{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,9]],"date-time":"2026-04-09T09:45:27Z","timestamp":1775727927712,"version":"3.50.1"},"reference-count":65,"publisher":"MDPI AG","issue":"5","license":[{"start":{"date-parts":[[2022,3,1]],"date-time":"2022-03-01T00:00:00Z","timestamp":1646092800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001809","name":"the National Natural Science Foundation of China","doi-asserted-by":"publisher","award":["42071309"],"award-info":[{"award-number":["42071309"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"publisher"}]},{"name":"the National Key R &amp; D project of China","award":["2021YFA0715104"],"award-info":[{"award-number":["2021YFA0715104"]}]},{"name":"the Strategic Priority Research Program of Chinese Academy of Sciences","award":["XDB 41000000"],"award-info":[{"award-number":["XDB 41000000"]}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>Monitoring the surface deformation is of great significance, in order to explore the activity and geophysical features of the underground deep pressure source in the volcanic regions. In this study, the time series surface deformation of the Changbaishan volcano is retrieved via Sentinel-1B SAR data, using the SBAS-InSAR method. The main results are as follows. (1) The mean surface deformation velocity in the Changbaishan volcano is uplifted as a whole, while the uplift is locally distributed, which shows a strong correlation with faults. (2) The time series surface deformation of the Changbaishan volcano indicates an apparently seasonal change. (3) The cumulative surface deformation shows a strong correlation with the maximal magnitude and number of annual earthquakes, and it is likely dominated by the maximal magnitude of the annual earthquakes. (4) The single Mogi source model is appropriate to evaluate the deep pressure source in the Changbaishan volcano, constrained by the calculated surface deformation. The optimal estimated depth of the magma chamber is about 6.2 km, and the volume is increased by about 3.2 \u00d7 106 m3. According to the time series surface deformation, it is concluded that the tectonic activity and faults, related to the deep pressure source, are pretty active in the Changbaishan volcano.<\/jats:p>","DOI":"10.3390\/rs14051213","type":"journal-article","created":{"date-parts":[[2022,3,1]],"date-time":"2022-03-01T21:25:14Z","timestamp":1646169914000},"page":"1213","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":14,"title":["Time Series Surface Deformation of Changbaishan Volcano Based on Sentinel-1B SAR Data and Its Geological Significance"],"prefix":"10.3390","volume":"14","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-4598-087X","authenticated-orcid":false,"given":"Zhiguo","family":"Meng","sequence":"first","affiliation":[{"name":"College of Geoexploration Science and Technology, Jilin University, Changchun 130026, China"},{"name":"The State Key Laboratory of Lunar and Planetary Sciences, Macau University of Science and Technology, Macau 999078, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-7109-7952","authenticated-orcid":false,"given":"Chuanzeng","family":"Shu","sequence":"additional","affiliation":[{"name":"College of Geoexploration Science and Technology, Jilin University, Changchun 130026, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-8938-671X","authenticated-orcid":false,"given":"Ying","family":"Yang","sequence":"additional","affiliation":[{"name":"Tianjin Research Institute for Water Transport Engineering M.O.T., Tianjin 300456, China"}]},{"given":"Chengzhi","family":"Wu","sequence":"additional","affiliation":[{"name":"Changbaishan Tianchi Volcano Observatory, Antu 133618, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0802-5929","authenticated-orcid":false,"given":"Xuegang","family":"Dong","sequence":"additional","affiliation":[{"name":"College of Geoexploration Science and Technology, Jilin University, Changchun 130026, China"}]},{"given":"Dongzhen","family":"Wang","sequence":"additional","affiliation":[{"name":"Key Laboratory of Earthquake Geodesy, Institute of Seismology, China Earthquake Administration, Wuhan 430071, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9244-8464","authenticated-orcid":false,"given":"Yuanzhi","family":"Zhang","sequence":"additional","affiliation":[{"name":"Laboratory of Deep-Space Exploration, National Astronomical Observatories, Chinese Academy of Sciences, Beijing 100101, China"},{"name":"School of Space Science and Astronomy, University of Chinese Academy of Sciences, Beijing 100049, China"}]}],"member":"1968","published-online":{"date-parts":[[2022,3,1]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"e1600913","DOI":"10.1126\/sciadv.1600913","article-title":"Quantifying gas emissions from the \u201cMillennium Eruption\u201d of Paektu volcano, Democratic People\u2019s Republic of Korea\/China","volume":"2","author":"Iacovino","year":"2016","journal-title":"Sci. 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