Spatiotemporal Evolution Simulation of Volcanic Ash Cloud from Remote Sensing Image

2019 ◽  
pp. 423-430
Author(s):  
Cheng Fan Li ◽  
Lan Liu ◽  
Xian Kun Sun ◽  
Jun Juan Zhao ◽  
Yuan Yuan ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Volcanic Ash ◽  
Remote Sensing Image ◽  
Spatiotemporal Evolution ◽  
Evolution Simulation ◽  
Volcanic Ash Cloud ◽  
Ash Cloud

Temporal and spatial structure of a volcanic ash cloud: ground-based remote sensing and numerical modeling

2010 ◽  
Author(s):  
Klaus Schäfer ◽  
Wolfram Birmili ◽  
Josef Cyrys ◽  
Stefan Emeis ◽  
Renate Forkel ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Numerical Modeling ◽  
Spatial Structure ◽  
Volcanic Ash ◽  
Volcanic Ash Cloud ◽  
Temporal And Spatial ◽  
Ash Cloud

scholarly journals Monitoring volcanic ash cloud top height through simultaneous retrieval of optical data from polar orbiting and geostationary satellites

2013 ◽  
Vol 13 (5) ◽  
pp. 2589-2606 ◽  
Author(s):  
K. Zakšek ◽  
M. Hort ◽  
J. Zaletelj ◽  
B. Langmann
Keyword(s):  
Remote Sensing ◽  
Satellite Remote Sensing ◽  
Volcanic Ash ◽  
Good Choice ◽  
Optical Data ◽  
Global Level ◽  
Geostationary Satellites ◽  
Volcanic Ash Cloud ◽  
Photogrammetric Method ◽  
Ash Cloud

Abstract. Volcanic ash cloud-top height (ACTH) can be monitored on the global level using satellite remote sensing. Here we propose a photogrammetric method based on the parallax between data retrieved from geostationary and polar orbiting satellites to overcome some limitations of the existing methods of ACTH retrieval. SEVIRI HRV band and MODIS band 1 are a good choice because of their high resolution. The procedure works well if the data from both satellites are retrieved nearly simultaneously. MODIS does not retrieve the data at exactly the same time as SEVIRI. To compensate for advection we use two sequential SEVIRI images (one before and one after the MODIS retrieval) and interpolate the cloud position from SEVIRI data to the time of MODIS retrieval. The proposed method was tested for the case of the Eyjafjallajökull eruption in April 2010. The parallax between MODIS and SEVIRI data can reach 30 km, which implies an ACTH of approximately 12 km at the beginning of the eruption. At the end of April eruption an ACTH of 3–4 km is observed. The accuracy of ACTH was estimated to be 0.6 km.

scholarly journals Volcanic ash cloud detection from space: a comparison between the RSTASHtechnique and the water vapour corrected BTD procedure

2011 ◽  
Vol 2 (3) ◽  
pp. 263-277 ◽  
Author(s):  
Alessandro Piscini ◽  
Stefano Corradini ◽  
Francesco Marchese ◽  
Luca Merucci ◽  
Nicola Pergola ◽  
...  
Keyword(s):  
Water Vapour ◽  
Volcanic Ash ◽  
Cloud Detection ◽  
Volcanic Ash Cloud ◽  
Ash Cloud
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