Along the U.S. Pacific Coast, coinciding positive and negative sea-level anomalies can demonstrate the interconnection between oceanic and atmospheric systems during climatic events such as the El Niño Southern Oscillation (ENSO).
Notes on verification
Confirmed by NOAA source text and independently corroborated by USGS and peer-reviewed JGR Oceans study, plus NOAA/OCB summary, all consistent with no contradicting evidence. [tier=gold indep_score=0.983 clusters=3 claim_tier=notable]
Sources
- Monthly Anomalies - Sea Level Trends - NOAA Tides & Currents (seed:science_and_space)
- https://pubs.usgs.gov/publication/70024249 (corroboration)
- https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9787497/ (corroboration)
- https://www.us-ocb.org/enso-diversity-and-its-implications-for-us-west-coast-marine-ecosystems/ (corroboration)