{"id":97815,"date":"2026-07-08T14:55:42","date_gmt":"2026-07-08T12:55:42","guid":{"rendered":""},"modified":"2026-07-12T16:02:31","modified_gmt":"2026-07-12T14:02:31","slug":"0198cc44e700-a3819238-5a35-4cd2-9df3-f158d5a82041","status":"publish","type":"nva_publication","link":"https:\/\/nilu.gnist.dev\/en\/publications\/0198cc44e700-a3819238-5a35-4cd2-9df3-f158d5a82041\/","title":{"rendered":"Influence of spring-time Eurasian-Himalayan snow on the evolution of the Indian summer monsoon"},"content":{"rendered":"","protected":false},"template":"","meta":{"_acf_changed":false,"_searchwp_excluded":"","_id":"","_status":"PUBLISHED","_sync_date":"2026-07-08 14:55:42","footnotes":""},"nva_tax_category":[985],"class_list":["post-97815","nva_publication","type-nva_publication","status-publish","hentry","nva_tax_category-poster"],"acf":[],"_links":{"self":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/97815","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication"}],"about":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/types\/nva_publication"}],"version-history":[{"count":1,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/97815\/revisions"}],"predecessor-version":[{"id":97816,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_publication\/97815\/revisions\/97816"}],"wp:attachment":[{"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/media?parent=97815"}],"wp:term":[{"taxonomy":"nva_tax_category","embeddable":true,"href":"https:\/\/nilu.gnist.dev\/en\/wp-json\/wp\/v2\/nva_tax_category?post=97815"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}