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Disruption of Drought Teleconnections Between ENSO‐Influenced Regions Around 1700 CE

Abstract Our understanding of pre‐modern El Niño Southern Oscillation (ENSO) variability is reliant on proxy records, often distant from the center of ENSO activity in the equatorial Pacific Ocean. Here, we assess the relationship between reconstructed soil moisture in four distant ENSO‐influenced r...

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Päätekijät: Max C. A. Torbenson, David W. Stahle, Edward R. Cook, Benjamin I. Cook, Ulf Büntgen, Feng Chen, Ernesto Tejedor, James H. Stagge, Miroslav Trnka, Dorian J. Burnette, Weipeng Yue, Jan Esper
Aineistotyyppi: Artigo
Kieli:Inglês
Julkaistu: Wiley 2025-07-01
Sarja:Geophysical Research Letters
Aiheet:
paleoclimate
teleconnection
drought dynamics
ENSO variability
Linkit:https://doi.org/10.1029/2025GL115600
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