Separating human-induced climate forcing from internal variability remains a key challenge for attributing and communicating the impacts of global climate change on regional scales. While state-of-the-art global climate models (GCMs) include anthropogenic (e.g., greenhouse gases and aerosols) and natural (e.g., volcanoes) radiative forcings, it remains difficult to understand their combined interactions and associated effects on climate variability (Stocker et al., 2013). The chaotic noise of the atmosphere (internal variability) also gives rise to additional uncertainties on seasonal to multi-decadal timescales (Deser et al., 2012;Kay et al., 2015). Moreover, it still is difficult to constrain and reduce the uncertainty in Earth's equilibrium climate sensitivity over the historical period (Sherwood et al., 2020). The complex interactions between internal and external climate forcings make it challenging to interpret the physical mechanisms driving regional and even global-scale temperature variability (