{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,7]],"date-time":"2026-03-07T12:31:51Z","timestamp":1772886711472,"version":"3.50.1"},"reference-count":47,"publisher":"American Geophysical Union (AGU)","issue":"6","license":[{"start":{"date-parts":[[2021,6,3]],"date-time":"2021-06-03T00:00:00Z","timestamp":1622678400000},"content-version":"vor","delay-in-days":2,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":["agupubs.onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["JGR Solid Earth"],"published-print":{"date-parts":[[2021,6]]},"abstract":"<jats:title>Abstract<\/jats:title>\n                  <jats:p>\n                    GPS observations of ocean tide loading displacements can help infer the regional anelastic properties of the asthenosphere. We estimate M\n                    <jats:sub>2<\/jats:sub>\n                    ocean tide loading displacements at 170 GPS sites in New Zealand and compare these to modeled values using a range of numerical tide and radially symmetric (1D) elastic and anelastic Earth models. Regardless of the model combination, we are unable to reduce the strong spatial coherence of the M\n                    <jats:sub>2<\/jats:sub>\n                    residuals across the North Island where they reach 0.4\u00a0mm (2%). The best fit in the North Island is obtained when combining the FES2014b tide model with spatially variable ocean density and water compressibility, and the STW105 Earth model. The residuals exhibit a change of \u223c0.3\u00a0mm in magnitude between the Taupo Volcanic Zone and the east coast (\u223c100\u00a0km), suggesting that this region's laterally varying, shallow rheological structure may need to be considered to explain these observations.\n                  <\/jats:p>","DOI":"10.1029\/2021jb021992","type":"journal-article","created":{"date-parts":[[2021,5,26]],"date-time":"2021-05-26T07:31:00Z","timestamp":1622014260000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":8,"title":["Limitations in One\u2010Dimensional (an)Elastic Earth Models for Explaining GPS\u2010Observed M\n                    <sub>2<\/sub>\n                    Ocean Tide Loading Displacements in New Zealand"],"prefix":"10.1029","volume":"126","author":[{"ORCID":"https:\/\/orcid.org\/0000-0001-9695-3823","authenticated-orcid":false,"given":"Bogdan","family":"Matviichuk","sequence":"first","affiliation":[{"name":"School of Geography, Planning, and Spatial Sciences University of Tasmania  Hobart Australia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5611-9498","authenticated-orcid":false,"given":"Matt A.","family":"King","sequence":"additional","affiliation":[{"name":"School of Geography, Planning, and Spatial Sciences University of Tasmania  Hobart Australia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-7464-4592","authenticated-orcid":false,"given":"Christopher S.","family":"Watson","sequence":"additional","affiliation":[{"name":"School of Geography, Planning, and Spatial Sciences University of Tasmania  Hobart Australia"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-1946-8637","authenticated-orcid":false,"given":"Machiel S.","family":"Bos","sequence":"additional","affiliation":[{"name":"Instituto Dom Luiz University of Beira Interior  Covilh\u00e3 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