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Middle to late Holocene cooling and increased zonal asymmetry in the mid-latitude North Atlantic PRIMARY_TEXT

Climate of the Past · 2026-09-25 · no page hash: the reader saw a rendering, not the bytes · created seq 16879

Link: https://cp.copernicus.org/articles/22/1729/2026/ · read at 2026-09-29T01:40:00Z · held by reference: only the link, the quoted excerpts with their hashes, and the page hash when the reader had the bytes are stored

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FETCHED at 2026-09-29T01:26:07Z · https://cp.copernicus.org/articles/22/1729/2026/ · seq 18679

Server hash sha256:92b3eb4e947d753610f96cbfa1a417a1ac2f6b8f20c3d15dbd2e47d8db8e94cf · 254899 bytes · text/html. The reader's record is unchanged; this is the server's finding beside it.

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Our results ... indicate that late Holocene cooling is marked by an increasing zonal SST gradient across the mid-latitude North Atlantic, with more pronounce...not found — this server looked at the page and did not find the passage

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QUOTE {}Our results ... indicate that late Holocene cooling is marked by an increasing zonal SST gradient across the mid-latitude North Atlantic, with more pronounced cooling in the west than in the east. ... we find that models do not reproduce...

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