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
References
7- 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.
- usesdoi:10.6073/pasta/7686da566d3589b95b01c530c8cd0a22
Raw and interpolated DO and temperature profiles and lake information (edi.698.4).
- usesdoi:10.6073/pasta/ac8b05bb0da19032b3df3efc21f83874
Published late-summer lake-year means used for reproduction, persistence tests and site validation (edi.624.1).
- usesdoi:10.6073/pasta/eeaa2a029eda1683f004d06da5d8d808
NTL-LTER physical limnology profiles 1981-2025 for the out-of-sample period.
- usesdoi:10.5066/P9QRKUVJ
Water Quality Portal DO and temperature profiles 2008-2025.
- 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).
- doi:10.1111/gcb.16525
Related analysis of stratification duration and hypoxia in the same lake set.
Cited by
5 publicationsPublic catalog entries on Sciscape.
- usesRemoving the deepest oxygen reading reduced gradient flags from 20 to 4 in 123 Wisconsin lake-years selected for March–June profile temperature ranges of at most 1°C
We reuse its retained unchanged NTL source CSV and metadata. All profile construction and gradient calculations are new.
- The median oxygen trend gap between middle and lower fixed sampled depths was uncertain in 149 northern lake records, 1980–2017
Its region analysis and lack of persistent individual lake slopes guide the uncertainty model and limits on interpretation. We read the catalog abstract.
- supportsAn update from prior August reduced squared oxygen forecast error by 8% against past means in 79 lake records, 2001–2017
The earlier trend test supports the need to test lake forecasts against simple means. The present test uses the same source compilation and is not independent evidence.
- supportsJune oxygen reduced August prediction error in fixed linear models for 40 northern lake records in 2001–2017
Its poor persistence of individual lake oxygen trends supports the use of simple reference models. It uses the same source compilation, so it is not independent data.
- With a 5 mg/L oxygen limit, adding an 18°C limit raised the median paired depth slope by 0.80 percentage points per decade in 149 northern lakes, 1980–2017
This related analysis limits extrapolation of individual lake oxygen trends and tests uncertainty across regions.