Weather and landscape morphology drive thermal regime variation among Mývatn ponds, and implications for resident Arctic charr
The study examined how weather and local landscape morphology influence thermal stratification regimes across ponds in the unique cave-pond system near Mývatn, Iceland, and linked these physical differences to growth and body condition of resident Arctic charr. Using comparisons between two ponds that differed in exposure to warm air and wind—modulated by cave opening orientation and catchment topography—the authors found that wind-driven mixing was stronger in the more exposed pond, while only the more sheltered pond remained continuously mixed. They reported that Arctic charr growth rates and body condition aligned with temperature-driven constraints on growth and metabolism in the cooler continuously mixed pond, but noted that prey limitation could also affect the observed patterns. This paper does not explicitly discuss endometriosis or adenomyosis; it was included in the corpus via a keyword match in the upstream search index.
Read from the paper's body, not the abstract. Not a substitute for reading the paper. No clinical advice. How this works
Full text
2,635 characters
· extracted from
oa-doi-fallback
· click to expand
Text is read by the "Ask this paper" AI Q&A widget below. Extraction quality varies by source — PMC NXML preserves structure cleanly, OA-HTML may include some navigation residue, and OA-PDF can have broken hyphenation. The publisher copy (via DOI) is the canonical version.
My notes (saved in your browser only)
Answers must be backed by verbatim quotes from this paper's full text. Hallucinated quotes are dropped automatically; if no verbatim passage answers the question, we say so. How this works
Citation neighborhood (no data yet)
We don't have any in-corpus citations linked to this paper yet. This is a recent paper (2025) — citers typically take a year or two to land, and the OpenAlex reference graph may still be filling in.
Source provenance
- europepmc
- last seen: 2026-05-20T01:45:00.602351+00:00