{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,9,15]],"date-time":"2026-09-15T13:38:16Z","timestamp":1789479496297,"version":"build-2803163510"},"reference-count":10,"publisher":"American Association for the Advancement of Science (AAAS)","issue":"6241","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Science"],"published-print":{"date-parts":[[2015,6,19]]},"abstract":"<jats:p>\n            Ye\n            <jats:italic>et al<\/jats:italic>\n            . have determined a maximum nitrous acid (HONO) yield of 3% for the reaction HO\n            <jats:sub>2<\/jats:sub>\n            \u00b7H\n            <jats:sub>2<\/jats:sub>\n            O + NO\n            <jats:sub>2<\/jats:sub>\n            , which is much lower than the yield used in our work. This finding, however, does not affect our main result that HONO in the investigated Po Valley region is mainly from a gas-phase source that consumes nitrogen oxides.\n          <\/jats:p>","DOI":"10.1126\/science.aaa3777","type":"journal-article","created":{"date-parts":[[2015,6,18]],"date-time":"2015-06-18T18:10:13Z","timestamp":1434651013000},"page":"1326-1326","source":"Crossref","is-referenced-by-count":11,"title":["Response to Comment on \u201cMissing gas-phase source of HONO inferred from Zeppelin measurements in the troposphere\u201d"],"prefix":"10.1126","volume":"348","author":[{"given":"Xin","family":"Li","sequence":"first","affiliation":[{"name":"Institut f\u00fcr Energie und Klimaforschung, Troposph\u00e4re (IEK-8), Forschungszentrum J\u00fclich, J\u00fclich, Germany."}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Franz","family":"Rohrer","sequence":"additional","affiliation":[{"name":"Institut f\u00fcr Energie und Klimaforschung, Troposph\u00e4re (IEK-8), 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