Open-ocean convection¶
Marshall, J., & Schott, F. (1999). Open-ocean convection: Observations, theory, and models. Reviews of Geophysics, 37(1), 1-64.
Cited by¶
2 citations across 2 artifacts.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Brunt–Väisälä Frequency
- Downwelling
- In the deep-water formation regions of the North Atlantic — the Labrador Sea and the Nordic Seas — seasonal surface cooling drives convective plumes that sink to 1,500–2,000 m
This sourceReviews of Geophysics, 1999. The canonical review of open-ocean deep convection, describing it as intermittent winter-storm-triggered overturning that changes the properties of large volumes of water.
Supported in partVerified against the publisher's abstract
“the properties of large volumes of water are changed by intermittent, deep‐reaching convection, triggered by winter storms”
- In the deep-water formation regions of the North Atlantic — the Labrador Sea and the Nordic Seas — seasonal surface cooling drives convective plumes that sink to 1,500–2,000 m
Verification¶
Does it exist? Confirmed. This work's DOI resolves to a registered record, which fixes its identity. That is all it fixes.
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Links previously used in the corpus¶
Before the registry existed this work was also linked 1 other way.
Registry ID ref:b8bf0a9931b2 · see in the full table