HAL (France)
open access
Development of overturning circulation in sloping waterbodies due to surface cooling
Cooling the surface of freshwater bodies, whose temperatures are above the temperature of maximum density, can generate differential cooling between shallow and deep regions. When surface cooling occurs over a long enough period, the thermally induced cross-shore pressure gradient may drive an overt
Conceptio Open Archive
Analyze & explore related research in Conceptio
Connect this record directly into your research workflow or AI agent. Explore citations across open repositories, query full text, and export structured proof bundles.
This document is indexed with metadata only: full text is not available in the archive for this record. Open the official source ↗
Related documents
- Lake sediment heatwaves under global warming#248694
- The Influence of Surface Fluxes on Export of Southern Ocean Intermediate and Mode Water in Coupled Climate Models#333878
- Sea surface temperatures calculated with modern analog technique on sediment core MD95-2012#145177
- Bottom Friction in a Baroclinic Ocean: Influences on Sea Level and Slope Currents#1220231
- Five years operational derivation of multichannel sea surface temperature at the German Remote Sensing Data Center#642024
Record · ID 1219538
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Retrieved via Conceptio: every document is proof-bundled with source, license, and retrieval metadata.
Bring this data into your agent: Connect via MCP or API · 20 free credits to start · no card required
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive
Read the Docs → · View CLI source on GitHub · Conceptio Open Knowledge Archive