Changes in the western flank of the North Atlantic subtropical high since 1140 CE: Extremes, drivers, and hydroclimatic patterns
- DOI
- 10.1126/sciadv.adr5065
- Published
- 2025-04-18
- Container
- Science Advances
- Publisher
- American Association for the Advancement of Science (AAAS)
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1126/sciadv.adr5065,
title = {Changes in the western flank of the North Atlantic subtropical high since 1140 CE: Extremes, drivers, and hydroclimatic patterns},
author = {Joshua C. Bregy and Justin T. Maxwell and Scott M. Robeson and Grant L. Harley and Valerie Trouet},
year = {2025},
journal = {Science Advances},
doi = {10.1126/sciadv.adr5065},
url = {https://doi.org/10.1126/sciadv.adr5065}
}RIS
TY - JOUR TI - Changes in the western flank of the North Atlantic subtropical high since 1140 CE: Extremes, drivers, and hydroclimatic patterns AU - Joshua C. Bregy AU - Justin T. Maxwell AU - Scott M. Robeson AU - Grant L. Harley AU - Valerie Trouet PY - 2025 JO - Science Advances DO - 10.1126/sciadv.adr5065 UR - https://doi.org/10.1126/sciadv.adr5065 ER -
APA
Bregy, J. C., Maxwell, J. T., Robeson, S. M., Harley, G. L., & Trouet, V. (2025). Changes in the western flank of the North Atlantic subtropical high since 1140 CE: Extremes, drivers, and hydroclimatic patterns. Science Advances. https://doi.org/10.1126/sciadv.adr5065
Source records
- crossref · retrieved 2026-09-24T23:44:10.238Z