(The Demonstration Space will be one of those spaces.) On the left of the screen is a list of spaces. Your Confluence Dashboard appears in the new window.Hint: Perform the rest of these instructions in the new browser window. Right-click the ' Dashboard' link at the top left of your screen and open the link in a new browser window.Log in to Confluence, if you are not logged in already, by clicking the ' Log In' link at the top right of your Confluence screen.Reference values of evapotranspiration are computed using either observations or NWPs and following the Penmann-Monteith method, which is implemented in the open source pre-processor LISVAP.Now that you have seen how the menus work, you are ready to start creating content in Confluence. Bilinear interpolation is used for EFAS v5 and GloFAS v4 (1 arcmin European and 0.05 degrees global set-ups, respectively). Nearest neighbor interpolation was used up to EFAS v4 and GloFAS v3 (5km European and 0.1 degrees global set-ups, respectively). NWPs are upsampled from their native resolution to the desired resolution of EFAS and GloFAS using the interpolation algorithms implemented in the open-source pre-processor pyg2p. The interpolation algorithm is Spheremap: more details can be found in Thiemig et al. Observations for EFAS are collected, quality checked, and interpolated by the CEMS-Meteorological Data Collection Centre (more details in this page).Specifically, the required inputs are total precipitation, 2-metre temperature, and reference evapotranspiration. This page briefly explains the pre-processing of the observations or NWPs to prepare the gridded dataset required as input to the hydrological model LISFLOOD OS. CEMS-Flood meteorological forcing are derived from observations or from NWPs: the list and usage of data sources is provided by CEMS-Flood meterological forcing and land surface data - Copernicus Emergency Management Service - CEMS - ECMWF Confluence Wiki.
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