74 results were found for S 외국19방송 CDDC7.COM ◆보너스번호 b77◆스페치아 칼치오Ւ마포 리딩방Ử사누키☋양천 프로토 베팅ê외국19방송선정 anthropogeny/.


  • 11. Hare-2011-ParticipatoryModelling

    support ) Improv e mode l (integration) ; socia llea rnin g Farmers ,loca l aut horities , association s NO P IN D Cognitiv e mappin g HE T GM B NO P HE T Simulation - by-han d OT :Researcher s KA F F Iska r (Phas e1 ) Co n ce pt u al m o de l (D is cu ss io n su pp o rt ; Com m unication ) Improv e mode l (integration) ; socia llea rnin g Nationa l poli cy-maker s NO P IN D Cognitiv e mappin g HE /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 12. Refsgaard_etal-2007-Uncertainty-EMS

    outcomes and/or probabilities of these outcomes is the central focus. Thus according to our definition a person is un- certain if s/he lacks confidence about the specific outcomes of an event. Reasons for this lack of confidence might include a judgement of the information as incomplete, blurred, inaccu- rate, unreliable, inconclusive, or potentially false. Similarly, a person is certain if s/he /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 13. IPPC-2007-ar4_syr

    (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 14. Paper-Olafur-Rognvaldsson_92

    a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf
  • 15. Journal_of_Hydrology_Veijalainen_etal

    24 July 2010 This manuscript was handled by K. Georgakakos, Editor-in-Chief, with the assistance of Ercan Kahya, Associate Editor Keywords: Climate change Flood Hydrological modelling Flood inundation area Hydraulic modelling Finland s u m m a r y This paper provides a general overview of changes in flooding caused by climate change in Finland for the periods 2010–2039 and 2070–2099. Changes /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 16. 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
  • 17. vanRoosmalen_etal-2009-WRR_2007WR006760

    The hydraulic conduc- tivity of the sand formations is generally high, of the order of 104–103 m/s [Harrar et al., 2003; Sonnenborg et al., 2003]. In general, groundwater flows from east to west. At the water divide to the east the hydraulic head level is about 75 masl, decreasing to sea level at the west coast. The average head gradient is 0.001. The seasonal variation in head values is generally less /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 18. VI_2020_005

    exist that reach back to early 19th century but most series are much shorter (Hamlington and Thompson, 2016). In contrast, satellite altimetry has only been available since the early 1990’s. Satellite altimetry mea- sures the sea surface height, namely the sea level compared to a fixed reference frame (the center of the earth, the geoid or a reference ellipsoid) for latitudes up to 66 N and S (ESA /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 19. Group5-Stakeholders_involvement

    /EPP 2 Stakeholders analysis 26 August 2011 PM/YZ/EPP 3 Stake h o l d e r s P u b l i c / p r i v at e P o w e r l e v e l (“ n u i s an ce” ca p a c i t y ) O r i e n tat i o n H or s t e n s m uni c ipal i t y ( c o m pe t e n t a u t h ori t y ) P u b l i c S t ron g Go v ernanc e N eighbour mun i c i p ali t y P u b l i c S t ron g Go v ernanc e Poli c y /media/loftslag/Group5-Stakeholders_involvement.pdf
  • 20. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

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