83 results were found for d 파생상품거래(WWW‸BYB‸PW) 파생상품매매 파생상품투자파생상품리딩⑨백산 nTh.

Results:

• 81. Dyrrdal_Anita_CES_2010

  Results W i n t e r t e m p e r a t u r e Max snow depth Trend slope Number of snow days Period II P e r i o d I I I Max snow depth Number of snow days Norwegian Meteorological Institute met.no Correlation analysis (1961-08) 138 mutual stations Introduction Data & Methods Results Correlation with winter temperature Correlation with winter precipitation In warmer regions both snow parameters /media/ces/Dyrrdal_Anita_CES_2010.pdf

• 82. RaisanenJouni_CES_2010

  not representative of present or future climate conditions? Winter mean T in Helsinki (1961-2008) 1961- 20081961- 1990 Temperature (°C) P r o b a b i l i t y d e n s i t y -12 4 Simplest case: change in mean climate, with no change in the magnitude of variability If variability changes as well, the two tails of the distribution (e.g., warm and cold) will be affected differently. IPCC (2001 /media/ces/RaisanenJouni_CES_2010.pdf

• 83. 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