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

Results:

• 31. Refsgaard_2-uncertainty

  ( % ) A2 B2 Future climate Down- scaling Bias correction Global 100-250 km Scale Regional 10-25 km Hydrological 50-500 m Present climate Climate change impacts on hydrology The cascade of uncertainties Models • Emission scenarios IPCC Greenhouse Gas Emission Scenarios Future climate Down scaling Bias correction Global 100-250 km Scale Regional 10-25 km Hydrological 50-500 m Present climate /media/loftslag/Refsgaard_2-uncertainty.pdf

• 32. VED_AnnualReport-2013_screen

  ; from which extensive data streams enter IMO and are utilized for forecasts and research purposes. Dissemination The main dissemination of IMO is in the form of forecasts and warnings; through radio, T V, direct di- alog with stakeholders and through IMO‘s web-site (vedur.is). Additionally, the web provides compre- hensive real-time data on the weather, earthquakes and deformation, as well /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 33. Paper-Olafur-Rognvaldsson_92

  ) and Jónsdóttir (2008). Therefore, comparison of measured and simulated water balance cannot be di- rectly used for validation of the model-generated precipitation. According to the non-scaled MM5 output for the period 1961–1990, mean precipitation for the whole of Iceland was 1790 mm y−1. After scaling the precipitation, this value was reduced to 1750mm y−1, i.e. by approximately 2%. This difference /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 34. 2010_016

  the largest runoff peak of the year. Compared to the period 1961–1990, a warming of about 1°C has already been observed for both watersheds during the period 2000–2009, causing considerable discharge changes in the same direction as the predicted future changes. 8 2 Introduction Increased concentration of greenhouse gases in the atmosphere is predicted to lead to changed climate (IPCC, 2007 /media/ces/2010_016.pdf

• 35. Climate Report

  main IPCC emission scenarios results on changes in temperature and precipitation in the above region surrounding Iceland where extracted from the CMIP5 model archives and examined. The scenarios range from a warm business-as-usual-case (RCP8.5) to an extensive reduction in greenhouse gas emissions (RCP2.6), resulting in only modes warming rates. For the middle of the century, the ensemble /climatology/iceland/climate-report

• 36. Climate Report

  main IPCC emission scenarios results on changes in temperature and precipitation in the above region surrounding Iceland where extracted from the CMIP5 model archives and examined. The scenarios range from a warm business-as-usual-case (RCP8.5) to an extensive reduction in greenhouse gas emissions (RCP2.6), resulting in only modes warming rates. For the middle of the century, the ensemble /climatology/iceland/climate-report/

• 37. VI_2021_008

  /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 38. 2013_001_Nawri_et_al

  /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 39. VI_2014_001

  at each site i 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 (see Crochet, 2012c). The index flood µi(D), is modeled at each site i as a continuous function of D, as follows: µi(D) = µi 1+(D=Di)li ; (5) where µi, Di /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 40. VI_2020_011_en

  Veðurstofa Íslands 2 Almannavarnadeild Ríkislögreglustjóra 3 Jarðvísindastofnun Háskólans 4 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Bologna 5 Istituto Nazionale di Geofisica e Vulcanologia (INGV), Pisa 6 Jarðvísindadeild Háskóla Íslands 7 Agricultural University of Iceland 8 Consultant Skýrsla nr. Dags. ISSN Opin Lokuð VÍ 2020-011 Desember 2020 1670-8261 Skilmálar: Heiti skýrslu /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf