60 results were found for WA 0812 2782 5310 Kontraktor GreenHouse Bunga Di Sukodono Sragen.

Results:

• 51. Adalgeirsdottir-etal-tc-5-961-2011

  value of the least squares line matched the expected 2010 value based on the AR modelling of the past climate. The trend analysis of the future climate eliminates the di- rect use of a past baseline period in the derivation of the sce- narios and provides a consistent match with the recent cli- mate development. Furthermore, the statistical matching of the past climate observations with the trend /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 52. GA_2009_91A_4_Andreassen

  /media/ces/GA_2009_91A_4_Andreassen.pdf

• 53. Refsgaard_etal-2007-Uncertainty-EMS

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

• 54. 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

• 55. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  water systems impacts and socio-economic impacts (Fig. 2). The main uncertainties in the different steps are characterized (Table 1) with respect to the sources and nature of uncertainty following our above typology. In our cascading process we see that: Future greenhouse gas (GHG) emissions cannot be known with certainty because they depend on future human decisions and are characterised /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 56. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 57. Bárðarbunga 2014 - September events

  change. These values are not to be used for further research as they are preliminary and all rights to the data belong to the scientists who are acquiring and interpreting the data. The participating institutions include: Icelandic Meteorological Office, Chalmers University of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of Applied Sciences, University of Palermo /earthquakes-and-volcanism/articles/nr/3001

• 58. Bardarbunga-2014_September-events

  University of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of Applied Sciences, University of Palermo, University of Cambridge, and British Geological Survey. 18 September 2014 11:30 - from the Scientific Advisory Board Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University of Iceland along with representatives from /media/jar/Bardarbunga-2014_September-events.pdf

• 59. Bárðarbunga 2014 - September events

  change. These values are not to be used for further research as they are preliminary and all rights to the data belong to the scientists who are acquiring and interpreting the data. The participating institutions include: Icelandic Meteorological Office, Chalmers University of Technology, Istituto Nazionale di Geofisica e Vulcanologia, Düsseldorf University of Applied Sciences, University of Palermo /earthquakes-and-volcanism/articles/nr/3001/

• 60. vanRoosmalen_etal-2009-WRR_2007WR006760

  on Climate Change (IPCC) report states that global atmospheric con- centrations of greenhouse gases (GHG) have increased markedly since 1750 as a result of human activities [Intergovernmental Panel on Climate Change (IPCC), 2007]. IPCC predicts that GHG concentrations will continue to rise during the present century at rates determined by global economic development with significant impacts /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf