{"record_type":"pith_number_record","schema_url":"https://pith.science/schemas/pith-number/v1.json","pith_number":"pith:2016:IOFWWL5EDPOEFYPITJITLCCKT6","short_pith_number":"pith:IOFWWL5E","schema_version":"1.0","canonical_sha256":"438b6b2fa41bdc42e1e89a5135884a9f802410c1d0e8d41c7274894459bb2edf","source":{"kind":"arxiv","id":"1603.01317","version":1},"attestation_state":"computed","paper":{"title":"The 2010 and 2014 floods in India and Pakistan: dynamical influences on vertical motion and precipitation","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":[],"primary_cat":"physics.ao-ph","authors_text":"Adam H. Sobel, Daniel A. Shaevitz, Ji Nie","submitted_at":"2016-03-04T00:08:44Z","abstract_excerpt":"Devastating floods in northeast Pakistan and northern India occurred in July 2010 and September 2014 as a consequence of extreme precipitation events. The 2010 and 2014 flood events had similar synoptic flow patterns that led to an anomalously high moisture content in the flood region. The quasi-geostrophic omega equation is inverted in order to attribute components of the large-scale vertical motion profile to synoptic forcing, diabatic heating, and mechanically forced orographic ascent. The results show that diabatic heating is the dominant contributor to the large-scale vertical motion, and"},"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":"1603.01317","kind":"arxiv","version":1},"metadata":{"license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","primary_cat":"physics.ao-ph","submitted_at":"2016-03-04T00:08:44Z","cross_cats_sorted":[],"title_canon_sha256":"dc92599081246c6c6ce21db972d8c9862c9a7a4e43c7ddef27598bffd174f125","abstract_canon_sha256":"d776ee25c796a798a3efd370596594875aff29eb100b201a697cd1107a0a5bfe"},"schema_version":"1.0"},"receipt":{"kind":"pith_receipt","key_id":"pith-v1-2026-05","algorithm":"ed25519","signed_at":"2026-05-18T01:19:37.934371Z","signature_b64":"Kf1YZeCwsY5x3gTWtvKIylDw7feZMxA4Od0anVdPaLvwl7vIQykTVjWFNMDL/cRlUcLU6UpvdDq9x7usiwubCw==","signed_message":"canonical_sha256_bytes","builder_version":"pith-number-builder-2026-05-17-v1","receipt_version":"0.3","canonical_sha256":"438b6b2fa41bdc42e1e89a5135884a9f802410c1d0e8d41c7274894459bb2edf","last_reissued_at":"2026-05-18T01:19:37.933756Z","signature_status":"signed_v1","first_computed_at":"2026-05-18T01:19:37.933756Z","public_key_fingerprint":"8d4b5ee74e4693bcd1df2446408b0d54"},"graph_snapshot":{"paper":{"title":"The 2010 and 2014 floods in India and Pakistan: dynamical influences on vertical motion and precipitation","license":"http://arxiv.org/licenses/nonexclusive-distrib/1.0/","headline":"","cross_cats":[],"primary_cat":"physics.ao-ph","authors_text":"Adam H. Sobel, Daniel A. Shaevitz, Ji Nie","submitted_at":"2016-03-04T00:08:44Z","abstract_excerpt":"Devastating floods in northeast Pakistan and northern India occurred in July 2010 and September 2014 as a consequence of extreme precipitation events. The 2010 and 2014 flood events had similar synoptic flow patterns that led to an anomalously high moisture content in the flood region. The quasi-geostrophic omega equation is inverted in order to attribute components of the large-scale vertical motion profile to synoptic forcing, diabatic heating, and mechanically forced orographic ascent. The results show that diabatic heating is the dominant contributor to the large-scale vertical motion, and"},"claims":{"count":0,"items":[],"snapshot_sha256":"258153158e38e3291e3d48162225fcdb2d5a3ed65a07baac614ab91432fd4f57"},"source":{"id":"1603.01317","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":""},"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":"1603.01317","created_at":"2026-05-18T01:19:37.933852+00:00"},{"alias_kind":"arxiv_version","alias_value":"1603.01317v1","created_at":"2026-05-18T01:19:37.933852+00:00"},{"alias_kind":"doi","alias_value":"10.48550/arxiv.1603.01317","created_at":"2026-05-18T01:19:37.933852+00:00"},{"alias_kind":"pith_short_12","alias_value":"IOFWWL5EDPOE","created_at":"2026-05-18T12:30:22.444734+00:00"},{"alias_kind":"pith_short_16","alias_value":"IOFWWL5EDPOEFYPI","created_at":"2026-05-18T12:30:22.444734+00:00"},{"alias_kind":"pith_short_8","alias_value":"IOFWWL5E","created_at":"2026-05-18T12:30:22.444734+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/IOFWWL5EDPOEFYPITJITLCCKT6","json":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6.json","graph_json":"https://pith.science/api/pith-number/IOFWWL5EDPOEFYPITJITLCCKT6/graph.json","events_json":"https://pith.science/api/pith-number/IOFWWL5EDPOEFYPITJITLCCKT6/events.json","paper":"https://pith.science/paper/IOFWWL5E"},"agent_actions":{"view_html":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6","download_json":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6.json","view_paper":"https://pith.science/paper/IOFWWL5E","resolve_alias":"https://pith.science/api/pith-number/resolve?arxiv=1603.01317&json=true","fetch_graph":"https://pith.science/api/pith-number/IOFWWL5EDPOEFYPITJITLCCKT6/graph.json","fetch_events":"https://pith.science/api/pith-number/IOFWWL5EDPOEFYPITJITLCCKT6/events.json","actions":{"anchor_timestamp":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6/action/timestamp_anchor","attest_storage":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6/action/storage_attestation","attest_author":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6/action/author_attestation","sign_citation":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6/action/citation_signature","submit_replication":"https://pith.science/pith/IOFWWL5EDPOEFYPITJITLCCKT6/action/replication_record"}},"created_at":"2026-05-18T01:19:37.933852+00:00","updated_at":"2026-05-18T01:19:37.933852+00:00"}