{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,11,3]],"date-time":"2025-11-03T03:59:41Z","timestamp":1762142381246,"version":"build-2065373602"},"reference-count":14,"publisher":"MDPI AG","issue":"3","license":[{"start":{"date-parts":[[2019,8,8]],"date-time":"2019-08-08T00:00:00Z","timestamp":1565222400000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Data"],"abstract":"<jats:p>Satellite-derived data, including an estimation of the eruption rate, proximal volcanic deposits and lava flow morphometric parameters (area, maximum length, thickness, and volume) are provided for the eruption that occurred at Mt Etna on 6\u20138 December 2015. This eruption took place at the New Southeast Crater (NSEC), the youngest of the summit craters of Etna, shortly after a sequence of four violent paroxysmal events took place in 65 h (3\u20135 December) at \u201cVoragine\u201d, the oldest summit crater. Multispectral SEVIRI images at 15 min sampling time have been used to compute time-averaged eruption rate curves, while tri-stereo Pl\u00e9iades images, at 50 cm spatial resolution, provided the pre-eruptive topography and topographic changes due to volcanic deposits. In addition to the two types of satellite data, other parameters have been inferred, such as probable vesicularity and pyroclastic deposits.<\/jats:p>","DOI":"10.3390\/data4030120","type":"journal-article","created":{"date-parts":[[2019,8,8]],"date-time":"2019-08-08T11:05:32Z","timestamp":1565262332000},"page":"120","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":16,"title":["Satellite-Based Reconstruction of the Volcanic Deposits during the December 2015 Etna Eruption"],"prefix":"10.3390","volume":"4","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-9914-1107","authenticated-orcid":false,"given":"Gaetana","family":"Ganci","sequence":"first","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Osservatorio Etneo, 95125 Catania, Italy"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-9947-8789","authenticated-orcid":false,"given":"Annalisa","family":"Cappello","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Osservatorio Etneo, 95125 Catania, Italy"}]},{"given":"Giuseppe","family":"Bilotta","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Osservatorio Etneo, 95125 Catania, Italy"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-3054-6840","authenticated-orcid":false,"given":"Claudia","family":"Corradino","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Osservatorio Etneo, 95125 Catania, Italy"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5734-9025","authenticated-orcid":false,"given":"Ciro","family":"Del Negro","sequence":"additional","affiliation":[{"name":"Istituto Nazionale di Geofisica e Vulcanologia, Sezione di Catania, Osservatorio Etneo, 95125 Catania, Italy"}]}],"member":"1968","published-online":{"date-parts":[[2019,8,8]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"217","DOI":"10.1016\/j.jvolgeores.2012.05.011","article-title":"Volcanology 2020: How will thermal remote sensing of volcanic surface activity evolve over the next decade?","volume":"249","author":"Ramsey","year":"2012","journal-title":"J. Volcanol. Geotherm. Res."},{"key":"ref_2","doi-asserted-by":"crossref","first-page":"52","DOI":"10.1007\/s004450050216","article-title":"Calculation of lava effusion rates from Landsat TM data","volume":"60","author":"Harris","year":"1998","journal-title":"Bull. Volcanol."},{"key":"ref_3","doi-asserted-by":"crossref","first-page":"223","DOI":"10.1016\/S0012-821X(01)00443-5","article-title":"A simple explanation for the space-based calculation of lava eruption rates","volume":"192","author":"Wright","year":"2001","journal-title":"Earth Planet. Sci. Lett."},{"key":"ref_4","doi-asserted-by":"crossref","first-page":"83","DOI":"10.3389\/feart.2018.00083","article-title":"Mapping Volcanic Deposits of the 2011\u20132015 Etna Eruptive Events Using Satellite Remote Sensing","volume":"6","author":"Ganci","year":"2018","journal-title":"Front. Earth Sci."},{"key":"ref_5","doi-asserted-by":"crossref","first-page":"553","DOI":"10.5194\/isprsarchives-XXXIX-B3-553-2012","article-title":"3D capabilities of Pleiades satellite","volume":"39","author":"Bernard","year":"2012","journal-title":"Int. Arch. Photogramm. Remote Sens. Spat. Inf. Sci."},{"key":"ref_6","doi-asserted-by":"crossref","first-page":"6267","DOI":"10.1002\/2016GL069457","article-title":"High-resolution digital elevation model from tri-stereo Pleiades-1 satellite imagery for lava flow volume estimates at Fogo Volcano","volume":"43","author":"Bagnardi","year":"2016","journal-title":"Geophys. Res. Lett."},{"key":"ref_7","doi-asserted-by":"crossref","unstructured":"Ganci, G., Vicari, A., Fortuna, L., and Del Negro, C. (2011). The HOTSAT volcano monitoring system based on a combined use of SEVIRI and MODIS multispectral data. Ann. 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Stand., 14.","DOI":"10.1186\/s40965-017-0027-2"},{"key":"ref_11","unstructured":"Ganci, G., Cappello, A., Bilotta, G., H\u00e9rault, A., Zago, V., and Del Negro, C. (2019). 3D Lava flow mapping at Etna volcano from Pl\u00e9iades-derived DEM differences. PANGAEA."},{"key":"ref_12","doi-asserted-by":"crossref","first-page":"271","DOI":"10.5194\/tc-5-271-2011","article-title":"Co-registration and bias corrections of satellite elevation data sets for quantifying glacier thickness change","volume":"5","author":"Nuth","year":"2011","journal-title":"Cryosphere"},{"key":"ref_13","first-page":"1","article-title":"Quantifying Lava Flow Hazards in Response to Effusive Eruption","volume":"128","author":"Cappello","year":"2016","journal-title":"Bull. Geol. Soc. Am."},{"key":"ref_14","doi-asserted-by":"crossref","unstructured":"Ganci, G., Cappello, A., Zago, V., Bilotta, G., H\u00e9rault, A., and Del Negro, C. (2018). 3D Lava flow mapping of the 17\u201325 May 2016 Etna eruption using tri-stereo optical satellite data. Ann. Geophys., 61.","DOI":"10.4401\/ag-7875"}],"container-title":["Data"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/www.mdpi.com\/2306-5729\/4\/3\/120\/pdf","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2025,10,11]],"date-time":"2025-10-11T13:09:43Z","timestamp":1760188183000},"score":1,"resource":{"primary":{"URL":"https:\/\/www.mdpi.com\/2306-5729\/4\/3\/120"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2019,8,8]]},"references-count":14,"journal-issue":{"issue":"3","published-online":{"date-parts":[[2019,9]]}},"alternative-id":["data4030120"],"URL":"https:\/\/doi.org\/10.3390\/data4030120","relation":{},"ISSN":["2306-5729"],"issn-type":[{"type":"electronic","value":"2306-5729"}],"subject":[],"published":{"date-parts":[[2019,8,8]]}}}