Comment on egusphere-2025-400

Abstract. Atlantic Canada experiences frequent major storms, particularly tropical cyclones transitioning into post-tropical storms. Events such as Hurricane Fiona (2022), Dorian (2019), and Juan (2003) have caused significant damage, loss of life, and coastal erosion, exacerbated by sea level rise and warming waters. Despite this, centennial- to millennial-scale storm records in the region remain scarce. Existing studies in North America focus primarily on marine and coastal overwash records, with limited use of aeolian mineral inputs in ombrotrophic peatlands as storm proxies. Here, we address these gaps by analysing grain-size and geochemical data from two peatlands in Quebec, Canada’s Magdalen Islands. Our two peat records reveal consistent storm signals over the past 4000 years, with three key periods of heightened activity: 800–550 BCE, 600–800 BCE, and 1300–1700 CE. These signals align with marine and overwash records spanning the past 2000 years across eastern Canada, the US, and the Bahamas, indicating low storm activity during the Medieval Climate Anomaly, followed by increased activity during the Little Ice Age. Our findings suggest that storm records in these regions are influenced by local climatic factors. Negative phases of the Atlantic Multidecadal Variability, which typically suppress hurricane activity in the North Atlantic, are associated with conducive hurricane formation and intensification north of the Bahamas. Additionally, the position of the Bermuda High seems to play a more significant role in directing storm tracks during different climatic phases. Our findings highlight the potential antiphase relationship in storm activity between regions north of the Bahamas and those in the Gulf of Mexico, suggesting broader climatic mechanisms that warrant further investigations. Despite the similarities between our two sites, discrepancies in geochemistry and mineralogical profiles highlight the importance of site-specific conditions in interpreting the storm record from peatlands, namely the distance of the sites to the coast and source of aeolian sediment, as well as peatland size. Challenges also remain in calibrating peat-based proxies with historical storm records, as identifying specific events from the past 150 years remains difficult.

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