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Deep-water oxygen loss is a shared decline across 195 temperate lakes, but lake-specific trends did not persist between 1990–2003 and 2004–2017 or predict 2018–2025

Jane et al. (2021) reported a widespread decrease of late-summer dissolved oxygen (DO) in temperate lakes. We used the public data (EDI edi.698.4, edi.624.1) to test two questions: is the network-wide decrease robust, and do the trends of individual lakes persist in time? We reproduced the published medians (deep DO -0.121, surface -0.110 mg/L per decade). A Python rebuild of the profile pipeline matched the published lake-year means (median difference 0.003 mg/L). The deep-water decrease is robust. With a bootstrap over 23 regions (US states or countries), the median deep trend is -0.12 mg/L per decade (95% CI -0.27 to -0.06), and all 10 regions with at least 5 lakes are negative. A fixed-depth layer with a sampling-date correction gives -0.15 (CI -0.24 to -0.08). But lake-specific trends do not persist. Deep-water lake slopes in 1990-2003 do not predict slopes in 2004-2017 (r = -0.10, 158 lakes; with a 4-year gap r = -0.15, CI -0.29 to -0.0004). A simulation with lake-specific AR(1) noise rejects a persistent lake trend SD of 0.3 mg/L per decade or more (p = 0.033). A random-effects meta-analysis of full-period slopes gives 0.30. For surface DO, the associations of trends with surface temperature and latitude change sign between the periods. New 2018-2025 profiles from the same monitoring sites (Water Quality Portal, NTL-LTER) reproduced the published values exactly at 140 surface and 71 deep lakes. In 95 surface and 16 deep lakes with enough data, the median change from 2008-2017 to 2018-2025 was -0.03 mg/L (CI -0.14 to +0.08) and -0.10 mg/L (CI -0.27 to +0.41). These agree with the network trend but do not confirm it. Extrapolation of each lake's surface trend predicted 2018-2025 worse than the 2008-2017 mean (MAE +0.18 mg/L, CI +0.10 to +0.28). Limits: the persistence bound is for 14-year linear trends with independent AR(1) noise. The out-of-sample lakes are mostly in Minnesota, New Hampshire and Wisconsin, and the deep test has low power.

lake deoxygenation · dissolved oxygen · hypolimnion · trend persistence · out-of-sample test · reproduction · Water Quality Portal · NTL-LTER · regional clustering · temperate lakes · long-term monitoring · random-effects meta-analysis

Admitted 5 citing publications

References

7
  1. supportsdoi:10.1038/s41586-021-03550-y

    We reproduce its median trends and show that the network-wide deep-water decrease is robust to sampling date, depth definition and regional clustering. We also show that lake-specific trend magnitudes did not persist between periods.

  2. usesdoi:10.6073/pasta/7686da566d3589b95b01c530c8cd0a22

    Raw and interpolated DO and temperature profiles and lake information (edi.698.4).

  3. usesdoi:10.6073/pasta/ac8b05bb0da19032b3df3efc21f83874

    Published late-summer lake-year means used for reproduction, persistence tests and site validation (edi.624.1).

  4. usesdoi:10.6073/pasta/eeaa2a029eda1683f004d06da5d8d808

    NTL-LTER physical limnology profiles 1981-2025 for the out-of-sample period.

  5. usesdoi:10.5066/P9QRKUVJ

    Water Quality Portal DO and temperature profiles 2008-2025.

  6. supportsSampling-date drift hid part of the deep-water oxygen loss in 183 temperate lakes (1941–2017), and in 120 northern lakes the loss was present by mid-June with no change in summer depletion rate sci:sha256:790bf5319d249f07cc3718b6795d9676c2e772b0001b7555cab4644dc9ddff0b

    Our independent rebuild also finds that sampling-date correction and fixed-depth layers make the median deep-water trend slightly more negative (-0.14 to -0.15 mg/L per decade).

  7. doi:10.1111/gcb.16525

    Related analysis of stratification duration and hypoxia in the same lake set.

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