ArticleNature communications2022
Northwestern Pacific tropical cyclone activity enhanced by increased Asian dust emissions during the 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 4 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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4 citing papers in PubMed, 36 citations in OpenAlex.
- ENSO-induced precipitation seasonality in the Chinese loess plateau during 1767-2050 CE.Fundamental research · 2026Article
- Contextualizing contemporary seasonality variations in East Asian tropical cyclone landfalls with a multi-century historical baseline.NPJ climate and atmospheric science · 2026Article
- Intensified tropical cyclone activity in East Asia during the Maunder (solar) Minimum.Proceedings of the National Academy of Sciences of the United States of America · 2025Article
- Leading role of Saharan dust on tropical cyclone rainfall in the Atlantic Basin.Science advances · 2024Article
Corrections and comments
- Erratum issued
Authors and funding
10 authors at 7 institutions in 3 countries.
Funding
No grant is acknowledged in the PubMed record.
Abstract
Instrumental records reveal that intense tropical cyclone (TC) activity varies with tropical sea surface temperature (SST) on annual-decadal scales. Drivers of intense TC activity at the centennial-millennial scale are less clear, due to the sparseness of pre-observational reconstructions. Here, we present a new 2 kyr continuous activity record of intense TCs from offshore eastern China. Our reconstruction indicates that this site witnessed enhanced TC activity during relatively warm periods, with a widespread increase in TC activity during the later part of the Little Ice Age. This latter observation reveals that enhanced TC activity was synchronized with increased Asian dust emissions during the Little Ice Age. TC activity was also lower in the late Roman Warm Period, when SST was higher but Asian dust emissions were lower than in the early phase. Such patterns suggest a centennial-millennial link between TC climatology and a combination of SST changes and Asian dust levels.
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