50 results were found for 线上娱乐电子游戏网站官网最新-5000块去澳门赌博-(✔️网址315bet.net✔️)-线上娱乐电子游戏网站官网最新-十大买球app排行网站注册最新-(✔️输入bet25.net✔️)-线上娱乐电子游戏网站官网最新-线上娱乐电子游戏网站官网最新-线上娱乐电子游戏网站官网最新-【✔️输入㊙️900bet.net✔️】.

Results:

• 11. 2010_017

  of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf

• 12. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 13. 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

• 14. 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

• 15. 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

• 16. 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

• 17. Reykholt-abstracts

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

• 18. VI_2022_006_extreme

  with Maximum Likelihood Estimation. From Massad et al., 2020. 6 Figure 2 – Distribution of annual rainfall (mm year-1) in Iceland for the period 1981 – 2010. Solid lines show the 1000, 3000, and 5000 mm year-1 values. Results based on the ICRA dataset. From Björnsson et al., 2018. 7 2 Study area Eleven hydropower catchments operated by Landsvirkjun were selected for this study /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 19. Journal_of_Hydrology_Veijalainen_etal

  precipitation and time of year (an index for available net radiation) (Vehviläinen and Huttunen, 1997). This equation has been calibrated and verified against observations of Class A pan evaporation values (Vehviläinen and Huttunen, 1997). The actual evaporation is calculated from potential evapora- tion and the soil moisture deficit. The changes in temperature and precipitation affect /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 20. 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