Hypoxia in Chesapeake Bay, 1950–2001: Long-term change in relation to nutrient loading and river flow¶
Hagy. (2004). Hypoxia in Chesapeake Bay, 1950–2001: Long-term change in relation to nutrient loading and river flow: Long-term change in relation to nutrient loading and river flow. Estuaries.
Cited by¶
1 citation across 1 artifact.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Estuarine Circulation
- The steady two-layer exchange has a signature ecological consequence — in summer, stratification seals bottom water off from the oxygenated surface, and the decay of sinking organic matter drives a large seasonal hypoxic "dead zone," one of the most-studied in the world
This sourceThe long-term record of expanding mid-summer hypoxia in Chesapeake Bay and its relation to nitrate loading and river flow.
Supported in partVerified against the publisher's abstract
“the volume of hypoxic water in mid summer increased substantially and at an accelerating rate”
- The steady two-layer exchange has a signature ecological consequence — in summer, stratification seals bottom water off from the oxygenated surface, and the decay of sinking organic matter drives a large seasonal hypoxic "dead zone," one of the most-studied in the world
Verification¶
Does it exist? Not checked yet. This work's DOI is recorded above but has not been resolved against an external catalogue, so nothing here confirms the work exists.
Does it back the claim? Read against the text for 1 of 1 citation: 1 supported in part. Each verdict is shown under its citation below, with what in the work backs the sentence.
Support is checked per citation rather than per work — the same source can be cited soundly in one article and wrongly in another. Per-citation recording began recently, so a citation with no recorded check is a gap in the record rather than evidence it went unchecked.
See how references were verified.
Registry ID ref:21968232cfd9 · see in the full table