{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,6,22]],"date-time":"2026-06-22T10:59:32Z","timestamp":1782125972612,"version":"3.54.5"},"reference-count":105,"publisher":"Wiley","issue":"1","license":[{"start":{"date-parts":[[2024,12,19]],"date-time":"2024-12-19T00:00:00Z","timestamp":1734566400000},"content-version":"vor","delay-in-days":0,"URL":"http:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100004493","name":"International Atomic Energy Agency","doi-asserted-by":"publisher","award":["1941"],"award-info":[{"award-number":["1941"]}],"id":[{"id":"10.13039\/501100004493","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":["nyaspubs.onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["Annals of the New York Academy of Sciences"],"published-print":{"date-parts":[[2025,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n                  <jats:p>\n                    Tropical cyclones (TCs) are one of the major natural hazards to island and coastal communities and ecosystems. However, isotopic compositions of TC\u2010derived precipitation (P) in surface water (SW) and groundwater (GW) reservoirs are still lacking. We tested the three main assumptions of the isotope storm \u201cspike\u201d hypothesis (sudden spikes in isotopic ratios). Our database covers 40 TCs and is divided into recent (\n                    <jats:italic>N<\/jats:italic>\n                    = 778; 2012\u20132023) and archived (\n                    <jats:italic>N<\/jats:italic>\n                    = 236; 1984\u20131995) rainfall isotope observations and SW\/GW isotope monitoring (\n                    <jats:italic>N<\/jats:italic>\n                    = 6013; 2014\u20132023). Seasonal rainfall contribution from TCs ranged from less than 1% to over 54% (4% on average) between 1984 and 2023. Mean \u03b4\n                    <jats:sup>18<\/jats:sup>\n                    O compositions across TCs domains were significantly lower than the regional (noncyclonic) \u03b4\n                    <jats:sup>18<\/jats:sup>\n                    O mean (\u22125.24 \u00b1 4.27\u2030): maritime (\u22126.29 \u00b1 3.28\u2030), coastal (\u22127.78 \u00b1 4.28\u2030), and inland (\u22129.80 \u00b1 5.18\u2030) values. Coastal and maritime TC convection resulted in large rainfall amounts with high isotope compositions. This could bias past climate reconstructions toward unrealistic drier conditions. Significant \u03b4\n                    <jats:sup>18<\/jats:sup>\n                    O and\n                    <jats:italic>d<\/jats:italic>\n                    \u2010excess differences were found between storm intensities. P\/SW and P\/GW isotope ratios revealed the rapid propagation of TC excursions in freshwater systems. Our findings highlight the potential of TC isotope observations for diagnosing intensity and frequency in paleoproxies beyond idealized TC models.\n                  <\/jats:p>","DOI":"10.1111\/nyas.15274","type":"journal-article","created":{"date-parts":[[2024,12,19]],"date-time":"2024-12-19T15:44:40Z","timestamp":1734623080000},"page":"145-165","update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":7,"title":["Stable isotope tempestology of tropical cyclones across the North Atlantic and Eastern Pacific Ocean basins"],"prefix":"10.1111","volume":"1543","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-8721-8093","authenticated-orcid":false,"given":"Ricardo","family":"S\u00e1nchez\u2010Murillo","sequence":"first","affiliation":[{"name":"Department of Earth and Environmental Sciences University of Texas at Arlington  Arlington Texas USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Dimitris 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