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

Results:

• 41. 2010_005_

  experiments with the GISS climate model (Hansen et al., 1983, 1984). Differences between the 1 CO2 and 2 CO2 equilibrium experiments were used to estimate greenhouse effects. Interpolated to Stykkishólmur, the warming annually was about 4 C, but ranging over the course of the year between 4.1–4.3 C from November to April, and between 3.6–3.8 C from June to September. Thus the wintertime warming exceeded /media/ces/2010_005_.pdf

• 42. Journal_of_Hydrology_Veijalainen_etal

  The hydrological simulations were performed with the Wa- tershed Simulation and Forecasting System (WSFS) developed and operated in the Finnish Environment Institute (Vehviläinen et al., 2005). The WSFS is used in Finland for operational hydrolog- ical forecasting and flood warnings (www.environment.fi/water- forecast/), regulation planning and research purposes (Vehviläinen and Huttunen, 1997 /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 43. VI_Arsskyrsla_2018_vef

  by the inhabitants on a daily basis for driving between towns and villages for work, school, hobbies or di?erent services. Public avalanche bulletins are also published for selected areas, aimed towards the increasing number of backcountry travellers in Iceland during winter time. The number of human-triggered avalanches recorded by the Meteorological O>ce has increased substantially over /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 44. 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

• 45. VI_2022_006_extreme

  Intercomparison Project (CMIP) is a large framework that collects the output from global coupled ocean-atmosphere general circulation models (GCMs) to project future climatic changes due to anthropogenic activity. For this project, results from the fifth 10 phase of the project (referred to as CMIP5; for details, see Taylor et al., 2012) are used based on two different greenhouse gas /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 46. VI_2014_005

  with vertical boundary-layer profiles calculated di- rectly from HARMONIE model levels. Due to the temporal and spatial variability of model level heights, for the calculation of average vertical profiles, individual model profiles above 6The large positive bias northeast of Vatnajökull is due to the unusually cold summertime temperatures measured at Station 5932, situated near the edge /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 47. Keskitalo_et_al-MLG_and_adaptation_FINAL

  /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 48. VI_2016_006_rs

  in a collaboration between the Austrian engineering company Ingenieurbüro Illmer Daniel e.U. (DI), Efla consulting engineers and the Icelandic Meteorological Office (IMO). Daniel Illmer carried out the analysis of landslide protection measures, Jón Kristinn Helgason, Tómas Jóhannesson and Eiríkur Gíslason wrote sections about the geographical setting, the land- slide history and the assessment /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 49. VI_2015_007

  with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D. The index flood, µi(D), is modelled at each site i as a continuous function of D, as follows: 12 µi(D) = µi 1+(D=Di)li ; (6) where µi, Di and li are basin dependent parameters /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

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

  of greenhouse gases. Then again, this will most probably hit the most vulnerable harder because of their exposure and least adaptive capacity. - Developing countries will be most affected as most countries are in tropical and sub-tropical regions. In addition, many workers lack work security and are paid according to output and as a result, workers might in the future have to work longer hours /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf