The Estimation of Lava Flow Temperatures Using Landsat Night-Time Images: Case Studies from Eruptions of Mt. Etna and Stromboli (Sicily, Italy), Kīlauea (Hawaii Island), and Eyjafjallajökull and Holuhraun (Iceland)

• Published in: Remote Sensing
• Main Authors: Ádám Nádudvari, Anna Abramowicz, Rosanna Maniscalco, Marco Viccaro
• Format: Article in Journal/Newspaper
• Language: English
• Published: MDPI AG 2020
• Subjects: lava flows; spectral radiance; Landsat series; brightness temperatures; Science; Q; Etna; Holuhraun; Eyjafjallajökull; Iceland
• Online Access: https://doi.org/10.3390/rs12162537; https://doaj.org/article/8d8c040cb3f94833aa5430a3415140b0

Using satellite-based remote sensing to investigate volcanic eruptions is a common approach for preliminary research, chiefly because a great amount of freely available data can be effectively accessed. Here, Landsat 4-5TM, 7ETM+, and 8OLI night-time satellite images are used to estimate lava flow temperatures and radiation heat fluxes from selected volcanic eruptions worldwide. After retrieving the spectral radiance, the pixel values were transformed into temperatures using the calculated calibration constants. Results showed that the TIR and SWIR bands were saturated and unable to detect temperatures over the active lava flows. However, temperatures were effectively detected over the active lava flows in the range ~500–1060 °C applying the NIR-, red-, green- or blue-band. Application of the panchromatic band with 15 m resolution also revealed details of lava flow morphology. The calculated radiant heat flux for the lava flows accords with increasing cooling either with slope or with distance from the vent.