North Atlantic meltwater during Heinrich Stadial 1 drives wetter climate with more atmospheric rivers in western North America

Climate model output for simulations of the Last Glacial Maximum (~21 ka) and Heinrich Stadial 1 (~16 ka) using the Community Earth System Model v1.3 (see README.txt file for more information).

Bibliographic Details
Main Authors: Oster, Jessica L., Macarewich, Sophia I., Lofverstrom, Marcus, de Wet, Cameron, Montañez, Isabel, Lora, Juan M., Skinner, Christopher, Tabor, Clay
Format: Article in Journal/Newspaper
Language:unknown
Published: 2023
Subjects:
North Atlantic
Online Access:https://zenodo.org/record/8342373
https://doi.org/10.5281/zenodo.8342373
Description
Summary:Climate model output for simulations of the Last Glacial Maximum (~21 ka) and Heinrich Stadial 1 (~16 ka) using the Community Earth System Model v1.3 (see README.txt file for more information).

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