91 results were found for y 신용대출㎃『𝟬𝟭𝟬-𝟲𝟳𝟱𝟯-𝟲𝟮𝟭𝟵」✘신용대출 카카오뱅크대출※신용대출 비대면대출 당일대출.

Results:

51. VI_2017_009

/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
52. 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
53. 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
54. 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
55. Moellenkampetal_etal-2010

/media/loftslag/Moellenkampetal_etal-2010.pdf
56. Eriksson_Garvill_Nordlund_2006

were collected through a mail survey in Sweden, Acceptability of travel demand managemen of problem awareness, persona Louise Erikssona,b,, Jo¨rgen Garvil aDepartment of Psychology bTransportation Research Unit Available onlin Abstract y 26 (2006) 15–26 t measures: The importance norm, freedom, and fairness la,b, Annika M. Nordlunda,b a˚ University, Sweden Umea˚ University, Sweden 14 July 2006 /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
57. Refsgaard_etal-2007-Uncertainty-EMS

on the quantity at hand (strengths and weaknesses in Box 1. The error propagation equation The error propagation equations for the most common operators are (s is the standard deviation): Addition and Subtraction: z ¼ x þ yþ/ or z ¼ x y/ sz ¼ ffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffiffi s2x þ s2y þ/ r Multiplication by an exact number: z /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
58. D2.3_CES_Prob_fcsts_GCMs_and_RCMs

climate changes between the CMIP3 and ENSEMBLES simulations 15 4. Impact of RCM data on forecasts of climate change 18 5. Probabilistic projections of temperature and precipitation change 24 5.1 Best estimates and uncertainty ranges of temperature and precipitation change 24 5.2 How probably will temperature increase (precipitation change) by at least X°C (Y%)? 28 6. Conclusions 34 References /media/ces/D2.3_CES_Prob_fcsts_GCMs_and_RCMs.pdf
59. Gudmundsson-etal-2011-PR-7282-26519-1-PB

from the glacier margins). This was done by shifting the x and y coordinates of the 40 m40 m DEMs in 5 m steps and calculating the correlation to the corresponding values of the 5 m5 m EMISAR DEM. In all cases, both the maximum correla- tion and minimum standard deviation yielded the same shift. After the co-registration, the same ice-free areas were used to correct the vertical offset of the DMA /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
60. Bárðarbunga 2014 - December events

moment release is observed before the onset of the fissure eruption (red bar), i.e. while the dyke was growing, and the moment release in the dyke is now 10,000 times less than it was before the eruption (logaritmic scale on y-axis). For the caldera (lower panels), things are a bit more complicated, although a clear trend of decreasing activity is found there as well. Most moment is released during /earthquakes-and-volcanism/articles/nr/3055