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Results:

• 21. GA_2009_91A_4_Andreassen

  ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf

• 22. IPPC-2007-ar4_syr

  a near-zero pre-industrial background concentration, primarily due to human activities. {WGI 2.3, SPM; SROC SPM} There is very high confidence that the global average net effect of human activities since 1750 has been one of warm- ing, with a radiative forcing of +1.6 [+0.6 to +2.4] W/m2 (Figure 2.4). {WGI 2.3, 6.5, 2.9, SPM} The combined radiative forcing due to increases in CO2, CH4 and N2O /media/loftslag/IPPC-2007-ar4_syr.pdf

• 23. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  -corrected SPOT 5 high-resolution geometric (HRG) images with 2.5 m 2.5 m spatial resolution, acquired in the autumn 2003 and (4) airborne polarimetric synthetic aperture radar images observed simultaneously to the 1998 EMISAR images and the EMISAR DEM viewed as a shaded relief image (Magnu´sson et al. 2005b). We estimate the average specific net mass balance (in m yr1 w. eq.) as bn r DV A1  N /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf

• 24. Group4

  ); new long-term investment strategy prioritizing low- or zero-net carbon forms of mobility 2040 Modal shift in logistics chains, especially within heavy industry. 3.3 Backcasting scenario narrative Low-Impact Mobility Project Evaluation (LIMPE) Climate change is occurring. Is it natural or anthropogenic? It doesn’t matter. Even though the future is inherently uncertain, one certainty /media/loftslag/Group4.pdf

• 25. vanRoosmalen_etal-2009-WRR_2007WR006760

  1998] and RCM output such as incoming and outgoing, short- and long-wave radiation, temperature, water vapor pressure, and wind speed: ETref ¼ 0:408D Rn
  Gð Þ þ g 900T þ 273 u2 es
  eað Þ Dþ g 1þ 0:34u2ð Þ ð3Þ where ETref is reference evapotranspiration (mm d
  1), Rn is net radiation at the crop surface (MJ m
  2 d
  1), G is soil heat flux density (MJ m
  2 d
  1), T is mean daily air temperature at 2 m /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 26. VI_2009_012

  The medians of ratios from the broad-band digitizers (G24) are close to one, but the lowest median values are obtained at stations with short-period digitizers (RD3) in combination with either 1-Hz short-period (LE1) sensors, or broad-band (BB) sensors. The reason for the low ratios in the LE1-RD3 combination is obviously failure to retrieve all the low frequency amplitude through instrument /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 27. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf

• 28. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

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

  (DGPS) equipment in 2001. Continuous profiles, approximately 1 km apart, were measured in the accumulation zone and a dense net- work of point measurements were carried out in the abla- tion zone. Digital Elevation Models (DEMs) of the surface and bedrock were created from these data (Fig. 2; Björns- son and Pálsson, 2004). The estimated errors are at most 1–5 m (bias less than 1 m) for the surface /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 30. VI_2020_011_en

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