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Infrared remote sensing of Earth degassing - Ground study
mofettes thermography remote sensing swarm earthquakes CO2-gas emission
2015/9/10
Geodynamical processes e.g., volcanoes, often cause degassing at the Earth surface. The geogas emanates via
mineral springs, water mofettes, or dry mofettes. It is assumed that the emerging gas influ...
Seismic infrared infrared anomalies detection in the case of the Wenchuan earthquake using bi-angular advanced along-track scanning radiometer data
infrared anomalies detection Wenchuan earthquake
2015/8/17
The paper has developed Robust Satellite data analysis Technique (RST)
to detect seismic anomalies in the case of the Wenchuan earthquake occurred
on May 12, 2008, using the bi-angular Advanced Alon...
Seismic infrared anomalies detection in the case of the Wenchuan earthquake using bi-angular advanced along-track scanning radiometer data
Seismic monitoring Infrared multi-angle Robustness of Satellite Techniques
2015/8/14
The paper has developed Robust Satellite data analysis Technique (RST) to detect seismic anomalies in the case of the Wenchuan earthquake occurred on May 12, 2008, using the bi-angular Advanced Along-...
Annex to:Volcanic Ash Cloud Observation using Ground-based Ka-band Radar and Near-Infrared Lidar Ceilometer during the Eyjafjallajökull eruption
Earthquake GPS Historical seismology Ionosphere Irpinia
2014/8/18
Volcanic ash plumes are formed during explosive volcanic eruptions. After advection over several thousands of kilometers, volcanic ash particles are highly fragmented, dispersed and aged with micron- ...
Volcanic Ash Cloud Observation using Ground-based Ka-band Radar and Near-Infrared Lidar Ceilometer during the Eyjafjallajökull eruption
Volcanic eruptions radar lidar
2014/8/18
Active remote sensing techniques can probe volcanic ash plumes, but their sensitivity at a given distance depends upon the sensor transmitted power, wavelength and polarization capability. Building on...
Stimulated infrared emission from rocks: assessing a stress indicator
Stimulated infrared emission rocks assessing stress indicator
2007/1/10
To study the effect of stress-activated positive hole (p-hole) charge carriers on the infrared (IR) emission from rocks, we subjected a portion (~10 vol.%) of a large (30×60×7.5 cm3) block of anorthos...