PANGAEA
metadata only
CC BY 3.0
Solar radiation over and under sea ice during the POLARSTERN cruise ARK-XXVI/3 (TransArc) in summer 2011
Arctic sea ice has declined and become thinner and younger (more seasonal) during the last decade. One consequence of this is that the surface energy budget of the Arctic Ocean is changing. While the role of surface albedo has been studied intensively, it is still widely unknown how much light penet
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
- Research priorities for the coupled Arctic land–ocean carbon cycle: integrating scientific and policy perspectives#171089
- Climate and Penguin-Mediated Carbon Burial Hotspots in Coastal Lakes of East Antarctica#339905
- The Seasonal Sun.#333094
- Terrestrial Arthropod Responses to Arctic Cryosphere Degradation.#465306
- Evidence against dust-mediated control of glacial-interglacial changes in atmospheric CO2.#1039366
Record · ID 1204803
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