Artificial intelligence (AI) is one of the most rapidly developing fields in the field of electronic information technology. Along with diverse data, researchers are putting AI-enabled technologies like image processing, smart sensors, and intelligent inversion to the test in a number of geosciences areas. These technologies have the potential to aid the transition from qualitative to quantitative analysis in geosciences. Artificial intelligence (AI) approaches have proven to be effective in a variety of Earth scientific fields (e.g., climate models, weather prediction, hydrology, space weather, and solid Earth). Prediction, anomaly detection, event classification, and onboard decision-making are all tasks that AI approaches are utilised for on satellites, and they could possibly give high-speed options for describing subgrid processes in climate models. Artificial intelligence (AI) is one of the most rapidly developing fields in the field of electronic information technology. Along with diverse data, researchers are putting AI-enabled technologies like image processing, smart sensors, and intelligent inversion to the test in a number of geosciences areas. These technologies have the potential to aid the transition from qualitative to quantitative analysis in the geosciences.
Title : Sustainable ocean: Blueprint for the planet
Dorrik Stow Frse, Heriot Watt University, United Kingdom
Title : Landslides.Rainfall one of the main triggering factors in the mountainous regions of Puebla, Mexico.
Oscar Andres Cuanalo Campos, Universidad Popular Autónoma del Estado de Puebla, Mexico
Title : Geomorphic evidence of the tectonic delamination of the upper crust in central Tien Shan
Alexander Strom, Chief Expert from Geodynamics Research Centre, Russian Federation
Title : Geotechnical ground investigation
Myint Win Bo, York University, Canada
Title : Machine learning to predict geological facies in complex carbonate reservoirs.
Ibrahim Milad, BP, United Kingdom
Title : Effect of infill thickness in the joint under cyclic loads
S M Mahdi Niktabar, Institute of Geonics Czech Academy of Sciences, Czech Republic