57 results were found for Fethiye Sanayi Kaportacı 0535 242 15 71 Özgür Oto Kaporta.

Results:

• 11. VI_2022_006_extreme

  Methodology ...................................................................................................... 11 4.1.2 Results ................................................................................................................ 15 4.2 Change in precipitation type .......................................................................................... 18 4.2.1 Total snow /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 12. BIEG_windrose_2005-2014

  N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 778 5 1016 4 491 0 235 8 95 2 68 6 41 5 45 4 70 0 55 7 31 9 63 7 47 6 51 1 146 2 162 3 242 3 505 1 345 2 459 6 494 2 417 2 371 5 220 7 73 2 45 3 66 2 32 4 27 5 53 0 40 6 63 8 106 0 90 7 97 1 277 8 Wind rose BIEG January 2005−2014 90 80 70 60 50 40 30 /media/vedur/BIEG_windrose_2005-2014.pdf

• 13. BIVO_windrose_2005-2014

  Wind rose BIVO 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 14 Frequency of wind direction (%) Aerodrome Total observations: 14082 Calm: 18% Variable winds: 2.1% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E /media/vedur/BIVO_windrose_2005-2014.pdf

• 14. Isskyrsla_20100407

  - W022°51' 12.N67°42' -W022°10' 13.N67°42'- W022°20' 14.N67°47' -W022°08' 15.N67°46'- W021°40' 16.N67°46' -W021°37' 17.N67°38' -W021°05' 18.N67°43' -W021°02' Næst landi: 52 sml NV af Barða. 48 sml NV af Straumnesi. Hér að neðan er nákvæm staðsettning ísjaðarsins ________________________ Friðrik Höskuldsson Yfirstýrimaður 1. N65°49.46' W028°04.81' 2. N65°44.19' W027°49.00' 3. N65°42.85' W027°38.41 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 15. CES_D2.4_task1

  was observed in 1961-2008 (80% vs. 61%), whereas the difference in January is only 9% (71% vs. 62%). In absolute terms, however, the projected warming is larger in January than in April. Note that Fig. 3.1 hides the latter difference, because the horizontal axis is scaled according to the range of interannual variability. x The two observation-based distributions (1961-1990 and 1961-2008) differ /media/ces/CES_D2.4_task1.pdf

• 16. Paper-Olafur-Rognvaldsson_91

  on Langjökull ice cap, central Iceland (Björns- son et al., 2002) (see location map on Fig. 2). Here, we use measurements of (accumulated) winter mass balance, expressed in terms of liquid water equiva- lents. Björnsson et al. (1998) estimated the uncertainty of the areal integrals of the mass balance to be a minimum of 15%. Due to surging of the Dyngjujökull glacier in 1998–2000, the uncertainty /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 17. VI_2015_006

  (33%) 71 (15%) Snow-free land & Overcast 335 (35%) 46 (14%) 119 (36%) 121 (36%) 49 (14%) Snow-covered & Clear 262 (27%) 95 (36%) -15 (-6%) 43 (16%) 139 (54%) Snow-covered & Overcast 132 (14%) 19 (15%) 22 (17%) 21 (16%) 70 (52%) Ice-free ocean & Clear 624 (66%) 100 (16%) 11 (2%) 49 (8%) 464 (74%) Ice-free ocean & Overcast 430 (45%) 24 (5%) 36 (8%) 45 (11%) 325 (76%) 40 incoming radiation flux /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 18. Daniell_etal-2010

  Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Moellenkamp, S., M. Lamers, C. Huesmann, S. Rotter, C. Pahl-Wostl, K. Speil, and W. Pohl. 2010. Informal participatory platforms for adaptive management. insights into niche-finding, collaborative design and outcomes from a participatory process in the rhine basin. Ecology and Society 15(4): 41. [online /media/loftslag/Daniell_etal-2010.pdf

• 19. 2010_005_

  Björnsson, Icelandic Meteorological Office   Contents 1 Introduction 9 2 Data and Methodology 11 3 Spatial Variability of Climate Trends 13 3.1 Surface Air Temperature . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 3.2 Total Precipitation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 4 Long-Term Trends of Annual Mean Values 16 4.1 Surface Air /media/ces/2010_005_.pdf

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

  response of the glacier to an ensemble of climate change scenarios. Temperature measurements from the meteorological station Hólar in Hornafjörður (HH) and precipitation measurements from the station Fagurhólsmýri (F), (15 and 85 km away from Hoffellsjökull, respectively; locations shown in Fig. 1a), are used to force the coupled model. A sensitivity study of various model parameters and model /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf