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  • 1. IPPC-2007-ar4_syr

    a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 2. GA_2009_91A_4_Andreassen

    ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 3. VI_2015_006

    ....................................................................................... 10 3 September 2012 .................................................................................. 12 3 Radiation fluxes at the surface ....................................................................... 16 4 Heat fluxes at the surface .............................................................................. 21 5 Net energy /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 4. VI_2015_005

    decreasing over the other maritime regions. Simultaneously, the percentage of continental 18 Table 1. Seasonal cyclone density [cyclones per season per 1000 km 1000 km] over the ocean / land areas in different sectors, for daily averages, as well as for 5-day and 31-day running means (RM) of daily grid-point time-series. Percentages measure cyclone density over land relative to that over the ocean. Time /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 5. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    la tio ns hi ps be tw ee n di ffe re nt dis cipline s = > bro ad inte grate d outp ut (bu tn o tq ua nt ita tiv e) Pr ogres s towa rd sIWR M measu re s Ind icator s o fe ffec to f measu res , invo lvin g m o n ito rin g M ul tip le fra m es (so cia l sy st em ):w at er u se s su ch as n av ig at io n , hy dr o ele ct ric po w er ge n er at io n , flo o d pr o te ct io n m u st be ha rm o n ize d w /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 6. PhD_course-Programme_26Aug2011-final

    PA (2007) Uncertainty in the environmental modelling process – A framework and guidance. Environmental Modelling & Software, 22, 1543-1556. http://dx.doi.org/10.1016/j.envsoft.2007.02.004 Milly PCD, Betancourt J, Falkenmark M, Hirsch RM, Kundzewicz ZW, Lettenmaier DP, Stouffer RJ (2008) Stationarity Is Dead: Whither Water Management. Science, 319, 573-574. Case study material Henriksen HJ /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
  • 7. ces-oslo2010_proceedings

    anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf
  • 8. Machguth_Horst_CES_2010

    experiments with different RCM’s • explore RCM biases • apply a different mass balance model data 2 RCM’s • HIRHAM4, Scenario A1B, 25 km, 1950-2100, Greenland • RCAO, Scenario A1B, 50 km, 1960-2100, Pan-Arctic 4 Weather Stations (Ta, Sin) • GC-Net Swiss Camp: 1150 m a.s.l. (1995 – 2006) • GC-Net Crawford: 2020 m a.s.l. (1995 – 2006) • Asiaq Station 437: 300 m a.s.l. (1983 – 2006) • DMI Illulisat /media/ces/Machguth_Horst_CES_2010.pdf
  • 9. VI_2015_007

    5 Days since 1st sep. n o rm al ise d Q, W S, SW E Q WS SWE vhm148 S O N D J F M A M J J A 0 100 200 300 0 1 2 3 4 5 Days since 1st sep. n o rm al ise d Q, W S, SW E Q WS SWE vhm149 S O N D J F M A M J J A 0 100 200 300 0 1 2 3 4 5 Days since 1st sep. n o rm al ise d Q, W S, SW E Q WS SWE vhm205 S O N D J F M A M J J A 0 100 200 300 0 1 2 3 4 5 Days since 1st sep. n o rm al ise d Q, W S /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
  • 10. Joining forces in weather forecasting and climate research

    of how climate change will impact our countries” says Árni.A sustainable solution Powered entirely by Icelandic hydropower and geothermal energy sources and taking advantage of the local tempered climate for keeping the supercomputer components cool, the running costs and CO2 footprint will be kept to a minimum, saving tonnes of CO2 in line with the four nations' efforts towards reaching Net /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

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