42 results were found for WA 0821 1305 0400 Biaya Jasa Plafon Industrial Murah Cikarang Selatan Kab Bekasi.

Results:

• 31. 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

• 32. Kok_et_al._TFSC_published_2011

  is stimulated in areas with enough water, supported by additional storage capacity and irrigation systems. By 2050, water supply for agriculture is secured. Closely linked to this is an improved efciency for industry. A changed industrial policy aims to get basic production back in the EU and works on diversication. This triggers tensions between the aim for reduced water use and the overall increase /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 33. Lorenzoni_Pidgeon_2006

  of these, global warming was ranked ninth (based upon the percentage of respondents who worried about it ‘a great deal’ in comparison to the other environmental concerns). This trend has been fairly consistent (Brechin, 2003, p. 113). According to the EB 58.0 of 2002, the most worrying environmental risks for most European respondents were associated with nuclear power and radioactive waste, and industrial /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 34. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 35. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  Most of the heatstroke deaths reported have been associated with occupational exposure at construction sites, agricultural settings, and hot industrial jobs requiring heavy work. In addition, outdoor urban workers may also be exposed to additional heat stress as a result of the ‘urban heat island effect’ of the urban built environments. The research includes field studies of work places in India /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 36. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  and a valuable source of water for the socio-economically important parts of the basin. The Rhine’s water resources and land area are mainly used for industrial and agricultural purposes, for the generation of energy, for the disposal of municipal wastewater, for recreational activities, and for providing drinking water. The main issues in the Rhine basin are pollution and flooding. From being /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 37. VI_2017_009

  2005 until 2100 and select two periods as a focus of this study; the mid-century (2041-2060) and the late-century (2081-2100). Furthermore, we choose RCP4.5 and RCP8.5 as emission scenarios. The numbers 4.5 and 8.5 indicated the possible radiative forcing in W/m2 in the year 2100 compared to pre- industrial values, and are a measure of the strength of the anthropogenic greenhouse effect /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 38. 2010_005_

  Coupl. Glob. Clim. Mod., Canadian Centre for Climate Modelling and Analysis, Victoria CSIRO MK 3.5 Glob. Clim. Mod., Commonwealth Scient. and Industrial Res. Organisation, Australia MIROC 3.2 Medres Model for Interdiscip. Res. on Clim., Division of Climate System Research, Tokyo, Japan MIUB Echo G Coupled Circulation Model, Meteorological Institute of the University of Bonn, Germany MPI ECHAM5-r3 /media/ces/2010_005_.pdf

• 39. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  –2°C, relative to the pre-industrial level, in the near future and by approximately 2–3°C towards the end of the century. The largest temperature increase is expected during winter. Equivalent projections for the mean annual precipitation show a small increase in the short term, becoming more pronounced in the long term. The strongest positive precipitation response is seen during winter, whereas /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 40. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf