35 results were found for WA 0821 1305 0400 Anggaran Biaya Pembuatan Rumah Type 21 2 Kamar Bogor Timur Kota Bogor.

Results:

• 21. 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

• 22. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  : option a is to accept the distribution and option b is to reject it. In decision 1, the responder chooses between accepting the distribution (20,0) (20 for the sender and zero for the responder) and rejecting it; in decision 2, the choice was between accepting (19,1) and rejecting it, and so on up to decision 21 where the choice was between accepting (0,20) and rejecting it. The responder’s /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 23. VI_2015_006

  radiation flux between snow-free and snow-covered regions, under clear shies, are of the same magni- tude as differences between overcast and clear-sky conditions over the same surface type. At around noon, across the southern edge of Vatnajökull on 27 July, and across the northern edge on 3 August, for example, the net shortwave radiation flux increases from 300 W m 2 over the glacier to 500 W m 2 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 24. Forecasts - Sáta

  ° SE 7 Cloud cover: 100% 20 GMT -2° ESE 7 Cloud cover: 100% 21 GMT -2° ESE 7 Cloud cover: 100% 22 GMT -2° ESE 5 Cloud cover: 100% 23 GMT -2° S 3 Cloud cover: 100% Tue 2.05 00 GMT -3° SW 4 Cloud cover: 100% 01 GMT -4° WSW 4 Cloud cover: 100% 02 GMT -5° WSW 3 Cloud cover: 100% 03 GMT -5° WSW 2 Cloud cover: 100% 04 GMT -6 /m/forecasts/areas

• 25. Group5-Participation_stages

  1 Stakeholders involvement – Participation stages Participation stage Duration stakeholders Participatory level Type of knowledge Knowledge elicitation 1 Problem identification (Stakeholder analysis) 2 months  Horsten municipality (Competent authority) n.a 2 Information provision 2 months  Horsten municipality  Policy maker  Insurers  Neighbouring municipality /media/loftslag/Group5-Participation_stages.pdf

• 26. VI_2020_008

  to be estimated based on return periods for accumulated precipitation over a fixed timescale, which is typically 24 hours. 10. Precipitation return periods need to be translated into engineering recommendations suitable to the type of infrastructure and activity in question. From the above list, this report addresses points 1, 2, 3, 4 and 7. Point 9 is considered but not addressed completely /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 27. 2013_001_Nawri_et_al

  Office Halldór Björnsson, Icelandic Met Office Kristján Jónasson, University of Iceland 4 Contents 1 Introduction 9 2 Spatial and temporal variability of low-level wind 11 3 Methodology 13 3.1 Wind modelling . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 13 3.2 Weibull statistics . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 15 3.3 Density /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 28. VI_2022_006_extreme

  on the snowpack, temperature and melting timeseries extracted from the ICRA dataset. 17 Table 2. Difference in the beginning of the melt season (in days) for all catchments over the timespan 1979 – 2017. Catchment Difference in beginning of the melt season days Mean date Blönduvirkjun -9 01/05 Búðarháls -21 04/04 Hágöngulón -5 19/05 Hálslón 0 22/05 Hraunaveita -11 08/05 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 29. Perrels-CBA

  26.8.2011 Social cost-benefit analysis in the context of regional adaptation planning Adriaan Perrels FMI NONAM PhD Summerschool on Adaptive management in relation to climate change GEUS/FIVA Copenhagen 21-26.8.2011 26.8.2011Adriaan Perrels/IL 2 Presentation structure • Context of climate change, adaptation and infrastructure • Cost-benefit analysis in brief • The basics and metrics /media/loftslag/Perrels-CBA.pdf

• 30. Observations - Steinar

  2 Max wind : 2 / 3Road temp. : 3.1° 02 GMT 2.4° NNW 2 Max wind : 2 / 3Road temp. : 3.8° 01 GMT 1.4° NNW 1 Max wind : 1 / 3Road temp. : 4.7° 00 GMT 2.5° NNE 1 Max wind : 2 / 3Road temp. : 5.7° Sun 30.04 23 GMT 3.6° N 1 Max wind : 2 / 3Road temp. : 7.1° 22 GMT 3.8° NNE 2 Max wind : 2 / 3Road temp. : 9.4° 21 GMT 3.8° NE 1 Max wind : 1 / 2Road /m/observations/areas