41 results were found for 495455411(q)百度留痕技术彭...yw4gq5..w3j.

Results:

• 31. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  s fro m climat e ch ang e an d cr o ss bou ndar y adaptatio n measu res . In th e Netherl and s fo r hyd rodyna m ic mod el syst em s lik e SOB EK- W AQ UA (loca lleve l) an d e.g . fo rR hi ne flo w (ba sin wi de )c o n sid er ab le u n ce rta in tie s ex ist (W ee rts et al .200 3) D ev el op m en to fi nt eg ra te d ba sin m o de l( flo od ing an d poll ution) . 2: St at ist ic al /q ua lit /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 32. 2010_005_

  A conservative enhancement of the reduced IPCC ensemble mean warming rate would therefore result in 0.37 K per decade for the Icelandic elevated terrain. 17 Table 4. Linear trends of surface air temperature in Kelvin per decade between specific years in different zones (ocean / land / low terrain / high terrain). 2004–50 2004–80 2004–99 IPCC GCM Mean 0.30 / 0.31 / - / - 0.28 / 0.29 / - / - 0.23 / 0.24 /media/ces/2010_005_.pdf

• 33. VI_2009_012

  Different kinds of weights were tried in the regression process in which case the least squares problem becomes the problem of minimizing { }2102 ,...),()(log∑ − i iiii rMfPGXw , with respect to the parameters of the model f. The weights wi were generally of the form ),( rMq p wi = , where p was a normalization constant and usually q(M,r) was a discrete density distribution made to correct /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 34. ces-oslo2010_proceedings

  Resources and Energy Directorate Edited by: Heidi H. Pikkarainen Print: Norwegian Water Resources and Energy Directorate Number printed: 130 Cover design: Rune Stubrud Prepared for: The CES project Norwegian Water Resources and Energy Directorate Middelthunsgate 29 P.O. Box 5091 Majorstua N-0301 OSLO NORWAY Telephone: +47 22 95 95 95 Fax: +47 22 95 90 00 /media/ces/ces-oslo2010_proceedings.pdf

• 35. Refsgaard_etal-2007-Uncertainty-EMS

  22 (2007) 1543e1556 defined as the summed squared deviation between the calibra- tion targets (field data) and their simulated counterparts. Many software tools support inverse modelling and some universal optimisation routines can be downloaded as freeware, e.g. PEST (Doherty, 2003) and UCODE (Poeter and Hill, 1998). Most inversion techniques have the benefit that they in ad- dition to optimal /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 36. 2010_003rs

  yfir röð stórra skjálfta af stærð M 6-7 í Suðurlandsbrotabeltinu og hafa yfirborðssprungur skjálfta á nútíma verið kortlagðar víða í brotabeltinu. Stefna þverbrotabeltisnis er A-V en þó sýnir yfirborðskortlagning, ásamt kortlögðum áhrifasvæðum, að sögulegir skjálftar hafi orðið á stórum N-S sprungum. Hefur aflögun á beltinu því verið lýst með svokallaðri bókahillutektóník, þar sem það brotnar /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 37. VI_2022_006_extreme

  above 95% for the later years. This can be explained by the high elevation of the catchment and the fact that most of it is glaciated. Catchments Hraunaveita and Þingvallavatn present similar patterns with large fluctuations from one year to the other. In the case of Hraunaveita, the snow-fractions range between 65 and 97%, with only five years under 75%. For catchment Þingvallavatn, being /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 38. 2010_012rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 39. VI_2020_011_en

  : Yfirfarið af: SG Lykilsíða 5 Contents ABSTRACT .............................................................................................................................. 8 1 INTRODUCTION ............................................................................................................... 9 1.1 Long-term volcanic hazard assessment /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 40. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf