57 results were found for WA 0812 2782 5310 Vendor Neon Box Menu Restoran Salatiga.

Results:

41. NONAM_1st_workshop_summary_v3

planning The set of seven questions is presented below in the text box. The synthesis of the discussion is however not purely organized in seven steps, as many issues re-appeared in the answering of different questions. Furthermore, various questions, notably no.1 and 2 require in fact joint consideration or stepwise answering, implying that the questions should be several times revisited /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
42. Hare-2011-ParticipatoryModelling

ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
43. VI_2009_006_tt

than can be expected to originate from the cauldrons, three to four times the wa- ter equivalent of the accumulation of snow over the watershed of the cauldrons. It has been estimated that flow from the cauldrons, in addition to the jökulhlaups, could be 2–5 m3 s 1 at maximum (Vatnaskil, 2005). It is possible that part of the sulfate-rich groundwater from the glacier comes from the cauldrons /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
44. Kok_JGEC658_2009

scenario development, with an example from Brazil Kasper Kok * Land Dynamics, Department of Environmental Sciences, Wageningen University, P.O. Box 47, 6700 AA Wageningen, The Netherlands 1. Introduction The world is undergoing rapid changes while globalising constantly, which gives the consideration of the future new urgency and importance. Scenario development has emerged as a key method when taking /media/loftslag/Kok_JGEC658_2009.pdf
45. Refsgaard_etal-2007-Uncertainty-EMS

equations are valid only if the following conditions are met: (1) the uncertainties have Gaussian (normal) distribu- tions; (2) the uncertainties for non-linear models are relatively small: the standard deviation divided by the mean value is less than 0.3; and (3) the uncertainties have no significant covariance. The error propagation equations for the most common oper- ators can be seen in Box 1 /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
46. VI_2014_005

), and the National Energy Authority (Orkustofnun). 3 Model terrain and surface type The HARMONIE model dominant surface type and terrain elevation are shown in Figures 1 and 2, respectively. Surface type is specified in SURFEX by the global land surface database ECOCLIMAP-I (Champeaux et al., 2005). Within each grid box, ground coverage is represented by fractions of one for each category of surface type /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
47. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

should be incorporated into decision support systems and tools to capture the and the complexity of water management as it is seen from different mental frames and interest group positions should be used in adaptive water management. The broad range of tools available for integrated water resource management (IWRM) includes e.g. GWP Tool- box, HarmoniCA/Catchmod tools, decision support sys- tems /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
48. 2010_005_

/media/ces/2010_005_.pdf
49. Adalgeirsdottir-etal-tc-5-961-2011

the location of the mass balance stakes at Breiðamerkurjökull (Bre). The red box indicates the posi- tion of the frame to the right. (C) Hoffellsjökull surface topography in 2001. The ice divide and the model domain are indicated with the red curve enclosing a glaciated area of ∼212 km2 in 2001. Black triangles show the locations of automatic weather stations on the glacier. N is the location /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
50. CES_D2.4_task1

1 Probability distributions of monthly-to-annual mean temperature and precipitation in a changing climate (CES Climate Modelling and Scenarios Deliverable D2.4, task I) Jouni Räisänen Department of Physics, P.O. Box 48, FI-00014 University of Helsinki, Finland Email: jouni.raisanen@helsinki.fi 17 November 2009 AVAILABLE FROM: http://www.atm.helsinki.fi/~jaraisan/CES_D2.4 /media/ces/CES_D2.4_task1.pdf