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Editorial

Editorial for Special Issue “Convective and Volcanic Clouds (CVC)”

by
Riccardo Biondi
1,* and
Stefano Corradini
2
1
Dipartimento di Geoscienze, Università degli Studi di Padova, 35131 Padova, Italy
2
Istituto Nazionale di Geofisica e Vulcanologia (INGV), ONT, 00143 Rome, Italy
*
Author to whom correspondence should be addressed.
Remote Sens. 2020, 12(13), 2080; https://doi.org/10.3390/rs12132080
Submission received: 19 June 2020 / Accepted: 23 June 2020 / Published: 29 June 2020
(This article belongs to the Special Issue Convective and Volcanic Clouds (CVC))

Abstract

:
In recent years, some volcanic eruptions have focused scientists’ attention on the detection and monitoring of volcanic clouds, as their impact on the air traffic control system has been unprecedented. In 2010, the Eyjafjallajökull eruption forced the disruption of the airspace of several countries, generating one of the largest air traffic shutdowns ever. Extreme convective events cause many deaths and injuries, and much damage to property every year, accounting for major economic damages related to natural disasters in several countries. Due to global warming, Atlantic tropical cyclones have increased their maximum intensity, hurricanes have more often become extratropical cyclones affecting northern Europe, and southeastern Europe is characterized by increasing annual stormy days. Convective and Volcanic Clouds (CVC) are very dangerous for aviation operations, as they can affect aircraft safety and economic, political, and cultural activities. The detection, nowcasting, and monitoring of CVC is therefore vital for organizing efficient early warning systems.

The aim of this Special Issue is to collect innovative techniques to detect and nowcast CVC and to create a solid background to be used by modelers and forecasters. The Special Issue includes three papers [1,2,3] reporting new techniques to detect volcanic cloud top heights: two papers focusing on the Etna eruptions [3,4] and one paper [5] showing a new function to nowcast extreme weather events on the European area with the highest frequency of strong convection.
Cigala et al. [1] report an innovative technique to detect the volcanic cloud top height by using the Global Navigation Satellite System radio occultation signal. The radio occultation is able to sound the atmosphere with a high vertical resolution, and it is sensitive to the atmospheric density variation due to the presence of the cloud. This paper focuses on the 2008 Kasatochi eruption showing an error of about 1 km on the estimation of the cloud top height when compared to the Cloud-Aerosol Lidar with Orthogonal Polarization (CALIOP) measurements. This technique can be applied to all the volcanic clouds and looks very promising due to the global coverage and high vertical resolution. However, it always needs a background measurement because it is not able to distinguish different types of clouds.
In Zhu et al. [2], the combination of the CALIOP and the Spinning Enhanced Visible and Infrared Imager (SEVIRI) data is used to estimate the volcanic ash cloud top height by exploiting a hybrid deep learning methodology. The algorithm, applied to the 2010 Eyjafjallajökull (Iceland) and the 2011 Puyehue-Cordón Caulle (Chile) eruptions, is able to give reliable results in both simple and complex meteorological conditions. The volcanic ash cloud height accuracy can be further increased by the use of atmospheric temperature vertical profiles. The methodology described in this paper can be extended to all the measurements derived from the instruments on board the new generation of geostationary weather satellites.
Corradini et al. [3], perform the near real time proximal and distal monitoring of the 24–30 December, 2018 Etna eruption by using the data derived from the SEVIRI instrument on board the MSG geostationary satellite. As proximal products, the start time of the eruption, the time average discharge rate, the cumulative lava volume emitted, and the height of the volcanic column are obtained while, as distal parameters, the volcanic cloud top height, ash, and the SO2 are carried out. All the products have been validated using satellite and ground based data. The results show the ability of geostationary satellite systems to characterize eruptive events, thus offering a powerful tool to mitigate the volcanic risk on both the local population and the airspace and to give insight into volcanic processes.
Scollo et al. [4], propose a new system to monitor and forecast the tephra fallout based on quantitative volcanological observations and modelling. It combines data from low-cost calibrated visible cameras and satellite images to estimate the variation of column height with time, and to model volcanic plume and fallout in near-real time. The system provides a reliable hazard assessment to the National Department of Civil Protection during explosive eruptions, thus contributing to mitigating the effect of the volcanic eruption on the local population. It is extremely interesting because it can be easily adapted to other volcano observatories worldwide, while the low-cost makes it also available for developing countries.
Guerova et al. [5] is the only paper of this Special Issue focusing on convection. This work studies thunderstorms developing in Bulgaria which is the European region with the highest frequency of extreme weather events. This work has improved the forecast of thunderstorms by using an index based on the combination of instability indices and Integrated Water Vapor derived from the Global Navigation Satellite System. Despite the non-optimal setting of the network used for this study, the results are encouraging, showing a decrease in false alarms when compared to forecasts using the instability indices only. The function proposed in the paper has only a local validity and will be operationally used within the national thunderstorm nowcasting tool, however, a similar analysis can be used and applied anywhere based on the same type of measurements.
Given the large uncertainties that still remain in monitoring and detecting the CVC, the blow-up of the research community for developing new techniques and improving our knowledge is required. A vast amount of information produced by the available techniques is not transferred in a way that is usable by the end-users (e.g., airlines, pilots), and a close interaction between scientists and end-users is important to convert the new research products into operational tools. With this vision, this Special Issue collects papers showing innovative techniques with the potential to become operational, to support policy makers and final users, and to inspire new research on CVC topics. We are grateful to all the authors for contributing to the cutting-edge research reported on the manuscripts and to all the reviewers and the editorial team for making this project possible.

Author Contributions

The authors contributed equally to the writing of this editorial. All authors have read and agreed to the published version of the manuscript.

Funding

The work is accomplished in the frame of the VESUVIO (Volcanic clouds dEtection and monitoring for Studying the erUption impact on climate and aVIatiOn) project funded by the Supporting Talent in ReSearch (STARS) grant at Università degli Studi di Padova, and the VISTA (Volcanic monItoring using SenTinel sensors by an integrated Approach) project funded by the European Space Agency (ESA) grant number 4000128399/19/I-DT.

Conflicts of Interest

The authors declare no conflict of interest.

References

  1. Cigala, V.; Biondi, R.; Prata, A.J.; Steiner, A.K.; Kirchengast, G.; Brenot, H. GNSS radio OccultationAdvances the monitoring of volcanic clouds: The case of the 2008 Kasatochi Eruption. Remote Sens. 2019, 11, 2199. [Google Scholar] [CrossRef] [Green Version]
  2. Zhu, W.; Zhu, L.; Li, J.; Sun, H. Retrieving volcanic ash top height through combined polar orbit activeand geostationary passive remote sensing data. Remote Sens. 2020, 12, 953. [Google Scholar] [CrossRef] [Green Version]
  3. Corradini, S.; Guerrieri, L.; Stelitano, D.; Salerno, G.; Scollo, S.; Merucci, L.; Prestifilippo, M.; Musacchio, M.; Silvestri, M.; Lombardo, V.; et al. Near real-time monitoring of the Christmas 2018 Etna eruption using SEVIRI and products validation. Remote Sens. 2020, 12, 1336. [Google Scholar] [CrossRef] [Green Version]
  4. Scollo, S.; Prestifilippo, M.; Bonadonna, C.; Cioni, R.; Corradini, S.; Degruyter, W.; Rossi, E.; Silvestri, M.; Biale, E.; Carparelli, G.; et al. Near-real-time tephra fallout assessment at Mt. Etna, Italy. Remote Sens. 2019, 11, 2987. [Google Scholar] [CrossRef] [Green Version]
  5. Guerova, G.; Dimitrova, T.; Georgiev, S. Thunderstorm classification functions based on instability indicesand GNSS IWV for the Sofia Plain. Remote Sens. 2019, 11, 2988. [Google Scholar] [CrossRef] [Green Version]

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MDPI and ACS Style

Biondi, R.; Corradini, S. Editorial for Special Issue “Convective and Volcanic Clouds (CVC)”. Remote Sens. 2020, 12, 2080. https://doi.org/10.3390/rs12132080

AMA Style

Biondi R, Corradini S. Editorial for Special Issue “Convective and Volcanic Clouds (CVC)”. Remote Sensing. 2020; 12(13):2080. https://doi.org/10.3390/rs12132080

Chicago/Turabian Style

Biondi, Riccardo, and Stefano Corradini. 2020. "Editorial for Special Issue “Convective and Volcanic Clouds (CVC)”" Remote Sensing 12, no. 13: 2080. https://doi.org/10.3390/rs12132080

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