38 results were found for 【77AGG.COM】gas138 slot semi toto slot slot gaming king999 km789 slot login app oud.

Results:

• 31. VI_2014_001

  WaSiM-ETH (Schulla and Jasper, 2007; Atladóttir et al., 2011; Þórarinsdóttir, 2012) was calibrated on 4 gauged catchments (vhm19, vhm38, vhm51 and vhm52). A semi-automatic multi-objective optimization based on the analysis of discharge information was used to assist in the selection of best model parameters for each catchment (Crochet, 2012d). The model was then used to simulate daily streamflow /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 32. VI_2015_005

  wintertime winds over Greenland, it can be assumed that positive changes in the zonal wind component are mostly due to a weakening of the large-scale circulation. Through the geostrophic wind relationship, this implies a weakening of the northward pressure gradient, and therefore a weakening of the Icelandic Low, relative to the semi-permanent high-pressure region over Greenland. The positive /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 33. Daniell_etal-2010

  are listed in a separate list in the Appendix, and most of them are available online. In order to thoroughly plan, establish, and evaluate the workshops and elicit answers to our research questions, we conducted in-depth interviews. These were semi-structured, guided face-to-face interviews, as well as telephone interviews, with the collaboration partners and workshop participants /media/loftslag/Daniell_etal-2010.pdf

• 34. Kok_et_al._TFSC_published_2011

  /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 35. Refsgaard_etal-2007-Uncertainty-EMS

  of the local optimisation routines based on non-linear regression, is that the prediction of interest is treated as an obser- vation, and the regression algorithm is then used to quantify the effect of the parameter uncertainty on this ‘‘observation’’. Some methods rely on a semi-analytical solution in which the regres- sion algorithm is used to compute either a predictive uncertainty interval /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 36. Reykholt-abstracts

  fields); automated feature tracking (using the VISICORR software (Dowdeswell and Benham, 2003)); and a semi-automated Fourier-transform based cross- correlation technique. In this paper, we extend this analysis to investigate the impact of various pre-processing steps (such as slope shading of the surface derived from the point cloud); the impact of the window size used to calculate the Fourier /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 37. VI_2020_004

  /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 38. Journal_of_Hydrology_Veijalainen_etal

  et al., 2008). The hydrological model of the WSFS is semi-distributed as it is divided to over 6000 small lumped sub-basins (40–500 km2) with their own water balance simulations (Vehviläinen et al., 2005). These sub-basins are connected to form the entire water- sheds. The WSFS includes a precipitation model for evaluation of areal precipitation and its form, a snow model based on tempera- ture /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf