83 results were found for D 출장안마홍보전문『까똑 @hongbos』 수지구청역출장샵추천 수지구청역출장서비스추천∵수지구청역출장숙소추천ⓝ수지구청역출장아가씨추천 tIC.

Results:

81. ces-glacier-scaling-memo2009-01

is ice flux and b is mass balance. For (small) changes in glacier geometry with respect to a datum (often steady) state, perturbations in ice thickness, flux and mass balance will satisfy ¶(Dh) ¶t + ¶(Dq) ¶x = Db or ¶(Dh) ¶t +~ (D~q) = Db : (2) Changes in mass balance are the driving factor of glacier changes in climate change simu- lations. If the datum glacier is initially comparatively close /media/ces/ces-glacier-scaling-memo2009-01.pdf
82. Refsgaard_2-uncertainty

Delta Change Method (correction of observed precipitation) Transformation of precipitation cont fut obsfut M M PP = Observeret n dbør 0 5 10 15 20 25 30 1-12-99 11-12-99 21-12-99 31-12-99 Dato N ed bø r (m m /d ag ) Observeret Skal ring af e 5 10 15 20 25 30 35 4 - - - - t N ed bø r (m m /d ag ) Observeret D lta Change Critical assumption: Future dynamics = present dynamics No change in number /media/loftslag/Refsgaard_2-uncertainty.pdf
83. 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 d1), Rn is net radiation at the crop surface (MJ m2 d1), G is soil heat flux density (MJ m2 d1), T is mean daily air temperature at 2 m /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf