60 results were found for WA 0859 3970 0884 Pemborong Pintu Sliding Slim Frame Terpercaya Kalibawang Kulon Progo.

Results:

• 41. Refsgaard_etal-2007-Uncertainty-EMS

  /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 42. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 43. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 44. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 45. VI_2017_009

  .................................................................................................................... 7 2 Data and methods ........................................................................................................... 8 2.1 Data and time frame .............................................................................................. 8 2.2 Domain and spatial resolution /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 46. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  that attempts to tackle the realities of these complex situations. Over the last three decades, Lin has coordinated efforts to develop an overarching frame- work for institutional analysis, namely, the IAD framework (most recently elaborated in Ostrom 2005, 2007b). This framework helps organize the task confronting a scholar or pol- icy analyst approaching a policy issue by directing /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 47. Daniell_etal-2010

  the workshops. One participant stated “the whole process took place within an acceptable time frame, required an acceptable effort, and led to a good result” [6]. Achieving both tangible outputs and learning processes The third challenge concerns the possible outcomes of the participatory process. Outcomes depend on the respective goals of the process, and are influenced by both contextual and procedural /media/loftslag/Daniell_etal-2010.pdf

• 48. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  water management. Thus, as stated previously, perceptions among stakeholders may diverge considerably about what really is at stake, i.e. there exists ambiguity on how to frame the problem. The second feedback between the blocks ‘Prepare Strategy and Action Plan’ and ‘Build Commitment to Action’ deals with the process of preparing the strategy and the action plan after the gap analysis. Also /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 49. Reykholt-abstracts

  of Greenland and Antarctica appear to be driven by changes in basal sliding that are most likely caused by variations in the amount and pressure of basal water. As a part of lidar mapping of the surface of glaciers and ice caps in Iceland 2008–2012, some source areas for jökulhlaups (glacier outburst floods) have been surveyed more than once. These include the Skaftá cauldrons in western /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 50. raisanen_ruosteenoja_CES_D2.2

  of greenhouse-gas- induced climate change becomes stronger. The sensitivity of the findings to the evolution of greenhouse gas emissions was also studied, by comparing forecasts derived for the SRES B1, A1B and A2 scenarios. However, due to the relatively short time frame considered, this source of uncertainty proved to be smaller than the uncertainties arising from natural climate variability /media/ces/raisanen_ruosteenoja_CES_D2.2.pdf