82 results were found for L 조루인터넷홍보{모든톡 @adgogo} 조루광고팀 조루광고대행‧조루광고문의㋽범내골조루 Adt.

Results:

• 31. norsem_lindholm

  Neotectonics in Nordland; NEONOR 2 C. Lindholm, O. Olesen, I. Janutyte, S. Gradman, M. Keiding, H. Kierulf, M. Ask, J. Dehls, Y. Maystrenko, F. Riis, L. Rise and other project partners The Nordland shore region is known to be seismically active with deep local sediment basins on the continental shelf that stretches some 200 km west of the coastline. The offshore areas west of Nordland have /media/norsem/norsem_lindholm.pdf

• 32. 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

• 33. Climate and Modeling Scenarios

  A. (2010b). 21st century changes in the European climate: uncertainties derived from an ensemble of regional climate model simulations. Tellus, published online. DOI: 10.1111/j.1600-0870.2010.00475. Ólafsson H, & Rögnvaldsson Ó. (2010). Regional and Seasonal Variability in Precipitation Scenarios For Iceland. Hydrology Research, in revision. Peltonen-Sainio, P., Hakala, K., Jauhiainen, L /ces/publications/nr/1680

• 34. Jokull-guidlines

  Reykjavík, 139 pp. Paterson, W.S.B. 1994. The Physics of Glaciers (Third Edition). Pergamon. 480 pp. Vogt, P.R., G.L. Johnson and L. Kristjánsson 1980. Morphology and magnetic anomalies north of Iceland. J. of Geophysics 47, 67-80. Walker, G.P.L. 1974. Eruptive mechanisms in Iceland. In L. Kristjánsson, ed. Geodynamics of Iceland and the North Atlantic Area. D. Reidel, Dordrecht /media/jar/Jokull-guidlines.pdf

• 35. Dataseries and components

  Analysed components - IMO's research: Sulphur and salinity measurements: Precipitation: SO4-S, NO3-N, Cl, Na, Mg, K, Ca (mg/l) Precipitation: conductivity (µS/cm), quantity (mm), pH Aerosol: SO4-S, Cl, Na, Mg, K, Ca, Fe (µg/m3) Air: SO2-S (µg/m3) Heavy metals in precipitation: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/ml) Cl, NO3-N, SO4-S, Na, K, Ca, Mg, NH4-N, Br, F (µg/ml) conductivity (µS/cm /pollution-and-radiation/pollution/components/

• 36. Dyrrdal_Anita_CES_2010

  • Analyse future snow scenarios Introduction Data & Methods Results 0 50 100 150 200 250 300 350 400 450 0-100 100- 200 200- 300 300- 400 400- 500 500- 600 600- 700 700- 800 800- 900 900- 1000 1000- 1100 1100- 1200 1200- 1300 1300- 1400 1400- 1500 1500- 1600 1600- 1700 1700- 1800 1800- 1900 1900- 2000 2000- 2100 2100- 2200 Høyde (m o.h.) A n t a l l v æ r s t a s j o n e r Elevation of met.no /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 37. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  ://www.ine.es/en/prensa/np583_en.pdf, July 20, 2010. [7] Fundación Empresa y Clima (2009): “Afectaciones del Cambio Climático sobre el Sector Turístico Español”, http://www.empresaclima.org 30 May 2009. [8] IPCC (Intergovernmental Panel on Climate Change), 2007. IPCC Fourth Assessment Report: Climate Change 2007. United Nations Environment Programme. [9] Hein, L.; Metzger, M.J. y Moreno, A. (2009 /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

• 38. Eriksson_Garvill_Nordlund_2006

  (F ð1; 905Þ ¼ 6:89, po0:01, partial Z2 ¼ 0:008), and a larger reduction in own and others’ car use compared to the increase with two SEK/l (F ð1; 880Þ ¼ 16:96, po0:001, partial Z2 ¼ 0:019 and F ð1; 879Þ ¼ 15:64, po0:001, partial Z2 ¼ 0:017 respectively). In addition, the increase with five SEK/liter was perceived as more unfair (F ð1; 904Þ ¼ 10:06, po0:01, partial Z2 ¼ 0:011) and respon- dents /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 39. 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 i
  ed .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

• 40. Hydropower - Glacier, Snow and Ice

  Guðmundsson, S., Björnsson, H., Pálsson, F., Jóhannesson, T., Hannesdóttir, H. o.fl. (2011). Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland. The Cryosphere, 5, 961-975, doi:10.5194/tc-5-961-2011. Andreassen, L. M., & Oerlemans, J. (2009). Modelling long-term summer and winter balances and the climate sensitivity of Storbreen, Norway. Geogr. Ann., 91 /ces/publications/nr/1940