82 results were found for L 출장마사지♩ㄲr톡 GTTG5♩飖태릉입구역슈얼마사지㌀태릉입구역슈얼출장詫태릉입구역스웨디시☐태릉입구역스웨디시출장♍murmurous/.

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

  : Significant at 90% CL Norwegian Meteorological Institute met.no Fokstugu (973 m.a.s.l.) Introduction Data & Methods Results Trends in start and end: Significant at 99% CL /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

  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

• 40. Hydropower - Glacier, Snow and Ice

  glacier-scaling-hydrological model. 88-89. Machguth, H., & Ahlstrøm, A. (2010). Surface Mass Balance of the Greenland Ice Sheet in the Paakitsoq Area, Illulisat, West Greenland - Scenarios and Related Uncertainties. p. 42-43. Melvold, K. & Laumann, T. (2010). A coupled mass-balance and ice-flow model for Midtdalsbreen; projection of glacier length based on climate scenarios (CES). 90-91. Radic, V /ces/publications/nr/1940