Extreme weather events are becoming more common in arctic and boreal regions. The soils and permafrost in these high-latitude regions contain one-third of the global soil carbon pool. Thus, understanding how extreme weather events (e.g., extreme heat, heavy precipitation) impact high-latitude CO₂ fluxes is crucial to understanding if these regions will act as a sink or a source of carbon as extreme events become more frequent. Here, we present a comparison between in-situ carbon flux measurements from an Arctic-Boreal Carbon Flux dataset, ABCFlux v2, and inventoried extreme climatic events. Through a combination of correlation analysis and random forest modeling, we aim to understand how seasonal and annual CO₂ fluxes respond to extreme weather events, and how these responses vary between 1) boreal and tundra sites, and 2) permafrost and non-permafrost soils.