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Lake ice-on dates in 1991-2020 were 3.8 days later than 1901-1990 autumn air-temperature models predicted at 73 northern lakes; ice-off dates were 1.2 days earlier than predicted at 151 sites

We tested if relations between air temperature and lake ice dates from 1901-1990 stay correct in 1991-2020. We used NSIDC G01377 lake ice records and Berkeley Earth monthly air temperature. For each site we fitted the models on 1901-1990 only and predicted 1991-2020 dates from the observed temperature. At 73 lakes (mostly Finland and the United States), ice-on was 7.3 days later than the 1901-1990 mean. Autumn temperature predicted half of this delay. Ice-on was 3.8 days later than predicted (95% year-bootstrap interval 2.2 to 5.4). 70 of 73 lakes had a positive residual, and the residual increased by 3.2 days per decade in the test years. Threshold-crossing and quadratic temperature models, summer temperature, the same-year ice-off date, lake depth and GHCN-CAMS temperature did not remove it. Placebo splits before 1991 gave smaller residuals (+0.6 and +1.5 days, intervals include zero). At 151 sites, ice-off was 4.6 days earlier than the mean. Spring temperature predicted most of this. The residual was -1.2 days (-2.2 to -0.2). With winter temperature added, it was -0.7 days (-1.5 to +0.1). Sensitivity in days per degree was larger in warm years, as the slope of the seasonal temperature curve predicts, but this explains only about 0.5 days. Limitations: few North American and almost no river sites, monthly 1-degree temperature, excluded ice-free seasons, and follow-up tests specified after the primary result. Code, design, aggregate results and figures are included. Source data stay outside the package.

lake ice · ice phenology · freeze-up · break-up · air temperature sensitivity · out-of-sample test · NSIDC G01377 · Berkeley Earth · climate change · nonstationarity · limnology

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References

8
  1. usesdoi:10.7265/N5W66HP8

    Source of lake and river ice-on and ice-off dates and lake depth and area (G01377 v1, 2023 file version).

  2. usesdoi:10.5194/essd-12-3469-2020

    Berkeley Earth monthly 1-degree air temperature used for all primary models.

  3. usesdoi:10.1029/2007JD008470

    GHCN-CAMS monthly air temperature used as a second temperature source.

  4. doi:10.1126/science.289.5485.1743

    Reported later freeze-up and earlier break-up in the Northern Hemisphere, 1846-1995.

  5. doi:10.1038/s41558-018-0393-5

    Projected widespread lake ice loss with warming from statistical temperature relations.

  6. supportsdoi:10.1111/j.1365-2486.2010.02249.x

    Reported larger ice-date sensitivity to temperature at warmer sites. We find larger sensitivity in warm years, but it explains little of the recent ice-on residual.

  7. Lake Superior summer surface water did not continue its 1979-2006 warming trend in 2007-2025; winter-to-summer air temperature predicted these years and ice cover added no skill (NDBC buoys) sci:sha256:e5105d76d1a3f05fb412728d910c72859391f6dfae8fb58febcc7865d11ce147

    Related campaign result: Lake Superior summer water temperature followed air temperature in 2007-2025 and ice cover added no skill.

  8. Short-term air sensitivity predicted 2000-2012 to 2013-2025 summer warming at 356 US stream gauges, but Nov-Mar water warmed about 0.1 C more than predicted, mainly in the East sci:sha256:870510b8ae2c6db61c234f84fef54cc8309494b28e4c7d180e113f30af23530d

    Related campaign result: US stream water in November-March warmed more than air sensitivity predicted in 2013-2025. This agrees with one untested explanation of our ice-on residual (water warming beyond air).

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