AbstractWe present a polynomial chaos based minimum variance formulation to solve inverse problems. The utility of the proposed approach is evaluated by considering the ash transport problem arising due to volcanic eruption. Volcanic ash advisory centers generally makes use of mathematical models for column eruption and advection and diffusion of ash cloud in atmosphere. These models require input data on source conditions such as vent radius, vent velocity and distribution of ash-particle size. The inputs are usually not well constrained, and estimates of the uncertainty in the inputs is needed to make accurate predictions of cloud motion. The recent eruption of Eyjafjallaj̈okull, Iceland in April 2010 is considered as test example. For va...
Determination of the volcanic eruption source parameters—total grain-size distribution and vertical ...
We present a Bayesian inversion method for estimating volcanic ash emissions using satellite retriev...
This is the final version. Available from the American Geophysical Union via the DOI in this recor...
We present a polynomial chaos based minimum variance formulation to solve inverse problems. The util...
AbstractWe present a polynomial chaos based minimum variance formulation to solve inverse problems. ...
Data on source conditions for the 14 April 2010 paroxysmal phase of the Eyjafjallajökull eruption, I...
In this paper, we will present ongoing work on using a dynamic data driven application system (DDDAS...
AbstractIn this paper, we will present ongoing work on using a dynamic data driven application syste...
The requirement to forecast volcanic ash concentrations was amplified as a response to the 2010 Eyja...
The requirement to forecast volcanic ash concentrations was amplified as a response to the 2010 Eyja...
AbstractIn this paper, we will present ongoing work on using a dynamic data driven application syste...
Volcanic ash can interact with the earth system on many temporal and spatial scales and is a signifi...
AbstractIn this paper we will present early work on using a DDDAS based approach to the construction...
Determination of the volcanic eruption source parameters—total grain-size distribution and vertical ...
Determination of the volcanic eruption source parameters—total grain-size distribution and vertical ...
Determination of the volcanic eruption source parameters—total grain-size distribution and vertical ...
We present a Bayesian inversion method for estimating volcanic ash emissions using satellite retriev...
This is the final version. Available from the American Geophysical Union via the DOI in this recor...
We present a polynomial chaos based minimum variance formulation to solve inverse problems. The util...
AbstractWe present a polynomial chaos based minimum variance formulation to solve inverse problems. ...
Data on source conditions for the 14 April 2010 paroxysmal phase of the Eyjafjallajökull eruption, I...
In this paper, we will present ongoing work on using a dynamic data driven application system (DDDAS...
AbstractIn this paper, we will present ongoing work on using a dynamic data driven application syste...
The requirement to forecast volcanic ash concentrations was amplified as a response to the 2010 Eyja...
The requirement to forecast volcanic ash concentrations was amplified as a response to the 2010 Eyja...
AbstractIn this paper, we will present ongoing work on using a dynamic data driven application syste...
Volcanic ash can interact with the earth system on many temporal and spatial scales and is a signifi...
AbstractIn this paper we will present early work on using a DDDAS based approach to the construction...
Determination of the volcanic eruption source parameters—total grain-size distribution and vertical ...
Determination of the volcanic eruption source parameters—total grain-size distribution and vertical ...
Determination of the volcanic eruption source parameters—total grain-size distribution and vertical ...
We present a Bayesian inversion method for estimating volcanic ash emissions using satellite retriev...
This is the final version. Available from the American Geophysical Union via the DOI in this recor...