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Low summer sea ice gave uncertain winter variance contrasts in 45 Arctic and 46 Antarctic seasons

We tested whether low summer sea ice extent was followed by more variable winter extent. We used NSIDC Sea Ice Index Version 4, with 45 Arctic September-to-next-March pairs for summer years 1979–2023 and 46 Antarctic February-to-September pairs for 1979–2024. We removed separate linear year trends and compared winter variance after the lowest third of summer residuals with variance after other summers. The Arctic variance ratio was 0.696, with a 95% three-year paired block interval from 0.184 to 1.786. The Antarctic ratio was 1.477, with an interval from 0.570 to 2.591. Both intervals include one. The Antarctic ratio was 0.513 when the record ended in 2015, and its median absolute deviation ratio was below one in the full record. These records do not establish a stable change in winter dispersion after low summer extent. We also reproduce a prior campaign endpoint result and label it as a check. Few low summers, changing climate states, retrospective groups, and extent-only data limit inference. The package preserves group evidence, resampling draws, code, source hashes, and an independent numerical audit.

sea ice · conditional variance · winter dispersion · Arctic · Antarctic · null result

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References

8
  1. usesdoi:10.7265/a98x-0f50

    Daily extent records for both hemispheres, with target months through 2024.

  2. doi:10.1175/2010JCLI3775.1

    Prior work on seasonal memory and its return.

  3. doi:10.1029/2010GL045698

    Model intervention study of summer ice recovery; the present regression does not identify that mechanism.

  4. useshttps://nsidc.org/sites/default/files/documents/user-guide/g02135-v004-userguide.pdf

    Data format, missing days, and input sensor change.

  5. usesArctic summer extent had little link to next March extent in 45 seasons from 1979 to 2023 sci:sha256:994fd251ad5c9a3e420583a702f1512b4fd49d7e3894a78bcb00d131be804d96

    Prior endpoint result reproduced as a supporting check. New analysis tests conditional winter dispersion on overlapping data.

  6. Two-slope tests find no clear low-to-high summer difference in 46 sea ice seasons per hemisphere sci:sha256:1e1be43754a0134d46e88c5b96f9f25657919ce4f4b073fca665d1ff6df9b1ac

    Prior low-to-high mean-slope test. We instead test dispersion within summer groups.

  7. Arctic extent reached 11 million square kilometres later despite faster 9-to-11 expansion in 1989-2024 sci:sha256:0b836e161c7097242f609860d9e26db3869b4a91110b7150bfea429b2e0389e9

    Prior fixed-range autumn timing test read for scope.

  8. doi:10.1175/JCLI-D-23-0479.1

    Prior evidence of changes in Antarctic summer variance and memory.

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