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As a result, there is a spatial gradient of decreasing marsh area and increasing shallow open water area in upstream direction along the Blackwater River. At five field sites along this marsh loss gradient, 15-minute water level measurements were recorded with pressure transducers (Hobo U20L-02, Onset, MA, USA). The measurements were recalculated to the NAVD88 vertical datum after local atmospheric pressure compensation.","EngDescr":null,"OrigAbstract":null,"OrigDescr":null,"Comments":null,"ReleaseDate":null,"ReleaseDate0":null,"OrigDescrLang":null,"EmbargoDate":null,"OrigDescrLangNL":null,"OrigLangCode":null,"OrigLangCodeExtended":null,"OrigLangID":null,"DescrCompFlag":0,"DescrTransFlag":0,"Citation":"Schepers, L.; Brennand, P.; Kirwan, M.L.; Guntenspergen, G.R.; Temmerman, S.; (2020): Water level measurements along a historical marsh loss gradient in the Blackwater Estuary, MD, USA in 2014. 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Recommended for maximum dissemination and use of licensed materials.","Lineage":null,"AccConID":21},"dois":[{"DOIID":407,"PublicationYear":2020,"DOI":"10.14284/407","Citation":"Schepers, L.; Brennand, P.; Kirwan, M.L.; Guntenspergen, G.R.; Temmerman, S.; (2020): Water level measurements along a historical marsh loss gradient in the Blackwater Estuary, MD, USA in 2014. 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