83 results were found for D 출장마사지◎ㄲr톡 gttg5◎隟부평삼거리역감성출장剆부평삼거리역감성테라피부평삼거리역건마ಒ부평삼거리역건마출장👩‍🦳electrostatic/.

Results:

• 81. 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

• 82. 2010_003rs

  .............................................................................. 13 Figure 2.1. The spatial extent of each group is defined by its radius, r, and the overlap by the distance between the groups’ centres, d. .................................. 16 Figure 2.2. Two examples of joint interpretation of event distributions and focal mechanisms. ...................................................................................................... 18 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

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

  derived from: (a) SPOT 5 high-resolution stereoscopic images from 5 October 2004; (b) SPOT 5 HRS from 14 August; (c) Electromagnetic Institute Synthetic Aperture Radar Sensor (EMISAR) images from 12 August 1998; and (d) aerial photographs from 1979 (Torfajo¨kull), 1980 (Tindfjallajo¨kull) and 1984 (Eyjafjallajo¨kull). Gaps in (a) and (b) allocate uncorrelated parts of the SPOT 5 HRS image pairs /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf