Note
Considerable increased run-off in the Fjallabak area, around Mýrdalsjökull and on SE-Iceland. More
Yellow alert for weather: South Iceland and Southeast Iceland More

78 results were found for WA 0821 1305 0400 Borongan Pekerjaan Pintu Spandrel Aluminium Ukuran Standard Koja Jakarta Utara.

Results:

51. Group4

of the road network with no major technical alterations in personal mobility, continued provision of standard levels of service and capacity expansion goals. No significant focus on creating more adaptive management processes within the Road Authority. Pros: few institutional/cultural changes required, cost savings from avoiding new infrastructure to accommodate CC impacts. Cons: potentially /media/loftslag/Group4.pdf
52. 2010_005_

ensemble mean SAT values during the 1961–90 control period. The exact values of linear SAT trends, determined by least-squares regression, are given in Table 4. Based on a standard t-test, all these trends are significantly different from zero on the 99.9% confidence level. As seen before, based on the reduced IPCC ensemble mean, differences in linear SAT trends over the ocean and the land are small /media/ces/2010_005_.pdf
53. Eriksson_Garvill_Nordlund_2006

The problem awareness variable had a high internal consistency (a ¼ 0:95). 3. Results 3.1. Descriptive analysis of values, beliefs, and norms In Table 2, means and standard deviations for pro- environmental orientation, problem awareness of private car use, personal norm, and willingness to reduce car use are shown. The sample was to some extent pro-environ- mental, and car use was perceived /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
54. VI_arsskyrsla2020

) in 1956. During that time that ambitions of utilizing hydropower had changed from providing the public and the sectors with electricity to aim for a large-scale utilization of hydropower for energy intensive industries. This came to fruition in 1969 with the first aluminium smelter in Iceland. Today, energy intensive industry matches fisheries as a key income sector for Icelandic society. During /media/vedurstofan-utgafa-2020/VI_arsskyrsla2020.pdf
55. VED_AnnualReport-2013_screen

of these projects, we have improved our earthquake, strain and GPS monitoring systems in collaboration with Icelandic and international partners, despite considerable cuts being made to our budget. Hydrological monitoring has improved significantly and the standard of the monitoring is now comparable to the weather and earth hazard monitoring. Hydrological models are in develop- ment /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf
56. 2011_005

Skógarheiði Trimble NetRS 64,640 ISK STE2 Steinsholt Trimble NetRS 55,509 ISK STKA Stóra Kjalalda Trimble NetRS 114,951 ISK SOHO Sólheimaheiði Trimble 4700 142,736 ISK Total 842,000 ISK When the numbers are summed up in Table 8 and 9, the figures are way too high compared to standard 3G connection /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
57. 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
58. 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
59. vanRoosmalen_etal-2009-WRR_2007WR006760

The precipitation is corrected for wetting and aerodynamic effects using the standard correction methods of Allerup et al. [1998]. The average precipitation in the area equals 1073 mm/a. ETref is calculated using the Makkink [1957] formula, and has an average value of 570 mm/a. The average annual temperature is 8.2C with a maximum of 16.5C in August and a minimum of 1.4C in January. [12] The central /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
60. Adalgeirsdottir-etal-tc-5-961-2011

of the sections and the terminus position at the different times. Fig. 5. Winter, summer and annual balance measured at Hoffellsjökull and Breiðamerkurjökull. Measurements from the 1930s expedition (at the lowest stakes only annual balance was measured and therefore winter balance set to zero) are shown with black symbols. The red dots show the average and standard deviation of the mass balance /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf