82 results were found for N 신용카드현금화 〔tktaka1¸com〕 티켓타카 O 신용카드현금화 전문 포탈 이용한🇷erythema/.

Results:

• 31. 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

• 32. Lorenzoni_Pidgeon_2006

  : PidgeonN@cardiff.ac.uk Climatic Change (2006) 77: 73–95 DOI: 10.1007/s10584-006-9072-z c© Springer 2006 74 I. LORENZONI AND N. F. PIDGEON national policies strongly on fossil fuels. The British Prime Minister encapsulated these tensions when he recently stated that there is “no bigger long-term question facing the global community” than climate change (BBC, 2004), whilst emphasising the need /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 33. Kjellstrom_Erik_CES_2010

  ANN−10 −5 0 5 10 15 20 delta w (% ) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17C h a n g e i n g e o s t r o p h i c w i n d s p e e d ( % ) Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling Chen and Aschberger, 2006 17 CM IP G CM s A need for regional ensemble simulations head2right Changes are uncertain head2right Size and sometimes even sign /media/ces/Kjellstrom_Erik_CES_2010.pdf

• 34. Journal_of_Hydrology_Veijalainen_etal

  in Finland Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland b Department of Geography, FI-20014 University of Turku, Turku, Finland a r t i c l e i n f o Article history: Received 7 January 2010 Received in revised form 13 June 2010 Accepted /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 35. VI_2015_009

  vhm145 Vestari-Jökulsá D+J+L 844 751 11.3 924 1971–2014 vhm167 Austari-Jökulsá D+J 553 916 28.8 1208 1985–2014 8 vhm59 vhm64 vhm66 vhm102 vhm116 vhm162 vhm233 vhm235 vhm238 vhm144 vhm145 vhm167 Figure 1. Location of river basins. 9 l l l l l l l l l l l l l l l l l l ll l l l l l l l l l l l l l ll l l l l l 0 100 200 300 50 15 0 25 0 35 0 Days since Sept. 1st Q (m ³/s ) vhm59 S O N D J F M A M J /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 36. 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

• 37. Crochet_Philippe_CES_2010

  ≤   ≤ >− 0 00 0 )( TTif TTifTTDDFsnow   ≤ >− 0 00 0 )( TTif TTifTTDDFice Mean annual temperature difference Difference relative to 1971-2000 Difference between 25% warmest and 25% coldest years barb2right +1°C (25% warmest) barb2right -0.7°C (25% coldest) barb2right +1.7°C Catchment elevation (m.a.s.l) Catchment elevation (m.a.s.l) s n o w m e l t ( m m / d ) g l a c i a l m e l t /media/ces/Crochet_Philippe_CES_2010.pdf

• 38. vanRoosmalen_etal-2009-WRR_2007WR006760

  Impact of climate and land use change on the hydrology of a large-scale agricultural catchment Lieke van Roosmalen,1 Torben O. Sonnenborg,2 and Karsten H. Jensen1 Received 5 December 2007; revised 21 November 2008; accepted 19 January 2009; published 18 March 2009. [1] This paper presents a quantitative comparison of plausible climate and land use change impacts on the hydrology of a large-scale /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 39. ces_risk_flyer

  including, for example, ensuring dam safety. The goal of the new Climate and Energy Systems project is to look at climate impacts closer in time and assess the a n o ect ves o  t e    ro ect An evaluation of risk under increased uncertainty in order to improve decision making in a changing climate was carried out through the following steps: development of the Nordic electricity system for the next /media/ces/ces_risk_flyer.pdf

• 40. Factsheet_Bardarbunga_140908

  Conclusions of the Scientific Advisory Board of the Icelandic Civil Protection:  The eruptive activity at Holuhraun continues at similar intensity. o The eruption sites are the same as before. Lava flows to the East at similar rates as yesterday. Although the lava is now in contact with the river Jökulsá á Fjöllum, it does not reduce the lava flow rates significantly. No explosive activity /media/jar/Factsheet_Bardarbunga_140908.pdf