66 results were found for Saklıkent Hotels | 0534 512 68 98 | Tlos Butik Otel.

Results:

• 11. The weather in Iceland in 2020

  141 -0.5 Hjarðarland 3.9 # 21 30 -0.6 Hveravellir -0.2 0.9 25 56 -0.5 Eyrarbakki 4.8 0.8 34 128 -0.3 Keflavíkurflugvöllur 4.9 0.5 32 68 -0.5 The annual mean was highest 6.3°C in Surtsey, off the Southern coast and at Steinar near the South coast. The annual mean was lowest -1.7°C at Gagnheiði /about-imo/news/the-weather-in-iceland-in-2020

• 12. ces-oslo2010_proceedings

  ...................................................................... 66 Roald, L.A., Beldring, S. and Engen-Skaugen, T. Long term variability and projection of shifts in the streamflow at selected catchments in Norwegian rivers induced by climate change .................................................................................................................................... 68 Wilson, D., Roald, L.A., Lawrence, D /media/ces/ces-oslo2010_proceedings.pdf

• 13. Publications 2014

  on the combined use of a hydrological model and an analogue method Philippe Crochet 68 2,8 2014-005 Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland Nikolai Nawri 31 12 2014-001 Flood frequency estimation for ungauged catchments in Iceland by combined hydrological modeling and regional frequency analysis Philippe Crochet & Tinna /about-imo/publications/2014/

• 14. 47th Nordic Seismology Seminar

  International Airport (KEF) to the BSÍ bus terminal in central Reykjavík. Additional prepaid service from BSÍ in smaller vehicles to some major hotels and guest houses in Reykjavík is possible. Flybus Reykjavík Excursions AirportExpressBus Iceland Excursions The company found by the first link (Reykjavík Excursions), operates more frequently and faster between the airport and central Reykjavík. If you /norsem/norsem2016/transportation/

• 15. Practical information

  on flightbus is given at Reykjavik Excursions. Accommodation Rooms have been pre-reserved at special price at Grand Hotel. Please confirm your own reservation at johann@grand.is and the reference is NONAM. Reservations have to be made before August 10th to use this promotion. Other hotels are available in the vicinity. Social Programme On Thursday the 26th of August we will have a small /nonam/workshop/information/

• 16. VI_2022_006_extreme

  77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 17. VI_2019_009

  .............................. 41 39 From left to right, the horizontal axis has the following SYNOP codes (in groups): 21 - 60,61 - 62,63 - 64,65 - 68 - 80 - 81 - 82. ................................................ 42 40 From left to right, the horizontal axis has the following SYNOP codes (in groups): 22 - 26 - 27,87 - 70,71 - 74....................................................................... 43 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 18. isskyrsla_14122010

  Hafísskýrsla TF-SIF 14. desember 2010 Flug nr. 17610.025 Óformleg ískönnun 14. desember 2010 Óformleg ískönnun var gerð og kom eftirfarandi í ljós. Ísröndin samkvæmt ratsjá TF-SIF 1) 68 03.0N 17 19.0W 2) 67 41.0N 18 19.0W 3) 67 36.0N 19 09.0W 4) 67 21.0N 19 43.0W 5) 66 53.0N 20 21.0W 6) 66 45.0N 19 58.0W 7) 66 38.0N 20 42.0W 8) 67 02.0N 21 /media/hafis/skyrslur_lhg/isskyrsla_14122010.pdf

• 19. norsem_mantyniemi

  Macroseismology in Finland from the 1730s to the 2000s: From an obligation of the learned elite to citizen science Päivi Mäntyniemi Institute of Seismology, Department of Geosciences and Geography, P.O. Box 68, FI-00014 University of Helsinki, Finland, e-mail: paivi.mantyniemi@helsinki.fi The presentation is based on a snapshot of macroseismology in Finland from the 1730s to the 2000s that has /media/norsem/norsem_mantyniemi.pdf

• 20. vanRoosmalen_etal-2009-WRR_2007WR006760

  occurring during winter from 86% in the present climate to 98% in the year 2100. High evapotranspiration during summer was mainly attributed to forests because forests were able to utilize most of the increase in soil moisture storage that came from winter recharge. For future studies Woldeamlak et al. [2007] suggested use of transient models to study seasonal varia- tions of the groundwater /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf