{"as_of":"2026-08-17T21:17:00Z","caps":{"database_statements":6,"inbound":100,"outbound":100},"context_digest":"sha256:dddb2b5169a62cc27e11c86673903903882c74d7c91e3c75a79f8b218c8f4a9f","coverage":[{"denominator":58,"lane":"reference_resolution","note":"Typed states for the displayed outbound observations.","records_observed":58,"source":"paper_references, paper_reference_links","source_observed_at":"2026-08-16T12:40:48.002003Z","state":"measured"},{"denominator":60,"lane":"standing_notices","note":"One-hop event checks from named stored sources.","records_observed":60,"source":"scholarly_work_events, retraction_status_cache","source_observed_at":"2026-08-17T06:30:58.91139+00:00","state":"measured"},{"denominator":2,"lane":"inbound_itemization","note":"Pith citing papers itemized under the disclosed page cap.","records_observed":2,"source":"paper_references, paper_reference_links","source_observed_at":"2026-08-09T23:28:40.107167Z","state":"measured"},{"denominator":1,"lane":"external_citation_measurements","note":"A source-named dated measurement, never combined with another source.","records_observed":0,"source":"pith","source_observed_at":"2026-08-06T16:51:55.402741Z","state":"measured"}],"external_citation_measurements":[],"inbound":[{"citation":{"cited_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":"2504.12030","snapshot_observed_at":"2026-08-09T23:28:40.107167Z","title":null,"venue":null,"work_id":null,"year":2025},"citing_paper":{"arxiv_id":"2501.18477","last_updated":"2025-08-29T17:04:43Z","snapshot_observed_at":"2026-08-17T02:13:56.845599Z","submitted_at":"2025-01-30T16:51:02Z","title":"A Comprehensive Reanalysis of K2-18 b's JWST NIRISS+NIRSpec Transmission Spectrum","version":2},"reference_index":85,"source":"arxiv_source","source_observed_at":"2026-08-09T23:28:40.107167Z"},"links":{"cited_paper":"/paper/2504.12030","citing_paper":"/paper/2501.18477"},"observation_digest":"sha256:72daa34efc0c7c2b486d411acc97b9da48d51a0be73c74d0c018f6fe26ae3a6f","observation_id":"71c07c44-d719-4dc0-a1a6-4f3423e6ecc2","resolution":{"observed_at":"2026-08-09T23:28:40.107167Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"cited_work":{"arxiv_id":"2504.12030","doi":null,"metadata_source":"pith","pith_arxiv_id":"2504.12030","snapshot_observed_at":"2026-08-06T16:51:55.402741Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","venue":"astro-ph.EP","work_id":"e08d6d6a-e0fc-4c8d-9346-c323e062445a","year":2025},"citing_paper":{"arxiv_id":"2507.12622","last_updated":"2025-07-16T20:37:03Z","snapshot_observed_at":"2026-08-16T08:54:20.965191Z","submitted_at":"2025-07-16T20:37:03Z","title":"A water-rich interior in the temperate sub-Neptune K2-18 b revealed by JWST","version":1},"reference_index":61,"source":"arxiv_source","source_observed_at":"2026-08-06T16:51:49.225283Z"},"links":{"cited_paper":"/paper/2504.12030","citing_paper":"/paper/2507.12622"},"observation_digest":"sha256:e956c38988eeb6049b4b1d118c6830416932d9890dbe6bb6e3bea5bfddfeba91","observation_id":"a5cf9f05-fba9-41b8-b533-d4f29a365ce3","resolution":{"observed_at":"2026-08-06T16:51:55.480622Z","resolver_source":"local_arxiv","status":"verified_exact"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}}],"links":{"evidence":"/evidence","html":"/paper/2504.12030/citation-record","integrity":"/paper/2504.12030/integrity","json":"/paper/2504.12030/citation-record.json","paper":"/paper/2504.12030"},"outbound":[{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.775904Z","title":", \" * write output.state after.block = add.period write newline","venue":null,"work_id":null,"year":null},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":1,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.775904Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:8498eb238a30b7c31733392b54757bdf7379196e964e75a9f481995f7dadcbe1","observation_id":"ed9b2217-87b2-4899-ac27-3a2ce3a7f1d2","resolution":{"observed_at":"2026-08-16T12:40:47.775904Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.781344Z","title":"write newline","venue":null,"work_id":null,"year":null},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":2,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.781344Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:35615c21cb4e15bb04b868e54c12da02c1f85c4a2364b78a82e9b1577d6c742e","observation_id":"7f8b6ff2-0472-466b-b937-8a7961c8d90e","resolution":{"observed_at":"2026-08-16T12:40:47.781344Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.785442Z","title":"r\\ L.ꞓkF & &QCZ7 CǺ? >w cױT T d\\Ә!9^T1fx4 O.0&W ɱlxr ;s/٭m cv ldWu + r1xHj_ j [z c> V¬ Yf(J#ŲO","venue":null,"work_id":null,"year":2021},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":3,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.785442Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:0d94d576ece5fe658f515fb85550509f741d38f353ae78a1cfad6a2b51e92b7c","observation_id":"9dd7fbb1-6c2c-43d7-911b-c74c33962f73","resolution":{"observed_at":"2026-08-16T12:40:47.785442Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.792900Z","title":null,"venue":null,"work_id":null,"year":1984},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":4,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.792900Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:310ac38be472248e646fb476f61a176e3ee7936fb33dc25c1c973936d13f50d1","observation_id":"91d11d14-9588-4a00-af04-b1fb36f4afe7","resolution":{"observed_at":"2026-08-16T12:40:47.792900Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.797164Z","title":"2017, , 834, 187, 10.3847/1538-4357/834/2/187","venue":null,"work_id":null,"year":2017},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":5,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.797164Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:291ba1c5fe00178cff478cc3d79b01d371a25dc7585a854bd2b0f97daf7eae61","observation_id":"19b0a3cf-8f49-407c-b525-cd62ce53bc13","resolution":{"observed_at":"2026-08-16T12:40:47.797164Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.801822Z","title":"2019, , 887, L14, 10.3847/2041-8213/ab59dc","venue":null,"work_id":null,"year":2019},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":6,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.801822Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:5452a5e23f887a8a33fdafd4d2cd21f99c685c91447c5d61e7fc8b94252f91b8","observation_id":"80907b9c-3ea1-4738-858a-38f693151c93","resolution":{"observed_at":"2026-08-16T12:40:47.801822Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":{"arxiv_id":"2403.03325","last_updated":"2024-03-05T21:07:43Z","snapshot_observed_at":"2026-08-16T14:12:30.090800Z","submitted_at":"2024-03-05T21:07:43Z","title":"JWST Reveals CH$_4$, CO$_2$, and H$_2$O in a Metal-rich Miscible Atmosphere on a Two-Earth-Radius Exoplanet","version":1},"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":"2403.03325","snapshot_observed_at":"2026-08-16T12:40:47.806516Z","title":"2024, arXiv e-prints, arXiv:2403.03325, 10.48550/arXiv.2403.03325","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":7,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.806516Z"},"links":{"cited_paper":"/paper/2403.03325","citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:b8a37fe39b70abbd54499f7b874993b3c9d61baaf5f920911e82a872e6c1084c","observation_id":"5e7ab988-5a01-440f-879f-a30f5341763c","resolution":{"observed_at":"2026-08-16T12:40:47.806516Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":{"arxiv_id":"2011.10424","last_updated":"2022-05-12T15:40:23Z","snapshot_observed_at":"2026-08-17T00:26:09.068669Z","submitted_at":"2020-11-20T14:42:13Z","title":"Methane as a dominant absorber in the habitable-zone sub-Neptune K2-18 b","version":2},"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":"2011.10424","snapshot_observed_at":"2026-08-16T12:40:47.810620Z","title":"2020, arXiv e-prints, arXiv:2011.10424, 10.48550/arXiv.2011.10424","venue":null,"work_id":null,"year":2020},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":8,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.810620Z"},"links":{"cited_paper":"/paper/2011.10424","citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:0c86cbd9755bbd9618024dba59b767b74a161de31350b15a55ec52f9b6e15a79","observation_id":"b82450a4-ce8e-454d-8510-8da77fdd7560","resolution":{"observed_at":"2026-08-16T12:40:47.810620Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":"10.1016/0030-4018(73)90289-7","metadata_source":"doi_reference","pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:48.353848Z","title":"1973, Optics Communications, 9, 432, 10.1016/0030-4018(73)90289-7","venue":null,"work_id":"59dbce11-43e2-4386-bb08-76708ae83ef8","year":1973},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":9,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.814620Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:4d6547e796afbf84d78eaa75f1737a06ff0e18fe673f28edd3d37415b8cedbc7","observation_id":"829e161d-7898-4db9-9ab7-52c3c8b1c4a3","resolution":{"observed_at":"2026-08-16T12:40:48.357851Z","resolver_source":"doi","status":"verified_exact"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":"10.1029/92jd00291","metadata_source":"doi_reference","pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:48.339423Z","title":null,"venue":null,"work_id":"dae21dc1-0677-4cb7-8224-53a2f07f1717","year":1992},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":10,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.819090Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:8b3cc2869fa8b7ba29535b12846ba0180e780afd2c5cd5f27334dd6b6394c3a5","observation_id":"a14b5ddf-83af-4071-8bbb-635911ede8b8","resolution":{"observed_at":"2026-08-16T12:40:48.344303Z","resolver_source":"doi","status":"verified_exact"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.822693Z","title":"A., & Charbonneau , D","venue":null,"work_id":null,"year":2007},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":11,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.822693Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:1aff9e75b7bdd84b3b0cc9a17c3dabfbdc59484bc093ab98514fbc967e178b83","observation_id":"29637a0b-f1a3-4ac7-a432-37bc736cf558","resolution":{"observed_at":"2026-08-16T12:40:47.822693Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.827498Z","title":"2017, , 608, A35, 10.1051/0004-6361/201731558","venue":null,"work_id":null,"year":2017},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":12,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.827498Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:b2548c1bc2f9a9908ea9da274839dba6b32b9c7aa8f830951db968a1be6f9d7d","observation_id":"f828bc0b-ce8b-41fe-b5a5-fe46267688e6","resolution":{"observed_at":"2026-08-16T12:40:47.827498Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.831749Z","title":"J., & Madhusudhan , N","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":13,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.831749Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:25d7250bd58863160cf27e02ad1e29746cb6e7ada118f6013e5e88d7c693ade2","observation_id":"9f50433f-48fa-42bb-98db-0172ccf7c761","resolution":{"observed_at":"2026-08-16T12:40:47.831749Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.835910Z","title":"N., & Pilachowski , C","venue":null,"work_id":null,"year":2000},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":14,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.835910Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:bf6fda78c447fc66354a75b7aa9951a2b081352dfee2b25464217f024641c985","observation_id":"a032547b-6bac-479e-835c-7457fe5f7586","resolution":{"observed_at":"2026-08-16T12:40:47.835910Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.839436Z","title":null,"venue":null,"work_id":null,"year":2016},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":15,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.839436Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:96fab17a9b39c2ea112b936fc8cd59c75f18d0b1622bc9ef6123cf12c58c64f7","observation_id":"476b036f-c129-41f4-9a11-67de12677720","resolution":{"observed_at":"2026-08-16T12:40:47.839436Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.842980Z","title":"E., Rothman , L","venue":null,"work_id":null,"year":2022},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":16,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.842980Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:6f0c697605775417c58cd8b4bc6bf557f29b234a42fda6d2d5249dbb6a2eaab3","observation_id":"96fd17d4-4eb3-4936-b07e-34c5aa498c78","resolution":{"observed_at":"2026-08-16T12:40:47.842980Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.846235Z","title":"2010, , 520, A27, 10.1051/0004-6361/200913396","venue":null,"work_id":null,"year":2010},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":17,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.846235Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:f7aecb7fa89cdec8e708fc65f06bd65efdaa975a106333d6503bf4a7648b93f4","observation_id":"98f7019f-3c14-4744-a47a-5ae7e8e97512","resolution":{"observed_at":"2026-08-16T12:40:47.846235Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.849578Z","title":null,"venue":null,"work_id":null,"year":2020},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":18,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.849578Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:a2e51297830e0d8f1a2ece5278aeecdfe2d4ecfbe85c94945f0893572227a800","observation_id":"6e6e01ed-2c36-45eb-bdbd-9d19efe16435","resolution":{"observed_at":"2026-08-16T12:40:47.849578Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":"10.1080/00268979000100611","metadata_source":"doi_reference","pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:48.287909Z","title":"1990, Molecular Physics, 69, 803, 10.1080/00268979000100611","venue":null,"work_id":"b37ad822-a825-45e1-b9dd-b98a1b9c769b","year":1990},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":19,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.852895Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:1fd2bc2ae79029a1904289ad54b4a7e783c002b40fa3c49f73b11744d5157cc7","observation_id":"29efe187-45f1-4bc0-ac48-be34d47e6516","resolution":{"observed_at":"2026-08-16T12:40:48.291904Z","resolver_source":"doi","status":"verified_exact"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.857575Z","title":"2024, , 683, L2, 10.1051/0004-6361/202348238","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":20,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.857575Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:507aa1eddb536e4e73816f53e7ff9fba07f98bcb7b8d3a1ed90bce78b9326f70","observation_id":"2d7e5d6b-8012-44ed-aafe-9f6d945e59bf","resolution":{"observed_at":"2026-08-16T12:40:47.857575Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.863536Z","title":"2021, , 921, L8, 10.3847/2041-8213/ac1f92","venue":null,"work_id":null,"year":2021},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":21,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.863536Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:259b0b6a5bde5ac3f7af753f19ef8d33d99c71a6a564eec7dd02200d9c3ef2e0","observation_id":"f40c9b1b-6e72-4ebf-9b7b-d627291055c2","resolution":{"observed_at":"2026-08-16T12:40:47.863536Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.867780Z","title":null,"venue":null,"work_id":null,"year":2023},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":22,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.867780Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:f4b3d65a411e548abb41a6d6890274245245c7062f8f574139fc432be0e0499e","observation_id":"ade20a41-12c5-40de-b204-12e2c28468b6","resolution":{"observed_at":"2026-08-16T12:40:47.867780Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.872392Z","title":null,"venue":null,"work_id":null,"year":2025},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":23,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.872392Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:e12208d45beb73f49139853d785801d1958961dc185eb78dfa8ac0369244e1af","observation_id":"accad33c-2906-4114-a120-027201cdce9b","resolution":{"observed_at":"2026-08-16T12:40:47.872392Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.878336Z","title":"H., Wiscombe , W","venue":null,"work_id":null,"year":1976},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":24,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.878336Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:4ece03cbb4b1b627c46132c4914677ce99046d8700edf899e94ef69fa2a87cd4","observation_id":"08d02d5d-49de-4aba-a955-c072251ac314","resolution":{"observed_at":"2026-08-16T12:40:47.878336Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.881915Z","title":"F., Whitmire , D","venue":null,"work_id":null,"year":1993},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":25,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.881915Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:0b6899ca382355218c65b29a21f4b713e8a6cdcaa66d5a122f357e7f28f8fa13","observation_id":"bc308d6c-3af8-43b5-a08d-690c04a05e13","resolution":{"observed_at":"2026-08-16T12:40:47.881915Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.885386Z","title":null,"venue":null,"work_id":null,"year":2023},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":26,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.885386Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:a1e637b28b1a2a1524fd0c951db27a44bb5d6bd161426cb278934e78189821f8","observation_id":"760125a7-49ab-4f52-a62b-3de32562964a","resolution":{"observed_at":"2026-08-16T12:40:47.885386Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.888699Z","title":"S., Fegley , Jr., B., Schaefer , L., & Ford , E","venue":null,"work_id":null,"year":2019},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":27,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.888699Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:9836e127a3d13b6617069425f9537111da3ac1c15b888df1980b077726e9c6b1","observation_id":"3f4f6717-836f-4641-9208-139ffe9a5f92","resolution":{"observed_at":"2026-08-16T12:40:47.888699Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.892441Z","title":"L., D \\'e sert , J.-M., et al","venue":null,"work_id":null,"year":2014},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":28,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.892441Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:8eaa20b8ed9b2a683cc5d4634b600af15f5b99785ef1a7ceb7a69a52d634d595","observation_id":"afe1b82d-30ec-418d-9bec-b88426c3e944","resolution":{"observed_at":"2026-08-16T12:40:47.892441Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.896175Z","title":"2024, , 686, A131, 10.1051/0004-6361/202348928","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":29,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.896175Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:1e3a312474438ac21d8df26dbe2fbbf0e30d244fc07a84f35947e008676e23d8","observation_id":"026741f5-a04d-4ece-9932-1571ed6155a3","resolution":{"observed_at":"2026-08-16T12:40:47.896175Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":{"arxiv_id":"2502.13856","last_updated":"2025-02-20T19:56:15Z","snapshot_observed_at":"2026-08-16T12:56:56.317319Z","submitted_at":"2025-02-19T16:20:24Z","title":"Examining the Potential for Methyl Halide Accumulation and Detectability in Possible Hycean-Type Atmospheres","version":2},"cited_work":{"arxiv_id":"2502.13856","doi":"10.48550/arxiv.2502.13856","metadata_source":"pith","pith_arxiv_id":"2502.13856","snapshot_observed_at":"2026-08-17T00:16:13.690415Z","title":"Examining the Potential for Methyl Halide Accumulation and Detectability in Possible Hycean-Type Atmospheres","venue":"astro-ph.EP","work_id":"ac9edc66-2233-43f5-a69b-2ab0fde5e0b4","year":2025},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":30,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.899581Z"},"links":{"cited_paper":"/paper/2502.13856","citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:71bf5ca126d898a894c31abb7a24160f0639b8af6bb5c0d225d9d338882ceecd","observation_id":"2c89d385-453e-4b68-bf22-28298c141f6b","resolution":{"observed_at":"2026-08-16T12:40:48.224299Z","resolver_source":"local_arxiv","status":"metadata_mismatch"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.903536Z","title":"2003, , 591, 1220, 10.1086/375492","venue":null,"work_id":null,"year":2003},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":31,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.903536Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:53e63398aeba7229fbfc2e4a0e77628a43c022864c23cf0fe861c07f8f3a687c","observation_id":"f039ece6-10c6-4dae-93ea-a24aab48abdf","resolution":{"observed_at":"2026-08-16T12:40:47.903536Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.907063Z","title":null,"venue":null,"work_id":null,"year":2016},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":32,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.907063Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:c97bc36ca646ac73441bdb400720b9fec86e8b6e628ff2545b07e23f0401a54d","observation_id":"38889e2b-4a0d-42b7-a395-71fc827b4302","resolution":{"observed_at":"2026-08-16T12:40:47.907063Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.910651Z","title":"2015, Astrobiology, 15, 119, 10.1089/ast.2014.1231","venue":null,"work_id":null,"year":2015},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":33,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.910651Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:56a7f3c54dd51749369d279f631b4b8c803c7308809274a42fc12409832bf096","observation_id":"2795a470-c938-4e9b-9480-97f52f38d154","resolution":{"observed_at":"2026-08-16T12:40:47.910651Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.913956Z","title":"2022, Science, 377, 1211, 10.1126/science.abl7164","venue":null,"work_id":null,"year":2022},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":34,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.913956Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:f567968d812260d9cabbf168cf2740314f14351b5f66cae538b18a6165f26e3d","observation_id":"4c6c37b7-4e22-4c42-84c5-2f8045607647","resolution":{"observed_at":"2026-08-16T12:40:47.913956Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.917537Z","title":"C., Welbanks , L., Piette , A","venue":null,"work_id":null,"year":2020},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":35,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.917537Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:535c48acdcc8f6ffd50623a1f1b318faa541969891536b206329a245aec59d81","observation_id":"898ac5ee-85b4-45b4-b176-81def8aaf271","resolution":{"observed_at":"2026-08-16T12:40:47.917537Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.921295Z","title":null,"venue":null,"work_id":null,"year":2021},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":36,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.921295Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:f1b2abe368d9046a28592893583ed375484aa4b0279bbfdcf5aeda5ada6611f0","observation_id":"aa7937c4-bdba-4b3e-986b-f4ee1cd3089f","resolution":{"observed_at":"2026-08-16T12:40:47.921295Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.924910Z","title":"2023, , 956, L13, 10.3847/2041-8213/acf577","venue":null,"work_id":null,"year":2023},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":37,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.924910Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:20afc9c82baf177490e90334e1db287cb63fae958c61260e5683949d06a583fa","observation_id":"800f7048-9c12-4c7c-8cf3-c504e112b5f4","resolution":{"observed_at":"2026-08-16T12:40:47.924910Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.928402Z","title":"A., Sasselov , D., Stewart , S","venue":null,"work_id":null,"year":2010},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":38,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.928402Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:94bed26207bbb54433390795bbea2f021d9366304ee99a71370afcc7d01407f0","observation_id":"e56e9daa-2924-45c0-813c-3907a7ee21b8","resolution":{"observed_at":"2026-08-16T12:40:47.928402Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":"10.1016/j.pss.2014.11.008","metadata_source":"doi_reference","pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:48.162538Z","title":"M., Read , P","venue":null,"work_id":"e1ba1601-04ff-4f2f-815e-078411c25644","year":2015},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":39,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.932138Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:a3f964a841ec0fdbb81583c626885868336ae3aa86747e92020f58d14e9bfa38","observation_id":"b4cd1281-e7fa-4817-8c90-6c73fb73d4c2","resolution":{"observed_at":"2026-08-16T12:40:48.166022Z","resolver_source":"doi","status":"verified_exact"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.935425Z","title":"T., Morton , T","venue":null,"work_id":null,"year":2015},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":40,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.935425Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:e29195d16c848eef5e8f494085d8e6ea9d8a1be21d361e2bc5f5fed17f24819f","observation_id":"b40abbdd-5f76-4467-a50a-ed1e37ad405a","resolution":{"observed_at":"2026-08-16T12:40:47.935425Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.938680Z","title":"C., Piette , A","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":41,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.938680Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:93f16787e6fa8e94e2afbd87affed74a5b6e8b6461d66336d469f45bea69d620","observation_id":"515bbb14-bfe2-4ce9-8955-af4031b6e67a","resolution":{"observed_at":"2026-08-16T12:40:47.938680Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.943002Z","title":"2024, , 977, 188, 10.3847/1538-4357/ad8e67","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":42,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.943002Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:9a9488320ebbcfa47c0474b8834df171e9a2f89a21cc28afc844f7ab6a1efd85","observation_id":"fc5140a0-d394-4906-8ea5-e2e3cb80418f","resolution":{"observed_at":"2026-08-16T12:40:47.943002Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":"10.1117/12.3019387","metadata_source":"doi_reference","pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:48.129695Z","title":"M., Ansdell, M., Crooke, J., et al","venue":null,"work_id":"e12e5548-854a-49b4-babe-c03a106f99e3","year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":43,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.946236Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:4be1fed3695a7b07a5a60988f89773be1c8dce28cb07ff322121d7b4bfaf7ced","observation_id":"1da5f245-0558-4f11-911f-4d3d0a8caabb","resolution":{"observed_at":"2026-08-16T12:40:48.135008Z","resolver_source":"doi","status":"verified_exact"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.950017Z","title":"2024, , 974, L10, 10.3847/2041-8213/ad6f00","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":44,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.950017Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:cd519e491deba793cf127491753ea49b43845408c1809bf8bb0185241347366e","observation_id":"de38686e-76ca-464b-a3c6-e0ded9f4b60b","resolution":{"observed_at":"2026-08-16T12:40:47.950017Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":"raw_reference","pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:48.639761Z","title":null,"venue":null,"work_id":"37dccaa1-5fd2-449e-8d89-ba8c897a64f7","year":2010},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":45,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.953568Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:bb5790a47a1b59ebf395a8d180104c5d9fd1bc71fde6ecc4af338eb062c3873c","observation_id":"b0b699c0-c8e4-46fb-b8f7-7ad01e759962","resolution":{"observed_at":"2026-08-16T12:40:48.643285Z","resolver_source":"raw_fallback","status":"unresolved"},"standing_notice":{"events":[],"observation":"No event found in the named queried sources as of 2026-08-17T06:30:58.91139+00:00.","reason":null,"source_receipts":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"state":"measured"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.957009Z","title":"P., Ottiger , M., Fontanet , E., et al","venue":null,"work_id":null,"year":2022},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":46,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.957009Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:dd375b04deb75ae4e8a4e9f4619cf47f5ed7f6f36e7db4706e9c2491b9b20fde","observation_id":"9c1ca294-123c-46a4-940e-2282bd9f8657","resolution":{"observed_at":"2026-08-16T12:40:47.957009Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.961434Z","title":"E., Pica-Ciamarra , L., Holmberg , M., et al","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":47,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.961434Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:0e8b2bf18fcaeee81e91cff5e08d0ab97c88a2fbd53f942adc20cd5a4086e3ca","observation_id":"9c607df7-386f-48d6-b28a-08e5eff14480","resolution":{"observed_at":"2026-08-16T12:40:47.961434Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":{"arxiv_id":"2501.18477","last_updated":"2025-08-29T17:04:43Z","snapshot_observed_at":"2026-08-17T02:13:56.845599Z","submitted_at":"2025-01-30T16:51:02Z","title":"A Comprehensive Reanalysis of K2-18 b's JWST NIRISS+NIRSpec Transmission Spectrum","version":2},"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":"2501.18477","snapshot_observed_at":"2026-08-16T12:40:47.964782Z","title":"P., MacDonald , R","venue":null,"work_id":null,"year":2025},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":48,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.964782Z"},"links":{"cited_paper":"/paper/2501.18477","citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:6c9a0362e4e11b5a94027bbb93760761736452b0fe2cbd8f3dacb3d07198f9de","observation_id":"972b3dd0-bf93-40ad-9abf-a0b89ab4068e","resolution":{"observed_at":"2026-08-16T12:40:47.964782Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.968863Z","title":null,"venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":49,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.968863Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:e0fa0f4e9bdb4160273d14ac8ce91f98268d6bf096cd1a38ba5c2485094ee74f","observation_id":"caf38d53-340a-44f1-b730-88b9fb75c6e3","resolution":{"observed_at":"2026-08-16T12:40:47.968863Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.972180Z","title":"2005, , 92, 293, 10.1016/j.jqsrt.2004.07.025","venue":null,"work_id":null,"year":2005},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":50,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.972180Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:9e6a0f5928bcc0271f0a9054c5cdda7432c92a627f847135e311422fabc24406","observation_id":"80807680-665b-4dd5-b88f-690507449d28","resolution":{"observed_at":"2026-08-16T12:40:47.972180Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.975983Z","title":"2021, , 922, L27, 10.3847/2041-8213/ac399a","venue":null,"work_id":null,"year":2021},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":51,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.975983Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:5ce2c2a35ff7f665eb7ee9e4567654fc378c2330c695f85d9adcececed5f89b0","observation_id":"82655a25-6f27-4205-acb7-5150adbd1dd9","resolution":{"observed_at":"2026-08-16T12:40:47.975983Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.979692Z","title":"P., Tinetti , G., Tennyson , J., & Yurchenko , S","venue":null,"work_id":null,"year":2019},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":52,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.979692Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:ff284fea58fa15476a6cdff05c42392fde6fe3e34671c5d18f9b4f32ee08e1b3","observation_id":"ac6a09ea-b8c2-414b-8300-dcfbedfced98","resolution":{"observed_at":"2026-08-16T12:40:47.979692Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":{"arxiv_id":"2504.20450","last_updated":"2025-07-18T01:55:11Z","snapshot_observed_at":"2026-08-17T00:25:19.473345Z","submitted_at":"2025-04-29T05:53:42Z","title":"Atmospheric C/O Ratios of Sub-Neptunes with Magma Oceans: Homemade rather than Inherited","version":2},"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":"2504.20450","snapshot_observed_at":"2026-08-16T12:40:47.983415Z","title":"E., Grimm , S","venue":null,"work_id":null,"year":2025},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":53,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.983415Z"},"links":{"cited_paper":"/paper/2504.20450","citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:f786384c8751be8a4b3969065048feddd752ec8d40f8fd338db4de2783efac7c","observation_id":"281d4cc7-bb12-41b4-9d3e-d87635f7a676","resolution":{"observed_at":"2026-08-16T12:40:47.983415Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.987998Z","title":"F., Batalha , N","venue":null,"work_id":null,"year":2024},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":54,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.987998Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:04d968f65b7736f7f3dcf6ca3e3747c52774b9a88aa6c987f43001e898fda83b","observation_id":"dc6ee278-93f7-4e3d-bf62-6d97009245c8","resolution":{"observed_at":"2026-08-16T12:40:47.987998Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.991454Z","title":"2017, , 44, 665, 10.1002/2016GL071766","venue":null,"work_id":null,"year":2017},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":55,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.991454Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:415e48d3b1bdc408e4087a31d3aef809444d37e207138ca2509e2e58f2eb3e8e","observation_id":"6e5db5d8-47fb-4090-9f45-f62c5f65cbb2","resolution":{"observed_at":"2026-08-16T12:40:47.991454Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.994913Z","title":"H., Hurowitz , J., et al","venue":null,"work_id":null,"year":2021},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":56,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.994913Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:e7f77abaa8e199a0620336737238430f63e66ad0c3a69e390e0fe325f8992269","observation_id":"07c143e1-d771-4d4d-8818-ca65b7464354","resolution":{"observed_at":"2026-08-16T12:40:47.994913Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:47.998493Z","title":null,"venue":null,"work_id":null,"year":2016},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":57,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:47.998493Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:f5ae022ea88e13abb8dd62cb1dc55d5b5e90ddc05281dc04c4f7e69284a34ed1","observation_id":"7a3744a5-0681-451a-882e-e1bf22ddf642","resolution":{"observed_at":"2026-08-16T12:40:47.998493Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}},{"citation":{"cited_paper":null,"cited_work":{"arxiv_id":null,"doi":null,"metadata_source":null,"pith_arxiv_id":null,"snapshot_observed_at":"2026-08-16T12:40:48.002003Z","title":"I., Fortney , J","venue":null,"work_id":null,"year":2021},"citing_paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate","version":2},"reference_index":58,"source":"arxiv_source","source_observed_at":"2026-08-16T12:40:48.002003Z"},"links":{"citing_paper":"/paper/2504.12030"},"observation_digest":"sha256:1486bf5292dc9a26b9f4a6ea9571cc06e36b9c165c4e3ef1f0180c911c9a7efc","observation_id":"4bb9e89e-93c0-4ca9-b1c2-b688d7558bc1","resolution":{"observed_at":"2026-08-16T12:40:48.002003Z","resolver_source":null,"status":"unresolved"},"standing_notice":{"events":[],"reason":"canonical_work_link_unavailable","source_receipts":[],"state":"unavailable"}}],"paper":{"arxiv_id":"2504.12030","last_updated":"2025-09-04T14:00:41Z","latest_version":2,"primary_category":"astro-ph.EP","snapshot_observed_at":"2026-08-17T11:50:15.811216Z","submitted_at":"2025-04-16T12:39:54Z","title":"Planetary albedo is limited by the above-cloud atmosphere: Implications for sub-Neptune climate"},"reference_resolution":{"displayed":58,"state_counts":{"malformed_identifier":0,"metadata_mismatch":1,"parse_uncertain":0,"unresolved":52,"verified_exact":5,"verified_fuzzy":0},"total_outbound_references":58},"refusal":"A citation records a reference. It does not transfer a finding from one paper to another.","schema":"pith.paper-citation-record.v1","standing_sources":[{"observed_at":"2026-08-17T06:30:58.91139+00:00","source":"crossref"},{"observed_at":"2026-08-17T06:30:54.323127+00:00","source":"retraction_watch"}],"thesis":"As of 17 August 2026, this Paper Citation Record lists 58 of 58 outbound references and 2 inbound Pith citation observations for arXiv:2504.12030."}