46 results were found for 99色中色网址M8K3典CC】w.

Results:

• 31. CES_D2.4_task2_CMIP3_winds

  changes in the September-April mean geostrophic wind speed from 1971- 2000 to 2046-2065 (left) and the statistical significance of the ensemble mean change according to a standard t test (right). Light, medium and dark red shading indicate significance at the 95%, 99% and 99.9% levels, respectively. 95 % 99 % 99,9 % 4 Fig. 4. As Fig. 3, but for the autumn (September /media/ces/CES_D2.4_task2_CMIP3_winds.pdf

• 32. Doctoral Student Position

  /nonam/news/nr/2171

• 33. Water_resources_man_Veijalainen_etal

  3 0 5 0 7 0 2070–99 (f) 0 20 0 60 0 100 0 2010–39(g) 0 20 0 60 0 100 0 2040–69(h) Lake Saimaa 0 20 0 60 0 100 0 2070–99(i) Outflo w(m 3 s ) Outflo w(m 3 s ) Outflo w(m 3 s ) Month Fig. 5 Average daily outflow (m3/s) from Lake Pielinen (a–c), Lake Syväri (d–f) and Lake Saimaa (g–i) in the reference period (blue) and in 2010–2039 (left), 2040–2069 (middle) and 2070–2099 (right). The results /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 34. vhmkerfi_mars_2012

  W W W W W W W D DD DD DD CB CA CB CA CA CB CB CB CA CA CB CA CA CA CBCB CB CA CB CB CB CBCBCB CB CB CA CA CACA CA CA CACACB CA CA CA CA CB CA CA CA CA CA CB CA CA CA CACA CA CB CA CA CA CA CA CA CB CA CA CA CBCA CA CACA CA CA CA CA CA CA CA CB CA CA CA CBCB CB C CA CA CB CB CA CA CB CA CB CA CA CB CA CA CA CACA CA CB B CA CA CA CA CA CB CA CA CA CA CB CA CA CAC CACB CA CBCB CB CB CB CACA CBCA C B /media/vatnafar/maelar/vhmkerfi_mars_2012.pdf

• 35. Sea ice in April 2010

  to land 52 nm NW of Barði and 48 nm NW of Straumnes. Two observations were received on icebergs, the 4th and the 5th. An observation from a ship on the 18th reported sea ice from 66°31´N and 26°08´W to 66°26´N and 25°47´W. Northeasterlies were somewhat less prevalent on the Greenland Strait than the average this month /sea-ice/monthly/2010/nr/2339

• 36. Sea ice in November 2010

  WNW of Straumnes and the ice was scattered. Two observations from ships were received 29th November, on a strip at location 66°50´N - 24°36´W and at 67°00´N - 24°02´W. Wind directions were mostly from the northeast and the east, however southwesterlies occurred for a few days at the Greenland Strait /sea-ice/monthly/2010/nr/2346

• 37. Sea ice in July 2011

  which implies the need of caution for passing ships. Two observations were received on icebergs from ships: 21st July in location 66°40.23‘N 025°13.34‘W 31st July in location 66°48.6‘N 023°03.7‘W In the Greenland Strait northeasterly wind directions were predominant but there were also a few days with southwesterlies /sea-ice/monthly/2011/nr/2403

• 38. ice-chart_colour-code-standard

  less than 10/10 9+ 10/10 10 Undetermined or unknown x Concentration (C) C – Total concentration of ice in the area, reported in tenths (see symbols in table 3.1). Note: Ranges of concentration may be reported. Ca Cb Cc – Partial concentrations of thickest (Ca), second thickest (Cb) and third thickest (Cc) ice, in tenths. Note: Less than 1/10 is not reported. 10/10 of one stage of development /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 39. Hare-2011-ParticipatoryModelling

  is ar tic le X X X X X X X Identif ygenera lform so f pa rt ici pa to ry m o de llin g Tabl e1 . Co m pa ris o n o ff ra m ew o rk s fo r ca te go riz in g pa rt ic ip at o ry m o de llin g pr o ce ss es . Th is ta bl e co m pa re s di ffe re n tf ra m ew o rk s (bo ld , fir st co lu m n )a cc o rdin gt o th e categorica lcriteri a the yemplo y(column si n italics )an d thei rpurpos e (bold ,fina /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 40. vanRoosmalen_etal-2009-WRR_2007WR006760

  to the description of the geological settings in the model, such that groundwater flow can be described at high spatial resolution (horizontal discretization is 500 m and vertically 16 model layers are used). The DK model was developed for water resources assessment and planning and as 99% of the water supply in Denmark is based on groundwater, it is important that this model accurately describes /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf