70 results were found for [77AGG. COM]pohonmas slot slot deposit 1000 perang88 slot puma33 slot lth.

Results:

• 41. IPPC-2007-ar4_syr

  Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

• 42. Pollution

  closer to Reykjavík, eight years before that. As elsewhere in Europe sulphur concentration is lower now than when measurements began. Average value of sulphur is about 0.5 mg/l in precipitation, about 0.1 μg/m3 in aerosol and about 0.07 μg/m3 in air. Stórhöfði - a seashore background station Stórhöfði is at the south end of island Heimaey which is the largest of the Westman islands /pollution-and-radiation/pollution/

• 43. Alam_Ashraful_CES_2010

  biomass at EBT and FF in Finland Management regimes Current c mate C mate c ange EBT FF Total EBT FF Total TWh yr-1 % TWh yr-1 % M0 (0%) 8.7 40.4 49.1 -- 17.8 67.5 85.4 -- M1 (+15%) 8.7 43.9 52.6 7 18.1 72.8 90.9 7 M2 (+30%) 8.4 46.4 54.8 12 18.4 76.4 94.8 11 M3 (+45%) 8.1 48.7 56.8 16 19.0 80.3 99.3 16 a l a r e a ( m 2 h a - 1 ) Basal area just before thinning Remaining basal area threshold /media/ces/Alam_Ashraful_CES_2010.pdf

• 44. Group3-Road-scenarios

  in asphalt, road maintenace Change: 30% more than BAU Socio-economic scenario Climate scenario Worst case (4.4 C increase; 17 % increase in prec) Best case (1.5 C increase; 2% increase in prec) BAU A B Change +30 % C D Spatial analogues: - regions which today have a similar climate to the expected future one the study region (IPCC TAR, 2001) - limited by possible lack /media/loftslag/Group3-Road-scenarios.pdf

• 45. VI_2015_006

  m 2 or less, compared with losses of 80 W m 2 or more over neigh- bouring cloud-free regions. The conditions around midnight, off the southeast coast on 27 July, and along the north coast on 3 September, clearly show the limited ability (in the model) of even a complete high-level cloud cover to affect the longwave radiation balance at the surface. Mid- level clouds are usually simulated together /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 46. Early work and an overview of measurements

  Reykjavík, 209 s. Ogilvie, A. E. J. 1991. Climatic changes in Iceland A. D. c. 865 to 1598. Í: The Norse of the North Atlantic (Presented by G. F. Bigelow). Acta Archaeologica 61(1990), 233-251. Ogilvie, A. E. J. 1992. Documentary evidence for changes in the climate of Iceland, A. D. 1500 to 1800. Í R.S. Bradley and P. D. Jones. Climate Since A.D. 1500. Routledge. London and New York, 92-117 /climatology/articles/nr/1138

• 47. Early work and an overview of measurements

  Reykjavík, 209 s. Ogilvie, A. E. J. 1991. Climatic changes in Iceland A. D. c. 865 to 1598. Í: The Norse of the North Atlantic (Presented by G. F. Bigelow). Acta Archaeologica 61(1990), 233-251. Ogilvie, A. E. J. 1992. Documentary evidence for changes in the climate of Iceland, A. D. 1500 to 1800. Í R.S. Bradley and P. D. Jones. Climate Since A.D. 1500. Routledge. London and New York, 92-117 /climatology/articles/nr/1138/

• 48. VI_2014_001

  flood method for deriving flood quantiles at gauged sites with limited data availability (see for in- stance Blazkova and Beven, 1997; Cameron et al., 1999; Fiorentino et al., 2007; and a review by Boughton and Droop, 2003). A distributed hydrological model calibrated on a gauged catch- ment can be used to continuously simulate discharge series at different sites on that catchment and flood /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 49. VI_2015_009

  flood models 1–24 (Eqs. 8 and 9 applied with variables 1–12). Ratio between esti- mated and reference index flood (solid black line). The solid blue line corresponds to the reference index flood (Ratio=1), estimated as the arithmetic mean of the observed AMF sample and the dashed blue lines the 95% CI derived from the GEV distribution. Large red symbol indicates overall best model. 18 4.2.2 Flood /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 50. “The small eruption” in

  This was very important as the eruption has attracted many people since the beginning. During the first weeks over 6000 people visited the eruptions site daily and during summer, when tourists could access Iceland again, it continued to be busy. “It has been challenging to guarantee a safe access to the area, given the frequent change in eruptive styles and consequent type of volcanic hazards /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months