<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>11(47)</volume><submitter>Chen J</submitter><pubmed_abstract>Bering Sea winter sea ice (BSWI), vital for regional climate, ecosystem, and livelihoods, is significantly influenced by El Niño-Southern Oscillation (ENSO). Here, we identify a shift in the ENSO-BSWI relationship. Pre-mid-1990s, traditional eastern Pacific ENSO dominated, driving a positive ENSO-BSWI linkage; post-mid-1990s, more frequent central Pacific (CP) ENSO events reversed this relationship to negative. Observations and model experiments show that CP El Niño coupled with positive-phase North Pacific meridional mode (NPMM) redirects poleward-propagating Rossby wave trains, enhancing Bering Sea southerlies. This suppresses ice advection, intensifies warm air intrusion, and reduces BSWI. Strengthened CP ENSO-NPMM coupling and heightened NPMM variability amplify this teleconnection, in</pubmed_abstract><journal>Science advances</journal><pagination>eady2329</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12629142</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>ENSO's changing grip on Bering Sea ice: The emerging control of the North Pacific meridional mode.</pubmed_title><pmcid>PMC12629142</pmcid><pubmed_authors>Liu J</pubmed_authors><pubmed_authors>Chen J</pubmed_authors><pubmed_authors>He Z</pubmed_authors><pubmed_authors>Wang C</pubmed_authors><pubmed_authors>Yu JY</pubmed_authors><pubmed_authors>Wang X</pubmed_authors><pubmed_authors>Zhang L</pubmed_authors><pubmed_authors>Chen S</pubmed_authors></additional><is_claimable>false</is_claimable><name>ENSO's changing grip on Bering Sea ice: The emerging control of the North Pacific meridional mode.</name><description>Bering Sea winter sea ice (BSWI), vital for regional climate, ecosystem, and livelihoods, is significantly influenced by El Niño-Southern Oscillation (ENSO). Here, we identify a shift in the ENSO-BSWI relationship. Pre-mid-1990s, traditional eastern Pacific ENSO dominated, driving a positive ENSO-BSWI linkage; post-mid-1990s, more frequent central Pacific (CP) ENSO events reversed this relationship to negative. Observations and model experiments show that CP El Niño coupled with positive-phase North Pacific meridional mode (NPMM) redirects poleward-propagating Rossby wave trains, enhancing Bering Sea southerlies. This suppresses ice advection, intensifies warm air intrusion, and reduces BSWI. Strengthened CP ENSO-NPMM coupling and heightened NPMM variability amplify this teleconnection, in</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025 Nov</publication><modification>2026-06-05T17:27:27.557Z</modification><creation>2026-05-19T03:12:00.763Z</creation></dates><accession>S-EPMC12629142</accession><cross_references><pubmed>41259501</pubmed><doi>10.1126/sciadv.ady2329</doi></cross_references></HashMap>