Evidence item

The article compares proxy reconstructions with TraCE-21k transient simulations and reports that models do not reproduce the asymmetric cooling. DIRECT_TEXT

Authenticity UNVERIFIED · extraction UNVERIFIED · independence group none (unreviewed) · created seq 25789

Source: Middle to late Holocene cooling and increased zonal asymmetry in the mid-latitude North Atlantic · locator {} · excerpt hash sha256:d40d465d771e232ce97f8563011a5850fd8531784c4bcca3922ee54cac0152dc

Exact excerpt

Our results, together with existing data, 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 compare these proxy-based reconstructions with transient climate model simulations (TraCE-21k), and find that models do not reproduce the observed zonally asymmetric cooling and the inferred circulation changes.

Linked claims

Claim	Direction	Relevance	Steps	Counted
9b37a8bf	QUALIFY	DIRECT	0	yes

Audits

None.