{"record_type":"pith_number_record","schema_url":"https://pith.science/schemas/pith-number/v1.json","pith_number":"pith:2024:C6LQ274XTOOA7YZCUEBWR2FW4D","short_pith_number":"pith:C6LQ274X","schema_version":"1.0","canonical_sha256":"17970d7f979b9c0fe322a10368e8b6e0f151a186057b4af8941045e0fda2d759","source":{"kind":"arxiv","id":"2412.11987","version":1},"attestation_state":"computed","paper":{"title":"Convective shutdown in the atmospheres of lava worlds","license":"http://creativecommons.org/licenses/by-nc-sa/4.0/","headline":"","cross_cats":[],"primary_cat":"astro-ph.EP","authors_text":"Harrison Nicholls, Laurent Soucasse, Raymond T. Pierrehumbert, Stef Smeets, Tim Lichtenberg","submitted_at":"2024-12-16T17:11:31Z","abstract_excerpt":"Atmospheric energy transport is central to the cooling of primordial magma oceans. Theoretical studies of atmospheres on lava planets have assumed that convection is the only process involved in setting the atmospheric temperature structure. This significantly influences the ability for a magma ocean to cool. It has been suggested that convective stability in these atmospheres could preclude permanent magma oceans. We develop a new 1D radiative-convective model in order to investigate when the atmospheres overlying magma oceans are convectively stable. Using a coupled interior-atmosphere frame"},"verification_status":{"content_addressed":true,"pith_receipt":true,"author_attested":false,"weak_author_claims":0,"strong_author_claims":0,"externally_anchored":false,"storage_verified":false,"citation_signatures":0,"replication_records":0,"graph_snapshot":true,"references_resolved":false,"formal_links_present":false},"canonical_record":{"source":{"id":"2412.11987","kind":"arxiv","version":1},"metadata":{"license":"http://creativecommons.org/licenses/by-nc-sa/4.0/","primary_cat":"astro-ph.EP","submitted_at":"2024-12-16T17:11:31Z","cross_cats_sorted":[],"title_canon_sha256":"d1d24cce7f55a0fde6edb87ddfa8f03b3cbbf88f4366f673a834180809a56626","abstract_canon_sha256":"edeba2d87fca5af7d6b5935d0c82b0c10be74896c0b4d8beb5bb1f9252be6636"},"schema_version":"1.0"},"receipt":{"kind":"pith_receipt","key_id":"pith-v1-2026-05","algorithm":"ed25519","signed_at":"2026-07-05T09:49:54.932214Z","signature_b64":"bzw01kr/7C5JcSofXZ5jqSACe4Y9zpsmjvyfDQwxvZA1n9woQYm0mPJzfDyGmKij8B5gxhpQXQj5hzJ9ipRLCg==","signed_message":"canonical_sha256_bytes","builder_version":"pith-number-builder-2026-05-17-v1","receipt_version":"0.3","canonical_sha256":"17970d7f979b9c0fe322a10368e8b6e0f151a186057b4af8941045e0fda2d759","last_reissued_at":"2026-07-05T09:49:54.931678Z","signature_status":"signed_v1","first_computed_at":"2026-07-05T09:49:54.931678Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54"},"graph_snapshot":{"paper":{"title":"Convective shutdown in the atmospheres of lava worlds","license":"http://creativecommons.org/licenses/by-nc-sa/4.0/","headline":"","cross_cats":[],"primary_cat":"astro-ph.EP","authors_text":"Harrison Nicholls, Laurent Soucasse, Raymond T. Pierrehumbert, Stef Smeets, Tim Lichtenberg","submitted_at":"2024-12-16T17:11:31Z","abstract_excerpt":"Atmospheric energy transport is central to the cooling of primordial magma oceans. Theoretical studies of atmospheres on lava planets have assumed that convection is the only process involved in setting the atmospheric temperature structure. This significantly influences the ability for a magma ocean to cool. It has been suggested that convective stability in these atmospheres could preclude permanent magma oceans. We develop a new 1D radiative-convective model in order to investigate when the atmospheres overlying magma oceans are convectively stable. Using a coupled interior-atmosphere frame"},"claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"2412.11987","kind":"arxiv","version":1},"verdict":{"id":null,"model_set":{},"created_at":null,"strongest_claim":"","one_line_summary":"","pipeline_version":null,"weakest_assumption":"","pith_extraction_headline":""},"integrity":{"clean":true,"summary":{"advisory":0,"critical":0,"by_detector":{},"informational":0},"endpoint":"/pith/2412.11987/integrity.json","findings":[],"available":true,"detectors_run":[],"snapshot_sha256":"c28c3603d3b5d939e8dc4c7e95fa8dfce3d595e45f758748cecf8e644a296938"},"references":{"count":0,"sample":[],"resolved_work":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57","internal_anchors":0},"formal_canon":{"evidence_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"author_claims":{"count":0,"strong_count":0,"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"builder_version":"pith-number-builder-2026-05-17-v1"},"aliases":[{"alias_kind":"arxiv","alias_value":"2412.11987","created_at":"2026-07-05T09:49:54.931750+00:00"},{"alias_kind":"arxiv_version","alias_value":"2412.11987v1","created_at":"2026-07-05T09:49:54.931750+00:00"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.2412.11987","created_at":"2026-07-05T09:49:54.931750+00:00"},{"alias_kind":"pith_short_12","alias_value":"C6LQ274XTOOA","created_at":"2026-07-05T09:49:54.931750+00:00"},{"alias_kind":"pith_short_16","alias_value":"C6LQ274XTOOA7YZC","created_at":"2026-07-05T09:49:54.931750+00:00"},{"alias_kind":"pith_short_8","alias_value":"C6LQ274X","created_at":"2026-07-05T09:49:54.931750+00:00"}],"events":[],"event_summary":{},"paper_claims":[],"inbound_citations":{"count":0,"internal_anchor_count":0,"sample":[]},"formal_canon":{"evidence_count":0,"sample":[],"anchors":[]},"links":{"html":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D","json":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D.json","graph_json":"https://pith.science/api/pith-number/C6LQ274XTOOA7YZCUEBWR2FW4D/graph.json","events_json":"https://pith.science/api/pith-number/C6LQ274XTOOA7YZCUEBWR2FW4D/events.json","paper":"https://pith.science/paper/C6LQ274X"},"agent_actions":{"view_html":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D","download_json":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D.json","view_paper":"https://pith.science/paper/C6LQ274X","resolve_alias":"https://pith.science/api/pith-number/resolve?arxiv=2412.11987&json=true","fetch_graph":"https://pith.science/api/pith-number/C6LQ274XTOOA7YZCUEBWR2FW4D/graph.json","fetch_events":"https://pith.science/api/pith-number/C6LQ274XTOOA7YZCUEBWR2FW4D/events.json","actions":{"anchor_timestamp":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D/action/timestamp_anchor","attest_storage":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D/action/storage_attestation","attest_author":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D/action/author_attestation","sign_citation":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D/action/citation_signature","submit_replication":"https://pith.science/pith/C6LQ274XTOOA7YZCUEBWR2FW4D/action/replication_record"}},"created_at":"2026-07-05T09:49:54.931750+00:00","updated_at":"2026-07-05T09:49:54.931750+00:00"}