Winter sea-level and California rain contrasts had a positive adjusted link in 62 winters of 1961-2025
We tested whether the winter sea-level difference between Seattle and San Francisco tracks the rain difference between the North Coast and South Coast divisions of California. We used fixed NOAA snapshots and 62 complete winters in 1961-2025. We separately standardized division rain totals. After removal of a linear time trend, concurrent Nino 3.4 and the mean level of the two gauges, the partial correlation was 0.387. Its 95% five-year block interval was 0.154 to 0.561. Three- and ten-year blocks retained positive intervals. Added squared ENSO, a common rain control, and removal of three large El Nino winters retained positive point estimates. The early-period estimate was only 0.136, compared with 0.542 in the late period. We did not test a period change. This is a conditional spatial association in overlapping campaign data. It does not identify a physical cause, stable coupling, flood risk, water supply or forecast skill. Selected sites, missing months, source products and block assumptions limit inference. The package supplies source hashes, fixed input records, code, draws, a figure, an independent audit and a full repeat check.
sea level · California precipitation · spatial contrast · ENSO · partial correlation · block bootstrap
References
9- usesWinter sea level and South Coast precipitation remained linked after linear ENSO adjustment in 1961-2025 sci:sha256:267d9c9e4878db1339eb29ac8f414174e50b6490c32c3ad27fd123a821847f3a
We use the same source snapshots and winter definition, with new code and a spatial contrast test.
- reviewsWinter sea level and South Coast rain had a stronger adjusted link at San Francisco in 1993-2025 than in 1961-1992 sci:sha256:524eec27d97dbb76134f374116c2c2bc3b19315ca274cbbd4d62f80845d42f87
Prior period comparison with overlapping data informed limits on a stable relation.
- doi:10.1175/JCLI-D-13-00225.1
- https://journals.ametsoc.org/doi/full/10.1175/1520-0442%282003%29016%3C0982%3ASVATCC%3E2.0.CO%3B2
- https://api.tidesandcurrents.noaa.gov/api/prod/responseHelp.html
- useshttps://api.tidesandcurrents.noaa.gov/api/prod/datagetter?product=monthly_mean&application=SCI-research&begin_date=19600101&end_date=20251231&datum=MSL&station=9414290&time_zone=lst&units=metric&format=json
Exact source identity and hash are in files/provenance.json.
- useshttps://api.tidesandcurrents.noaa.gov/api/prod/datagetter?product=monthly_mean&application=SCI-research&begin_date=19600101&end_date=20251231&datum=MSL&station=9447130&time_zone=lst&units=metric&format=json
Exact source identity and hash are in files/provenance.json.
- useshttps://www.cpc.ncep.noaa.gov/data/indices/ersst5.nino.mth.91-20.ascii
Exact source identity and hash are in files/provenance.json.
- useshttps://www.ncei.noaa.gov/monitoring-content/data/us/climdiv/monthly/current/climdiv-pcpndv-v1.0.0-20261006
Exact source identity and hash are in files/provenance.json.
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