<?xml version="1.0" encoding="UTF-8"?>
<resource xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4/metadata.xsd"
          xmlns="http://datacite.org/schema/kernel-4"
          xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance">
    <identifier identifierType="DOI">10.26165/JUELICH-DATA/JYGQ65</identifier>
    <creators><creator><creatorName>Chen, Shuying</creatorName><nameIdentifier schemeURI="https://orcid.org/" nameIdentifierScheme="ORCID">https://orcid.org/0000-0002-0986-0950</nameIdentifier><affiliation>(Forschungszentrum Jülich GmbH)</affiliation></creator><creator><creatorName>Poll, Stefan</creatorName><affiliation>(Forschungszentrum Jülich GmbH)</affiliation></creator><creator><creatorName>Hendricks Franssen, Harrie-Jan</creatorName><affiliation>(Forschungszentrum Jülich GmbH)</affiliation></creator><creator><creatorName>Heinrichs, Heidi</creatorName><affiliation>(Forschungszentrum Jülich GmbH)</affiliation></creator><creator><creatorName>Vereecken, Harry</creatorName><affiliation>(Forschungszentrum Jülich GmbH)</affiliation></creator><creator><creatorName>Goergen, Klaus</creatorName><affiliation>(Forschungszentrum Jülich GmbH)</affiliation></creator></creators>
    <titles>
        <title>Convection-permitting ICON-LAM Simulations for Renewable Energy Potential Estimates over Southern Africa</title>
    </titles>
    <publisher>Jülich DATA</publisher>
    <publicationYear>2024</publicationYear>
    <resourceType resourceTypeGeneral="Dataset"/>
    
    <descriptions>
        <description descriptionType="Abstract">This regional atmospheric modelling dataset was produced by a dynamical downscaling setup, the ICOsahedral Nonhydrostatic (ICON) Numerical Weather Prediction (ICON-NWP) model v2.6.4 was run in limited area mode (ICON-LAM) with a weather forecast configuration (ICON-D2) from the German Weather Service (DWD), driven by the initialized analysis based on the 13km global deterministic ICON-NWP forecasts from DWD. The simulations cover three years, from 2017 to 2019, at a convection-permitting spatial resolution of 3.3km over a southern African model domain. To ensure a good agreement of the ICON-LAM simulations with the observed weather over the large model domain, the atmosphere was reinitialized every 6 days with one preceding spin-up day, and the land surface as well as subsurface were run transiently.</description>
    </descriptions>
    <contributors><contributor contributorType="ContactPerson"><contributorName>Chen, Shuying</contributorName><affiliation>(Forschungszentrum Jülich GmbH)</affiliation></contributor></contributors>
</resource>
