26 results were found for 하이로미로미▥문의카톡 gttg5▥㍓하이로미로미출장椢하이마사지賙하이마사지샵䭂하이마사지업소🤸🏽‍♂️longitude/.

Results:

• 21. VI_2022_006_extreme

  used. Because the ERA-20c dataset has a much coarser resolution than the ICRA dataset, for each catchment a mean latitude and longitude was calculated and this point value used to retrieve a timeseries based on the weighted-average among the four nearest grid-points. These timeseries were then used to complement the results from the ICRA. 3.3 The CMIP5 projections The Coupled Model /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 22. 2013_001_Nawri_et_al

  atlas files follows the standard developed by Risø National Laboratory (Troen and Petersen, 1989). An anno- tated example is shown in Figure 3. The header line contains information about the model run, the index numbers of the particular grid point, the local surface roughness length (SRL), as well as a triplet of numbers with longitude in degrees east, latitude in degrees north, and height above /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 23. ces-oslo2010_proceedings

  interpolated onto a longitude- latitude grid. The analysis has been applied to the whole year. The storm frequency for events with central pressure below a threshold values of 960, 970, 980 and 990hPa were examined, and the gradient wind from the simulated storm systems were compared with corresponding estimates from the re-analysis. The analysis also yielded estimates for the spatial extent /media/ces/ces-oslo2010_proceedings.pdf

• 24. VI_2020_004

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

• 25. VI_2013_008

  Iceland. MSLP was extracted twice daily from ERA-40 (Uppala et al., 2005) for the period 1958–2001 and available ECMWF analysis from 2002 to 2006, on a 1 X 1 latitude-longitude grid. As daily precipitation, temperature and derived variables were averaged from 00 to 00UTC, only the 12UTC MSLP data were used so as to be centered on the same 24-h period. 4 Method implementation Below, details /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 26. VI_2014_006

  scale, used to identify weather analogues. These fields are extracted twice daily (00UTC and 12UTC) on a 1 x 1 latitude-longitude grid from the ECMWF operational analysis and forecasts available for the period 2001–2006. The ana- logue meteorological situations are extracted from the ERA-40 reanalysis archive (Uppala et al., 2005) for the period 1958–2001. 14 Predictants: Gridded series of daily /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf