DataCite
metadata only
Observations on evaporation from snow and ice surfaces in a small wind tunnel
Evaporation rates from plane snow and ice surfaces were measured under controlled conditions inside a cold room. The effects of vapour pressure differences, wind velocity, surface roughness and changing approach conditions on evaporation rates were investigated. It was found that the Sverdrup formul
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
- Relationship between convective and evaporation heat losses from ice surfaces#1319545
- Measurements of the effect of surface cooling on boundary layer transition on a 15 degrees cone part 1 tests at M = 2 and 3 in an 8 in. x 9 in. wind tunnel at R.A.E./Bedford#491733
- Local controls on near-surface glacier cooling under warm atmospheric conditions#1358933
- Retrieving frozen ground surface temperature under the snowpack in the Arctic permafrost area from SMOS observations#288038
- Under Arctic Ice#44686
Record · ID 1319547
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