83 results were found for 【K06.CC】陌陌半年实名男号25-30级 52kug.

Results:

• 31. 2010_003rs

  .................................................................................................... 22 2.4 Summary................................................................................................................ 25 3 Results and interpretation ............................................................................................ 27 3.1 The two large June 2000 faults /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 32. VI_2022_006_extreme

  an estimate of uncertainties. Further details can be found in Poli et al. (2016). Data from the ten realizations were retrieved for temperature, total precipitation and snow- fraction for a box around Iceland, extending between latitudes 58 to 72°N and longitudes -5 to -30°W. Data were available from the ECMWF archive at hourly resolution, but for this project, only monthly summed variables were /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 33. BIKF_windrose_2005-2014

  89 7 72 0 47 7 29 7 32 3 43 8 40 2 40 2 40 5 44 3 52 3 79 1 67 4 51 3 43 9 34 6 31 1 28 3 29 9 40 5 45 3 45 8 39 1 25 2 29 0 20 1 18 0 19 6 22 4 19 2 19 6 21 8 17 3 29 4 Wind rose BIKF May 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 1 2 3 4 5 6 7 Frequency of wind direction (%) Aerodrome Total /media/vedur/BIKF_windrose_2005-2014.pdf

• 34. PhD_course-Programme_26Aug2011-final

  Cooke and Kothare (2007) Daniell et al. (2010) Hare (2011) Coffee 14:30 - 18:00 Exersize works Students Thursday, August 25 9:00 - 10:15 Acceptability of policy LE Eriksson et al. (2006) Samuelson (1993) Coffee 10:30 - 12:30 Exercize works Students Lunch 13:30 - 14:45 Social cost-benefit analysis in the context of regional adaptation planning AP Coffee 15:00 - 18:00 Exercize works. Prepare draft /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 35. norsem_begga

  The observed travel time differences already mentioned can either be obtained from absolute times of measured (picked) phase arrivals (logged in earthquake catalogs) or as relative times between phases measured with cross-correlation (CC) of waveforms. CC between closely spaced earthquakes can give highly accurate relative time differences between phases, and can correct bad picks from /media/norsem/norsem_begga.pdf

• 36. Instructions on using Atlantic Ocean forecasts

  of the wind direction. Wind-speed is symbolised by diagonal lines at the end of the barb; a long line represents 5 m/s, a short line 2.5 m/s and a triangle represents 25 m/s. Temperature forecast: Temperature levels are shown over the Atlantic Ocean in degrees Celsius (°C) at an altitude of about 1,500 m above the ocean surface. This altitude equates to an air pressure of 850 hPa /weather/articles/nr/1218

• 37. Two TRI/TFI projects with roots in the CES collaboration funded

  networks. Two of these applications have now been funded: SVALI (Stability and Variations of Arctic Land Ice, ~40 million NOK applied for to the TRI), under the sub-programme Interaction between Climate Change and the Cryosphere of the TRI; and ICEWIND (Icing and Wind Energy Integration in Northern Norden, total budget ~25 million NOK, ~12 million NOK applied for to the TRI), under the sub-programme /ces/nr/1978

• 38. ces_cg_flyer

  -relevant indices defined in co-operation with the Statistical Analysis Package. Focus of the Climate modelling and scenarios group in CES Activities and results 1) Regional climate models are used to produce climate change scenarios at 25 km resolution. The work is done in parallel to the European fp6 project ENSEMBLES. In total more than 30 simulations with different combinations of global /media/ces/ces_cg_flyer.pdf

• 39. Hafisskyrsla-13-12-2010

  27.0N 025 40.0W 11) 66 05.0N 026 47.0W 12) 66 15.0N 028 22.0W 13) 66 00.0N 028 10.0W 14) 65 38.0N 029 12.0W Utan meginísjaðars eru ísdreifar og stærri jakar. Nokkrir borgarísjakar eru sjáanlegir, sem og stærri íshellur. Næst landi var meginísinn á eftirfarandi stöðum: 1. 53 sjml VNV af Grímsey. 2. 32 sjml NNV af Skagatá. 3. 32 sjml ANA af Hornbjargi 4. 25 sjml norður af Hornbjargi. 5. 20 /media/hafis/skyrslur_lhg/Hafisskyrsla-13-12-2010.pdf

• 40. 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