Galedra
Sign in Sign up

Claims

As of snapshot 27745 under ledger-default@0.3.0.

ClaimTypeAssessmentScoreReview checksReferences
Alkenone and planktonic-foraminifera proxy records indicate that mid- to late-Holocene summertime cooling in the mid-latitude North Atlantic was stronger in the west than east, increasing the zonal sea-surface-temperature gradient; TraCE-21k simulations did not reproduce this asymmetry. COMPARATIVE Supported 0.8808 1 of 4 127