91 results were found for y 사천유흥ゲ［dm080.com｝☏사천타이✫사천아로마 사천아로마✦사천출장.

Results:

• 61. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 62. glacier_mass_balance_poster

  750-1170 AAR of the warm year of 2004 - digitized using the October 2004 SPOT 5 HRS images Ice cap E: Eyjafjallajökull To: Torfajökull Ti: Tindfjallajökull AAR (%) 20-25 <5 0 Method References Berthier E., Arnaud Y., Baratoux D., Vincent C. and Rémy F. 2004. Recent rapid thinning of the "Mer de Glace" glacier derived from satellite optical images. Geophys. Res. Lett., 31, L17401, doi:10.1029 /media/ces/glacier_mass_balance_poster.pdf

• 63. VI_2022_006_extreme

  and the y-axis the dates between March and July. For every year, the melt season starting date is plotted (blue dots), and a blue line connects the dates for all the years. A regression line fitting those values (orange line) is shown, and the difference in days between the beginning and the end of the period, as calculated from the regression line, is indicated at the top of the plot. In 9 cases /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 64. VI_2017_009

  /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 65. 2010_017

  ) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y direction. The hydraulic conductivity is adjusted in distributed grids unlike /media/ces/2010_017.pdf

• 66. Paper-Olafur-Rognvaldsson_91

  High-resolution regional climate simulations over Iceland using polar MM5. Mon. Wea. Rev., 133, 3527– 3547. Buzzi A., Tartaglione N. and Malguzzi P. 1998. Numerical simulations of the 1994 Piedmont flood: Role of orography and moist processes. Mon. Wea. Rev., 126, 2369–2383. Chiao, S., Lin Y.-L. and Kaplan M. L. 2004. Numerical study of the orographic forcing of heavy precipitation during MAP IOP /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 67. 2010_003rs

  Use of relatively located micro- earthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland Sigurlaug Hjaltadóttir VÍ 2010-003 Skýrsla   f l l l dUse o re ative y ocate micro- earthquakes to map fault patterns and estimate the thickness of the brittle crust in Southwest Iceland Sigurlaug Hjaltadóttir, Veðurstofu Íslands VÍ 2010-003 ISSN 1670-8261 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 68. VI_2016_006_rs

  Such landslides fall from a comparatively high elevation, cause extensive disruption and upheaval of loose materials and soils in their way, and can travel considerable distances uphill against opposing slopes. Secondly, there are medium-sized or large, rapid debris flows that are released from com- paratively high elevations and are confined to gullies as they travel down the mountain- side, similar /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 69. VI_2020_005

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

• 70. Moellenkampetal_etal-2010

  /media/loftslag/Moellenkampetal_etal-2010.pdf