85 results were found for r 사상오피▥《dm080.com〉 사상안마♛사상출장☏사상출장 사상오피♧사상유흥.

Results:

• 21. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 22. Dyrrdal_Anita_CES_2010

  Results W i n t e r t e m p e r a t u r e Max snow depth Trend slope Number of snow days Period II P e r i o d I I I Max snow depth Number of snow days Norwegian Meteorological Institute met.no Correlation analysis (1961-08) 138 mutual stations Introduction Data & Methods Results Correlation with winter temperature Correlation with winter precipitation In warmer regions both snow parameters /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 23. Sigurður Th. Rögnvaldsson

  Veðurstofu Íslands VÍ-G99007-JA02. Sigurður Th. Rögnvaldsson 1999. Kort yfir sjálfvirkt ákvarðaðar staðsetningar jarðskjálfta á Íslandi. URL: http://hraun.vedur.is/ja/englishweb/index.html, 21.06.1999. Sigurður Th. Rögnvaldsson og R. Slunga 1993. Routine fault plane solutions for local networks: A test with synthetic data. Bull. Seism. Soc. Am. 83, pp. 1232 1247. Sigurður Th. Rögnvaldsson og R /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/

• 24. Sigurður Th. Rögnvaldsson

  Veðurstofu Íslands VÍ-G99007-JA02. Sigurður Th. Rögnvaldsson 1999. Kort yfir sjálfvirkt ákvarðaðar staðsetningar jarðskjálfta á Íslandi. URL: http://hraun.vedur.is/ja/englishweb/index.html, 21.06.1999. Sigurður Th. Rögnvaldsson og R. Slunga 1993. Routine fault plane solutions for local networks: A test with synthetic data. Bull. Seism. Soc. Am. 83, pp. 1232 1247. Sigurður Th. Rögnvaldsson og R /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur

• 25. Climatological data

  values t mean temperature tx average daily maximum temperature txx highest maximum temperature month/year txx_dag1 date of highest maximum temperature tn average daily minimum temperature tnn lowest minimum temperature month/year tnn_dag1 date of lowest minimum temperature rh mean relative humidity r preciptiation total rx maximum 24-hour precipiation /climatology/data/

• 26. ces_SA_group_flyer_new

  by season (%) between 1991-2007 and 1961-1990 in the Baltic countries 1 9 0 0 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 - 1 5 - 1 0 - 5 0 5 1 0 1 5 P r e c i p i t a t i o n a n o m a l y ( % ) R e g i o n 1 R e g i o n 2 R e g i o n 3 R e g i o n 4 F un c t ion P lo t 5 1 9 0 0 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 - 1 . 5 - 1 - 0 . 5 0 0 . 5 1 1 . 5 T e m p e r a t u r e a n o m /media/ces/ces_SA_group_flyer_new.pdf

• 27. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  ). NeWater is based on the hypothesis that IWRM cannot be realised unless current management regimes undergo a transition towards more 0301-4797/$ - see front matter r 2007 Elsevier Ltd. All rights reserved. doi:10.1016/j.jenvman.2007.05.009 Corresponding author. Tel.: +45 38 14 27 71; fax: +45 38 14 20 50. E-mail address: hjh@geus.dk (H.J. Henriksen). (Downing et al., 2005). Vulnerability /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 28. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  inty in decision making linking pluriform uncertainty combining certified and tacit knowledge Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos Eivind Junker Jussi Ylhäisi Athanasios Votsis Karoliina Pilli-Sihvola Yuang Zheng Väi ö Nurmi Jiao Xi nj Wejs a p p l i c a n t n o . a b s t r a c t n o . n a m e c o u n t r y d i s c i p l i n e ( M S c . ) 1 3 /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 29. 2013_001_Nawri_et_al

  grid points on Hellisheiði (blue and cyan lines), and for two grid points on Skagi (red and magenta lines). speed, but also with air density. To simplify wind energy assessments, and to allow for the use of Weibull statistics, it is commonly assumed that air density, r , is not correlated in time with wind speed, at least on a seasonal basis (Hennessey, 1977). Average wind power density /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 30. Paper-Olafur-Rognvaldsson_92

  a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf