{"record_type":"pith_number_record","schema_url":"https://pith.science/schemas/pith-number/v1.json","pith_number":"pith:2024:KJT4VP4PEBZPHHTHSXUDLKUFDX","short_pith_number":"pith:KJT4VP4P","schema_version":"1.0","canonical_sha256":"5267cabf8f2072f39e6795e835aa851de7072bbd057d67b6c9e42bbe39585fa9","source":{"kind":"arxiv","id":"2401.12931","version":1},"attestation_state":"computed","paper":{"title":"Mars 2020 Perseverance rover studies of the Martian atmosphere over Jezero from pressure measurements","license":"http://creativecommons.org/licenses/by/4.0/","headline":"","cross_cats":[],"primary_cat":"astro-ph.EP","authors_text":"A.-M. Harri, A. Munguira, A. S\\'anchez-Lavega, A. Vicente-Retortillo, C. Newman, Daniel Vi\\'udez-Moreiras, D. Banfield, D. Toledo, G. M. Mart\\'inez, I. Arruego, I. Jaakonaho, J. A. Rodr\\'iguez-Manfredi, J. G\\'omez-Elvira, J. Pla-Garc\\'ia, J. Polkko, L. K. Tamppari, M. de la Torre Ju\\'arez, M. Genzer, M. Hieta, M. T. Lemmon, M. Wolff, R. Hueso, S. Guzewich, T. Bertrand, T. del Rio-Gaztelurrutia, T. M\\\"akinen, V. Ap\\'estigue","submitted_at":"2024-01-23T17:33:59Z","abstract_excerpt":"The pressure sensors on Mars rover Perseverance measure the pressure field in the Jezero crater on regular hourly basis starting in sol 15 after landing. The present study extends up to sol 460 encompassing the range of solar longitudes from Ls 13{\\deg} - 241{\\deg} (Martian Year (MY) 36). The data show the changing daily pressure cycle, the sol-to-sol seasonal evolution of the mean pressure field driven by the CO2 sublimation and deposition cycle at the poles, the characterization of up to six components of the atmospheric tides and their relationship to dust content in the atmosphere. They al"},"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":"2401.12931","kind":"arxiv","version":1},"metadata":{"license":"http://creativecommons.org/licenses/by/4.0/","primary_cat":"astro-ph.EP","submitted_at":"2024-01-23T17:33:59Z","cross_cats_sorted":[],"title_canon_sha256":"38b0380cdbc4cda746b1457ac34d6437e939e5d3c7b5d8256ed988ed767afcd9","abstract_canon_sha256":"55e280896d5f21f4208fd6282333c6316c43a5e6a42534b213de9919f5fd3893"},"schema_version":"1.0"},"receipt":{"kind":"pith_receipt","key_id":"pith-v1-2026-05","algorithm":"ed25519","signed_at":"2026-07-05T07:39:13.153178Z","signature_b64":"7jcZPr2xVjfTAv9xn3cHsVHnA2c3ALL6inCiGPXgN9f1lrIpS2gzlAj3Of2y8uLPTr0QMHG5s6r/vxraJwoAAA==","signed_message":"canonical_sha256_bytes","builder_version":"pith-number-builder-2026-05-17-v1","receipt_version":"0.3","canonical_sha256":"5267cabf8f2072f39e6795e835aa851de7072bbd057d67b6c9e42bbe39585fa9","last_reissued_at":"2026-07-05T07:39:13.152638Z","signature_status":"signed_v1","first_computed_at":"2026-07-05T07:39:13.152638Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54"},"graph_snapshot":{"paper":{"title":"Mars 2020 Perseverance rover studies of the Martian atmosphere over Jezero from pressure measurements","license":"http://creativecommons.org/licenses/by/4.0/","headline":"","cross_cats":[],"primary_cat":"astro-ph.EP","authors_text":"A.-M. Harri, A. Munguira, A. S\\'anchez-Lavega, A. Vicente-Retortillo, C. Newman, Daniel Vi\\'udez-Moreiras, D. Banfield, D. Toledo, G. M. Mart\\'inez, I. Arruego, I. Jaakonaho, J. A. Rodr\\'iguez-Manfredi, J. G\\'omez-Elvira, J. Pla-Garc\\'ia, J. Polkko, L. K. Tamppari, M. de la Torre Ju\\'arez, M. Genzer, M. Hieta, M. T. Lemmon, M. Wolff, R. Hueso, S. Guzewich, T. Bertrand, T. del Rio-Gaztelurrutia, T. M\\\"akinen, V. Ap\\'estigue","submitted_at":"2024-01-23T17:33:59Z","abstract_excerpt":"The pressure sensors on Mars rover Perseverance measure the pressure field in the Jezero crater on regular hourly basis starting in sol 15 after landing. The present study extends up to sol 460 encompassing the range of solar longitudes from Ls 13{\\deg} - 241{\\deg} (Martian Year (MY) 36). The data show the changing daily pressure cycle, the sol-to-sol seasonal evolution of the mean pressure field driven by the CO2 sublimation and deposition cycle at the poles, the characterization of up to six components of the atmospheric tides and their relationship to dust content in the atmosphere. They al"},"claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"2401.12931","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/2401.12931/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":"2401.12931","created_at":"2026-07-05T07:39:13.152687+00:00"},{"alias_kind":"arxiv_version","alias_value":"2401.12931v1","created_at":"2026-07-05T07:39:13.152687+00:00"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.2401.12931","created_at":"2026-07-05T07:39:13.152687+00:00"},{"alias_kind":"pith_short_12","alias_value":"KJT4VP4PEBZP","created_at":"2026-07-05T07:39:13.152687+00:00"},{"alias_kind":"pith_short_16","alias_value":"KJT4VP4PEBZPHHTH","created_at":"2026-07-05T07:39:13.152687+00:00"},{"alias_kind":"pith_short_8","alias_value":"KJT4VP4P","created_at":"2026-07-05T07:39:13.152687+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/KJT4VP4PEBZPHHTHSXUDLKUFDX","json":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX.json","graph_json":"https://pith.science/api/pith-number/KJT4VP4PEBZPHHTHSXUDLKUFDX/graph.json","events_json":"https://pith.science/api/pith-number/KJT4VP4PEBZPHHTHSXUDLKUFDX/events.json","paper":"https://pith.science/paper/KJT4VP4P"},"agent_actions":{"view_html":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX","download_json":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX.json","view_paper":"https://pith.science/paper/KJT4VP4P","resolve_alias":"https://pith.science/api/pith-number/resolve?arxiv=2401.12931&json=true","fetch_graph":"https://pith.science/api/pith-number/KJT4VP4PEBZPHHTHSXUDLKUFDX/graph.json","fetch_events":"https://pith.science/api/pith-number/KJT4VP4PEBZPHHTHSXUDLKUFDX/events.json","actions":{"anchor_timestamp":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX/action/timestamp_anchor","attest_storage":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX/action/storage_attestation","attest_author":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX/action/author_attestation","sign_citation":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX/action/citation_signature","submit_replication":"https://pith.science/pith/KJT4VP4PEBZPHHTHSXUDLKUFDX/action/replication_record"}},"created_at":"2026-07-05T07:39:13.152687+00:00","updated_at":"2026-07-05T07:39:13.152687+00:00"}