{"record":{"author":{"account_ref":null,"orcid":null},"builds_on":[],"content_schema":"pubphys.content.topic/1","content_sha256":"6d348fa2d5ddf7d6f0294085feb0b6b56efd0cf30723170a948e6383e29d7c2e","created":"2026-10-03T07:17:51Z","files":[],"origin":{"assisted_by":[],"kind":"seed"},"parents":[],"salt":"27e2ab825a2610627668dcfe9908c235d089f7dd22210de8d24fdde4e41f4578","schema":"pubphys.record/2","site":"pubphys.com","target":null,"type":"topic"},"content":{"external_id":"fluid.strat-rot","field":"fluid","n":"1","review_cite":"A. Alexakis, L. Biferale, Cascades and transitions in turbulent flows, Physics Reports, 2018","review_link":"https://arxiv.org/abs/1808.06186","review_verified":"true","summary":"In the ocean and atmosphere, layers of different density and the rotation of the Earth constrain turbulent motion. How efficiently such turbulence mixes heat, salt and momentum, and in which direction it moves energy between scales, are open questions.","title":"Stratified and rotating turbulence and mixing","topic_ref":null,"why":"Ocean circulation and climate models rely on assumed mixing rates and energy pathways that come from this physics."},"attested":{"attestation":{"batch":null,"client_id":null,"id_token_sha256":null,"kind":"platform"},"record_hash":"10bf729b197d5ee7bbcb1c2f468901326f7231ccc5c3ae2967db2e962f472a39","schema":"pubphys.attested/1"},"envelope":{"attested_hash":"096003710612081212b5dbd49e09b2f0904a76308d575605bdc0853aebdac41d","platform_signature":{"key_id":"c6afc19b31429869751f06879c75cd64ea92654423d15b44be775bf1310a60da","sig":"MDz35_EhU6Iaorp_oQ8g7DmlzcEpMp9mVwXOXRR-YhXEY4VhguzTI3Jogagr4In_t1r2cq_xAekFynEL7NcdAg"},"schema":"pubphys.envelope/1"},"record_hash":"10bf729b197d5ee7bbcb1c2f468901326f7231ccc5c3ae2967db2e962f472a39","leaf_index":222}