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Record W7029213405

The Influence of Meteorology and Hydrology on Phytoplankton Blooms in Lake Winnipeg Over the Last 37 Years (1984–2020)

2025· article· en· W7029213405 on OpenAlexaboutno aff

Bibliographic record

VenueUniversity Library (University of Saskatchewan) · 2025
Typearticle
Languageen
FieldEnvironmental Science
TopicAquatic Ecosystems and Phytoplankton Dynamics
Canadian institutionsnot available
Fundersnot available
KeywordsWetlandPhytoplanktonWatershedEutrophicationHydrology (agriculture)Aquatic ecosystemEcosystemSurface water
DOInot available

Abstract

fetched live from OpenAlex

Eutrophication poses a significant threat to the health of aquatic ecosystems worldwide. Wetlandscapes—networks of hydrologically connected wetlands—can potentially mitigate eutrophication. However, climate change and human activities have altered wetlandscapes properties, reducing their effectiveness in controlling nutrient transfer to downstream lakes. In this study, we focus on the Lake Winnipeg Watershed (LWW) in North America to examine how climate-driven changes in wetlandscape characteristics affect nutrient loading and subsequent phytoplankton blooms in Lake Winnipeg (LW) in the face of global warming. First, we developed a method for mapping wetlands and extracting wetlandscape properties using a fusion of two Landsat-derived inundation products, Global Surface Water Extent (GSWE) and Dynamic Surface Water Extent (DSWE), finding that this fusion reduced omission errors from 17% for GSWE and 18% for DSWE to 8% overall. We then mapped the properties of the LWW's wetlandscapes (i.e., number, size, and wetland-to-wetland and wetland-to-river connectivity) from 1984 to 2020. During this period, we observed a trend toward more extensive wetlands that are better interconnected and have increased hydrological connectivity to LW (p ≤ 0.1). We then created the longest time series of chlorophyll-a (Chl-a), a proxy for phytoplankton biomass, for LW (1984–2023) using Landsat data and LW basins-specific Chl-a prediction models, demonstrating that accounting for the variance in optical complexity within lake’s basins can improve Chl-a predictions (p ≤ 0.1). The Chl-a time series showed significant increases in the frequency, magnitude, and extent of LW phytoplankton blooms concomitant with the observed changes in the wetlandscape properties. The two major basins of LW responded differently to climate-driven changes. In the north basin, climate-driven wetter conditions with larger, connected wetlands elevated nutrient loading and intensified phytoplankton blooms (p ≤ 0.1). This phenomenon was not observed in the south basin (p > 0.1). Within the watershed, those sub-watersheds with shorter flow distances to LW exhibited stronger correlations with blooms (p ≤ 0.1), while those with longer flow paths showed weak or no correlations, likely due to nutrient retention and transformation. Incorporating runoff travel distance into wetlandscape assessments improved correlations with nutrient inputs and bloom dynamics. A second climate factor, rising temperature, further exacerbated bloom extent and magnitude (p ≤ 0.1). As climate change amplifies nutrient loading and warming in LW, prioritizing wetlandscape management in high- impact sub-watersheds is essential for sustainable water quality. Using globally available Landsat products, the methodologies developed here provide scalable tools for assessing wetlandscape impacts on water quality worldwide.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.048
Threshold uncertainty score0.968

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0010.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.002
GPT teacher head0.156
Teacher spread0.154 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2025
Admission routes1
Has abstractyes

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