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Contributions from Changing Large-Scale Atmospheric Conditions to Changes in Scandinavian Temperature and Precipitation Between Two Climate Normals
2022
Tellus: Series A, Dynamic Meteorology and Oceanography
Multidecadal changes in regional climate can occur as a forced response to changing greenhouse gases and aerosols, as a result of natural internal climate variability, or due to their combination. Internal climate variability is frequently associated with regional changes in large-scale circulation. We investigate how changes in Scandinavian temperature and precipitation conditions during 1961-2020 can be linked to changes in the atmospheric large-scale circulation. The study is based on data
doi:10.16993/tellusa.49
fatcat:jqqblx32dzh67ljys3evtir2da