During an eruptive event, the near-real-time monitoring of volcanic explosion onset and its mass flow rate (MFR) is a key factor to predict ash plume dispersion and to mitigate risk to air traffic. Microwave (MW) weather radars have proved to be a fundamental instrument to derive eruptive source parameters. We extend this capability to include an early-warning detection scheme within the overall volcanic ash radar retrieval methodology. This scheme, called the volcanic ash detection (VAD) algorithm, is based on a hybrid technique using both fuzzy logic and conditional probability. Examples of VAD applications are shown for some case studies, including the Icelandic Grímsvötn eruption in 2011, the Eyjafjallajökull eruption in 2010, and the I...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
During an eruptive event, the near-real-time monitoring of volcanic explosion onset and its mass fl...
During an eruptive event, the near-real-time monitoring of volcanic explosion onset and its mass flo...
The potential of ground-based microwave weather radar systems for volcanic ash cloud detection and q...
The sub-glacial Eyjafjoll explosive volcanic eruptions of April and May 2010 are analyzed and quanti...
The explosive eruption at the summit of sub-glacial Ejyafjallajökull volcano in April-May 2010 was ...
The eruption of the Eyjafjallajokull volcano in April-May 2010 was continuously monitored by the Kef...
The eruption of the Eyjafjallajökull volcano in April-May 2010 was continuously monitored by the Ke...
The potential of ground-based microwave weather radar systems for volcanic ash cloud detection and ...
The sub-glacial Plinian explosive eruption of the Grímsvötn volcano, which occurred on May 2011, is ...
Microphysical and dynamical features of volcanic tephra due to Plinian and sub-Plinian eruptions can...
Microphysical and dynamical features of volcanic tephra due to Plinian and sub-Plinian eruptions can...
The microphysical and dynamical features of volcanic clouds, due to Plinian and sub-Plinian eruption...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
During an eruptive event, the near-real-time monitoring of volcanic explosion onset and its mass fl...
During an eruptive event, the near-real-time monitoring of volcanic explosion onset and its mass flo...
The potential of ground-based microwave weather radar systems for volcanic ash cloud detection and q...
The sub-glacial Eyjafjoll explosive volcanic eruptions of April and May 2010 are analyzed and quanti...
The explosive eruption at the summit of sub-glacial Ejyafjallajökull volcano in April-May 2010 was ...
The eruption of the Eyjafjallajokull volcano in April-May 2010 was continuously monitored by the Kef...
The eruption of the Eyjafjallajökull volcano in April-May 2010 was continuously monitored by the Ke...
The potential of ground-based microwave weather radar systems for volcanic ash cloud detection and ...
The sub-glacial Plinian explosive eruption of the Grímsvötn volcano, which occurred on May 2011, is ...
Microphysical and dynamical features of volcanic tephra due to Plinian and sub-Plinian eruptions can...
Microphysical and dynamical features of volcanic tephra due to Plinian and sub-Plinian eruptions can...
The microphysical and dynamical features of volcanic clouds, due to Plinian and sub-Plinian eruption...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...
International audienceThe morning of November 23, 2013, a lava fountain formed from the New South-Ea...