ArticleNature communications2022
Split westerlies over Europe in the early Little Ice Age.
Article in Nature communications, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. An erratum has been issued. Cited by 5 papers.
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The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.
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Who cites it
5 citing papers in PubMed.
- Protracted ocean circulation slowdown drove exceptional ice-sheet melting during ice age termination IV.Nature communications · 2026Article
- Sub-epsilon naturalScience advances · 2025Article
- A 1600-year record of extreme rainfall in northern Arabia.Science advances · 2025Article
- Past hydroclimate extremes in Europe driven by Atlantic jet stream and recurrent weather patterns.Nature geoscience · 2025Article
- Sustained North Atlantic warming drove anomalously intense MIS 11c interglacial.Nature communications · 2024Article
Corrections and comments
- Erratum issued
- Erratum issued
Authors and funding
15 authors.
Funding
No grant is acknowledged in the PubMed record.
Abstract
The Little Ice Age (LIA; ca. 1450-1850 C.E.) is the best documented cold period of the past millennium, characterized by high-frequency volcanism, low solar activity, and high variability of Arctic sea-ice cover. Past studies of LIA Atlantic circulation changes have referenced the North Atlantic Oscillation (NAO), but recent studies have noted that LIA climate patterns appear to possess complexity not captured by an NAO analogue. Here, we present a new precipitation-sensitive stalagmite record from northern Italy that covers the past 800 years. We show that in the early LIA (1470-1610 C.E.), increased atmospheric ridging over northern Europe split the climatological westerlies away from central and northern Europe, possibly caused by concurrent Artic sea-ice reduction. With ongoing ice melting in the northern high latitudes and decreasing solar irradiance in the coming years, the early LIA may potentially serve as an analogue for European hydroclimatic conditions in the coming decades.
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