{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,8,14]],"date-time":"2026-08-14T15:15:26Z","timestamp":1786720526477,"version":"build-2736575974"},"reference-count":32,"publisher":"Cambridge University Press (CUP)","license":[{"start":{"date-parts":[[2024,1,15]],"date-time":"2024-01-15T00:00:00Z","timestamp":1705276800000},"content-version":"unspecified","delay-in-days":14,"URL":"http:\/\/creativecommons.org\/licenses\/by\/4.0"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Camb. prisms Coast. futures"],"published-print":{"date-parts":[[2024]]},"abstract":"<jats:title>Abstract<\/jats:title>\n                  <jats:p>Major technological advances have made measurements of coastal subsidence more sophisticated, but these advances have not always been matched by a thorough examination of what is actually being measured. Here we draw attention to the widespread confusion about key concepts in the coastal subsidence literature, much of which revolves around the interplay between sediment accretion, vertical land motion and surface-elevation change. We attempt to reconcile this by drawing on well-established concepts from the tectonics community. A consensus on these issues by means of a common language can help bridge the gap between disparate disciplines (ranging from geophysics to ecology) that are critical in the quest for meaningful projections of future relative sea-level rise.<\/jats:p>","DOI":"10.1017\/cft.2024.1","type":"journal-article","created":{"date-parts":[[2024,1,14]],"date-time":"2024-01-14T21:11:25Z","timestamp":1705266685000},"source":"Crossref","is-referenced-by-count":17,"title":["What is coastal subsidence?"],"prefix":"10.1017","volume":"2","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-1563-1716","authenticated-orcid":false,"given":"Torbj\u00f6rn E.","family":"T\u00f6rnqvist","sequence":"first","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Michael D.","family":"Blum","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"56","published-online":{"date-parts":[[2024,1,15]]},"reference":[{"key":"S2754720524000015_r27","doi-asserted-by":"crossref","first-page":"40","DOI":"10.1038\/s43017-020-00115-x","article-title":"Measuring, modelling and projecting coastal land subsidence","volume":"2","author":"Shirzaei","year":"2021","journal-title":"Nature Reviews Earth and Environment"},{"key":"S2754720524000015_r22","first-page":"58","article-title":"A new subsidence map for coastal Louisiana","volume":"27","author":"Nienhuis","year":"2017","journal-title":"GSA Today"},{"key":"S2754720524000015_r6","doi-asserted-by":"crossref","first-page":"56","DOI":"10.1016\/j.rse.2017.11.016","article-title":"Understanding land subsidence in salt marshes of the Venice Lagoon from SAR interferometry and ground-based investigations","volume":"205","author":"Da Lio","year":"2018","journal-title":"Remote Sensing of Environment"},{"key":"S2754720524000015_r2","doi-asserted-by":"crossref","first-page":"1867","DOI":"10.1073\/pnas.1912921117","article-title":"Water level changes, subsidence, and sea level rise in the Ganges-Brahmaputra-Meghna delta","volume":"117","author":"Becker","year":"2020","journal-title":"Proceedings of the National Academy of Sciences of the United States of America"},{"key":"S2754720524000015_r24","first-page":"321","volume-title":"IPCC Special Report on the Ocean and Cryosphere in a Changing Climate","author":"Oppenheimer","year":"2019"},{"key":"S2754720524000015_r9","doi-asserted-by":"crossref","first-page":"5578","DOI":"10.3390\/rs14215578","article-title":"An integrated InSAR and GNSS approach to monitor land subsidence in the Po River Delta (Italy)","volume":"14","author":"Fabris","year":"2022","journal-title":"Remote Sensing"},{"key":"S2754720524000015_r25","doi-asserted-by":"crossref","first-page":"121","DOI":"10.1046\/j.1365-3091.2000.00006.x","article-title":"Quantitative models of sedimentary basin filling","volume":"47","author":"Paola","year":"2000","journal-title":"Sedimentology"},{"key":"S2754720524000015_r8","doi-asserted-by":"crossref","first-page":"1173","DOI":"10.1130\/0091-7613(1990)018<1173:SUUORA>2.3.CO;2","article-title":"Surface uplift, uplift of rocks, and exhumation of rocks","volume":"18","author":"England","year":"1990","journal-title":"Geology"},{"key":"S2754720524000015_r4","doi-asserted-by":"crossref","first-page":"e2021JF006153","DOI":"10.1029\/2021JF006153","article-title":"Does load-induced shallow subsidence inhibit delta growth?","volume":"126","author":"Chamberlain","year":"2021","journal-title":"Journal of Geophysical Research: Earth Surface"},{"key":"S2754720524000015_r10","doi-asserted-by":"crossref","first-page":"481","DOI":"10.1146\/annurev-earth-082517-010255","article-title":"Marsh processes and their response to climate change and sea-level rise","volume":"47","author":"FitzGerald","year":"2019","journal-title":"Annual Review of Earth and Planetary Sciences"},{"key":"S2754720524000015_r13","doi-asserted-by":"crossref","first-page":"230","DOI":"10.1130\/L322.1","article-title":"Diagnosing climatic and tectonic controls on topography: Eastern flank of the Northern Bolivian Andes","volume":"6","author":"Gasparini","year":"2014","journal-title":"Lithosphere"},{"key":"S2754720524000015_r17","doi-asserted-by":"crossref","first-page":"14792","DOI":"10.1038\/ncomms14792","article-title":"Vulnerability of Louisiana\u2019s coastal wetlands to present-day rates of relative sea-level rise","volume":"8","author":"Jankowski","year":"2017","journal-title":"Nature Communications"},{"key":"S2754720524000015_r19","doi-asserted-by":"crossref","first-page":"3867","DOI":"10.1002\/2015JB012636","article-title":"Anthropogenic and geologic influences on subsidence in the vicinity of New Orleans, Louisiana","volume":"121","author":"Jones","year":"2016","journal-title":"Journal of Geophysical Research: Solid Earth"},{"key":"S2754720524000015_r11","first-page":"1211","volume-title":"Climate Change 2021. 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