82 results were found for f 부산진주점㏉（dm080.com》♦부산진건마●부산진주점 부산진휴게텔✭부산진휴게텔.

Results:

• 61. VI_2013_008

  systematically underestimated. The bias is not as pronounced for the non glacial rivers. Com- bining synoptic-scale and basin-scale predictors (method 3) leads to a substantial improvement compared to the use of MSLP fields alone (method 1). Analogue forecasts become similar or better than persistence, depending on catchment and lead time. Usually, persistence performs better for T=1 day and then method 3 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 62. 2010_003rs

  Use of relatively located micro- earthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland Sigurlaug Hjaltadóttir VÍ 2010-003 Skýrsla   f l l l dUse o re ative y ocate micro- earthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland Sigurlaug Hjaltadóttir, Veðurstofu Íslands VÍ 2010-003 ISSN 1670-8261 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 63. VI_2015_007

  study and location of catchments. Catchment vhm278 is embedded within vhm148 and catchment vhm277 is embedded within vhm149. 9 l l l l l l ll l l l l l l l l l l l l ll l l l l l l ll l ll l l l l l l 0 100 200 300 10 0 20 0 30 0 40 0 Day since 1st Sept. Q m³ /s VHM 148 S O N D J F M A M J J A l l ll l l l ll l l l ll l l ll l l 0 100 200 300 15 0 25 0 35 0 45 0 Day since 1st Sept. Q m³ /s VHM /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 64. Refsgaard_etal-2007-Uncertainty-EMS

  and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 65. 2013_001_Nawri_et_al

  rather than from the data directly. This reduces the amount of data that needs to be disseminated to a few parameters, that describe each wind speed distribution. Of the various probability density functions for boundary-layer wind speeds, s, the 2-parameter Weibull distribution, f (s;A;k) = k A s A k 1 exp s A k ; (1) is the one most commonly employed for wind energy studies (Morgan /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 66. Dataseries and components

  Analysed components - IMO's research: Sulphur and salinity measurements: Precipitation: SO4-S, NO3-N, Cl, Na, Mg, K, Ca (mg/l) Precipitation: conductivity (µS/cm), quantity (mm), pH Aerosol: SO4-S, Cl, Na, Mg, K, Ca, Fe (µg/m3) Air: SO2-S (µg/m3) Heavy metals in precipitation: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/ml) Cl, NO3-N, SO4-S, Na, K, Ca, Mg, NH4-N, Br, F (µg/ml) conductivity (µS/cm /pollution-and-radiation/pollution/components/

• 67. Hydropower, Hydrology

  Førland, E.J., Roald, L.A. (2008). Climate change impacts on hydrological processes in Norway based on two methods for transferring regional climate model results to meteorlogical station sites. Tellus Series A: Dynamic Meteorology and Oceanograph, 60, 439-450 (pdf). Jónsdóttir, J. F. (2008). A runoff map based on numerically simulated precipitation and a projection of future runoff in Iceland /ces/publications/nr/1938

• 68. AnneFleig_May2010_CES

  c h I n s t i t u t e , D e n m a r k CES conference, Oslo, Norway, 31 May - 2 June 2010 -6 -4 -2 0 2 4 5 0 5 2 5 4 8 9 10 11 12 5 4 . 5 5 5 . 0 D a t a s o u r c e : C e n t r e f o r E c o l o g y a n d H y d r o l o g y , U K D a t a s o u r c e I n s t i t u t e , D e n m a r k • 37 British and 22 Danish stations; • natural or naturalized daily streamflow data /media/ces/AnneFleig_May2010_CES.pdf

• 69. Cradden_Lucy_CES_2010

  Capacity (A) F r e q u e n c y control future +0.4std dev (as % of mean) -0.68max -8.32min -1.74mean % change June 2010 15 Time series 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year of control period Seasonal average rating Calculated capacity 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year under future scenario Calculated capacity Seasonal average /media/ces/Cradden_Lucy_CES_2010.pdf

• 70. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  Surface 110, F04001, doi: 10.1029/2005 JF000289. Adalgeirsdo´ttir G., Jo´hannesson T., Bjo¨rnsson H., Pa´lsson F. & Sigurdsson O. 2006. Response of Hofsjo¨kull and southern S. Gudmundsson et al. Mass balance of three ice caps in southern Iceland Citation: Polar Research 2011, 30, 7282, DOI: 10.3402/polar.v30i0.7282 9 (page number not for citation purpose) Vatnajo¨kull, Iceland, to climate change /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf