60 results were found for Seydikemer Merkez Otelleri | 0534 512 68 98 | Tlos Butik Otel.

Results:

• 51. VI_2015_007

  –3736. Jenkinson, A.F. (1955). The frequency distribution of the annual maximum (or minimum) of meteorological elements. Quart. J. R. Met. Soc. 81, 158–171. Jingyi, Z. & Hall, M.J. (2004). Regional flood frequency analysis for Gan-Ming river basin in China. J. Hydrol., 296, 98–117. Kjeldsen, T.R. & Jones, D. (2007). Estimation of an index flood using data transfer in the UK. Hydrol. Sci. J., 52(1 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 52. VI_2009_013

  Volcanol. 68: 377–393. Doi:10.1007/s00445-005-0020-y. Rögnvaldsson, S. Th. and R. Slunga (1993). Routine fault plane solutions for local networks: a test with synthetic data. Bull. Seism. Soc. Am., 83, 4, 1232–1247. Rögnvaldsson, S. Th. and R. Slunga (1994). Single and joint fault plane solutions for microearthquakes in South Iceland. Tectonophysics, 237, 73–86. Scholz, C. H. (1988 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 53. VI_Arsskyrsla_2018_vef

  /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 54. VI_2017_009

  % 20% Langjökull 42% 81% 21% Mýrdalsjökull 38% 74% 17% Reykjavík 23% 45% 4% Vatnajökull 89% 98% 47% 2081–2100 RCP4.5 Akureyri 25% 52% 11% Langjökull 28% 61% 10% Mýrdalsjökull 23% 49% 13% Reykjavík 15% 24% 1% Vatnajökull 70% 81% 22% 2081–2100 RCP8.5 Akureyri 17% 41% 5% Langjökull 21% 43% 5% Mýrdalsjökull 18% 40% 7% Reykjavík 11% 19% 0.5% Vatnajökull 65% 75% 18% 4.2 Precipitation /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 55. GA_2009_91A_4_Andreassen

  Fokstua to Fokstugu in 1968 reveals thatthe model underestimates winter balance in the firstperiod 1948/49–1967/68, the rmse is noticeablyhigher in this period (0.33 m w.e.), than in the sec- Fig. 7. Reconstructed winter and summer balance of Storbreen (1896) for years 1924–1948 and modelled and measured winter balanceand summer balance for Storbreen for years1949–2006. Pw Bulken and Pw Røldal /media/ces/GA_2009_91A_4_Andreassen.pdf

• 56. VI_2009_012

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 57. Journal_of_Hydrology_Veijalainen_etal

  /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 58. 2010_012rs

  2006), as well as the fault of a M 4.6 earthquake near to the station kri in March 2006. 27 Figure 3. (Upper) A map showing the Hengill- and Ölfus test area. (Lower) A vertical cross section, viewed from the south. Pink circles show the 1997–98-library events, orange circles show library events from 2000 and green circles show 2008-library events. The red stars show location of two M>5 /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 59. VI2010-006_web

  tímabilið 1949–2009. T P1d P2d P3d P5d 1 22 29 35 43 2 26 35 41 51 5 32 43 50 61 10 36 49 56 68 20 40 55 62 75 50 46 62 71 85 og 5 daga tímabil fyrir veðurstöðina á Akureyri. Taflan sýnir úrkomu sem svarar til 1, 2, 5, 10, 20 og 50 ára endurkomutíma, þ.e. tölfræðileg greining bendir til að úrkoma verði ekki meiri en sem nemur gildunum í töflunni oftar en endurkomutíminn segir til um þegar til langs /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 60. VI_2014_006

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf