82 results were found for D 정보이용료현금화 [문의카톡 1SEC] 티켓타카 E 정보이용료현금화 전문 포탈 콘텐츠이용료현금👫couchant/.

Results:

• 71. Journal_of_Hydrology_Veijalainen_etal

  the largest floods and scenarios with large temperature increases (No. 7–9, HadCM3) produce the small- est floods. The catchment characteristics and current hydrological proper- ties can be used to explain the results and their correlations with the average changes in 100-year floods by 2010–2039 and 2070– a Reference Period 1971−2000 2070−2099 Maximum scenario 2070−2099 Minimum scenario b c d e 0 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 72. VI_Arsskyrsla_2018_vef

  Forsíðumynd: Svava Björk Þorláksdóttir mælir með öldustilli niður á festur í Iðu í Hvítá. Ljósmynd: Njáll Fannar Reynisson. V E Ð U R S T O F A Í S L A N D S / Á R S S K Ý R S L A 2 0 1 8 3 Viðburðaríkt ár er að baki hjá starfsfólki Veðurstofunnar enda felast jafnan margar og fjöl breyttar áskoranir í vöktun og rannsóknum á náttúru - öflum landsins. Loftslagsmál eru mjög á döfinni enda stærsta /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 73. vanRoosmalen_etal-2009-WRR_2007WR006760

  1998] and RCM output such as incoming and outgoing, short- and long-wave radiation, temperature, water vapor pressure, and wind speed: ETref ¼ 0:408D Rn
  Gð Þ þ g 900T þ 273 u2 es
  eað Þ Dþ g 1þ 0:34u2ð Þ ð3Þ where ETref is reference evapotranspiration (mm d
  1), Rn is net radiation at the crop surface (MJ m
  2 d
  1), G is soil heat flux density (MJ m
  2 d
  1), T is mean daily air temperature at 2 m /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 74. VI_2017_009

  and glaciers. The former trend is mainly visible in the Westfjords, an area in northwest Iceland, in the winter (see Figure 8a and 8b) and in northeast Iceland in the summer, especially east of Akureyri in the RCP8.5 scenario (see Figures 8c and d). The latter trend is most clearly seen during summer and in cases with the RCM RCA4 with RCP8.5. Extreme temperature trends In a previous section we /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 75. Forecasts - Skarðsfjöruviti

  Forecasts - Skarðsfjöruviti | Station forecasts | Icelandic Meteorological office Forecasts - Skarðsfjöruviti Mon 1.05 14 GMT 8° E 5 Cloud cover: 100% 15 GMT 8° E 6 Cloud cover: 100% 16 GMT 7° E 5 Cloud cover: 100% 17 GMT 7° E 6 Cloud cover: 100% 18 GMT 7° E 6 Cloud cover: 100% 19 /m/forecasts/areas

• 76. 2005EO260001

  Dashed lines encompass the V-shaped zone of tephra deposition. (c) Oblique aerial view from west of the tephra plume at Grímsvötn on 2 November. Note the ashfall from the plume. (Photo by M. J. Roberts.) (d) Weather radar image at 0400 UTC on 2 November. The top portion shows its projection on an EW-vertical plane. The minimum detection height for Grímsvötn is seen at 6 km, and the plume extends /media/jar/myndsafn/2005EO260001.pdf

• 77. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  Communication Washington, DC Marx S, Weber E, Orlove B, Leiserowitz A, Krantz D, Roncoli C, Phillips J (2007) Communication and mental processes: Experiential and analytic processing of uncertain climate information. Glob Environ Chang 17(1):47–58 Moser SC, Dilling L (2004) Making climate hot: communicating the urgency and challenge of global climate change. Environment 46:32–46 Moser S, Dilling L /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf

• 78. ces-glacier-scaling-memo2009-01

  Energy Sources: Their role in the Nordic energy system. Copenhagen, Nordic Council of Ministers, Nord 2007:003. Harrison, W. D., D. H. Elsberg, K. A. Achelmaeyer and R. M Krimmel. 2001. On the charac- terization of glacier response by a single time-scale. J. Glaciol., 47(159), 659–664. Jóhannesson, T., G. Aðalgeirsdóttir, H. Björnsson, P. Crochet, E. B. Elíasson, S. Guðmundsson, J. F. Jónsdóttir, H /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 79. CES_D2.4_solar_CMIP3

  incident solar radiation with observations. Red squares: the baseline period (1971-2000) mean of the global radiation observed at Jokioinen in southwestern Fin- land (60.8◦N, 23.5◦E) for each calendar month. The thick black curve: the corresponding quantity as an average of the simulations performed with 18 global climate models. Grey shaded area: mean ± standard deviation of the simulations /media/ces/CES_D2.4_solar_CMIP3.pdf

• 80. Adalgeirsdottir-etal-tc-5-961-2011

  The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ doi:10.5194/tc-5-961-2011 © Author(s) 2011. CC Attribution 3.0 License. The Cryosphere Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland G. Aðalgeirsdóttir1,2, S. Guðmundsson1, H. Björnsson1, F. Pálsson1, T. Jóhannesson3, H. Hannesdóttir1, S. Þ. Sigurðsson4, and E. Berthier5 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf