41 results were found for w 성남오피타임ⓞ“otam13.com】 성남오피 성남핸플 성남건마 성남오피타임 성남오피타임.

Results:

• 21. Heavy rainfall and increased river discharge

  Warning against increased risk 25.9.2015 A low is approaching Iceland Saturday morning and high precipitation levels are forecast until early Sunday morning for much of S- and W-Iceland. Heavy rainfall is expected in the southeastern part of the country, leading /about-imo/news/nr/3197

• 22. Sea ice in March 2007

  was well within the median and closest to shore, about 50n.m. NW off Straumsnes and 60n.m. W off Barði. The ice-edge density was extensively 4/10 or less than 7-9/10 north off 67°20'N. A considerable diagenis was discovered in the southernmost part of the exploratory territory. No other dispatches were made during the month. Easterly and later northeasterly winds were common in the Greenland /sea-ice/monthly/2007/nr/2300

• 23. Sea ice in April 2011

  was seen just within the jurisdiction of Greenland. No large floes were seen on radar beyond the ice edge. No observations were received from ships but 3rd April one observation was received from land, reporting an ice berg in location 65°42' N 32°07'W. On the Greenland Straight easterlies were predominant but occasionally strong southwesterly wind prevailed for a few days /sea-ice/monthly/2011/nr/2375

• 24. ces_SA_group_flyer_new

  series analysis Regional series are compiled based on regions having similar climatological characteristics and streamflow regimes. These series are also useful for evaluating patterns and trends, both in time and by region. Regional series for precipitation, temperature and runoff are being compiled, updated and analysed within the CES project. - 4 0 - 2 0 0 2 0 4 0 6 0 W S P S U M A Q , % - 4 0 /media/ces/ces_SA_group_flyer_new.pdf

• 25. BIGJ_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 35 62 48 77 8 4 83 63 64 22 19 14 7 4 11 11 14 41 1 5 24 25 18 45 64 41 3 2 93 35 11 17 7 11 47 16 24 67 36 Wind rose BIGJ January 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 Frequency of wind /media/vedur/BIGJ_windrose_2005-2014.pdf

• 26. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf

• 27. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 28. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 29. Hare-2011-ParticipatoryModelling

  O P N O P H ET Sh o w - an d- te ll ve rif ic at io n HE T Us e by deman d OT :Researcher s M M (mode l alread yd ened )M (pa ra m er iza tio n for scenarios ) F M Wadde n Se a Conceptua lmodel s an d simulatio n mode l(DSS ) Im pr o ve m o de l (quality , acceptance , integration ) Po lic y-m ak er s N O P IN D Interview s (conceptua l models ) NO P NO P IN D Dire ct us e (of res u ltin g DSS /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

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

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf