of equip- system work post- ruction tion of ment missi- on of the added laneous cost operating manage- ment develop- poned-, of land grants ons European tax over- level costs ment ment comprehen- build- and com- Regional De- heads 1991- 1991- sive- and ings pensation /media/loftslag/Traffc-maintenance_expenditures.pdf

• 54. Hare_2-participation

  Kick-off meeting Administration a73 Landkreis Osnabrück ● FD Planen u. Bauen ● FD Umwelt a73 Samtgemeinde Bersenbrück Agriculture & Forestry a73 Landwirtschaftsamt Osnabrück a73 Hauptverband des Osnabrücker Landvolkes a73 Gartenbaubetrieb a73 Maschinenring und Betriebs- hilfedienst Artland e.V a73 Forstamt Osnabrück a73 Kreisforstverband Environmental Organisation a73 Naturschutzbund Osnabrück /media/loftslag/Hare_2-participation.pdf

• 55. ces_geus_paakitsoq_full_report

  of annual accumulation rate on the Greenland ice sheet (1958–2007), Journal of Geophysical Research, 115, F02,004, doi:10.1029/2009JF001293. Corripio, J. (2003), Vectorial algebra algorithms for calculating terrain parameters from DEMs and solar radiation modelling in mountainous terrain, International Journal of Geographical Information Science, 17 (1), 1–23, doi: 10.1080/713811744. Döscher, R., U /media/ces/ces_geus_paakitsoq_full_report.pdf

• 56. VI_2017_009

  In Chapter 3 we focus on the following monthly averages: Near-surface 2 meter temperature (TAS), total precipitation (TP), and sea ice cover (SI). In Chapter 4 we add surface air pressure (PSL) and snow cover thickness (SNCT). The following daily fields will be studied as well: Near-surface wind speeds, (U and V sfcWind), maximum near-surface 2 meter temperature (TASMAX), minimum mean-surface 2 meter /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 57. 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

• 58. Kok_2-scenarios-lecture-2

  (2000) Fuzzy Cognitive Mapping: applications in education. International Journal of Intelligent Systems 15, 1-25. Khan, M.S. and Quaddus, M. (2004) Group decision support using Fuzzy Cognitive Maps for causal reasoning. Group Decision and Negotiation 13, 463-480. Kosko, B. (1986) Fuzzy cognitive maps. International Journal of Man-Machine Studies 24, 65-75. Özesmi, U. and Özesmi, S.L. (2003 /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 59. 2010_003rs

  ca ti o n s fo r th e la rg est e a rt h q u a ke s w it h in t h e S IS Z b et w ee n 1 7 0 6 a n d 2 0 0 8 d en o te d b y w h ite fil le d c ir cles. E stim a te d f a u lt p la n es o f h is to ric a l ea rt h q u a ke s a re s h o w n a s w h ite , th ick li n es ( fr o m R o th , 2 0 0 4 ). F a u lt p la n es f ro m 1 9 9 8 ( V o g fj ö rd et a l. , 2 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 60. Linnet_Ulfar_CES_2010

  °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf