ICELEARNING · Artificial Intelligence techniques for ice core analyses
Horizon 2020 — Marie Skłodowska-Curie Actions
- Duration
- 2020-01-15 → 2022-01-14
- EU contribution
- €171,473
- Participants
- 1
- Scheme
- MSCA-IF-EF-ST
Lines connect the coordinator with its partners.
Results in brief
Artificial Intelligence techniques for ice core analyses
Earth System scientists can investigate the Earth past climate by studying natural archives where information can be frozen in time. Examples of such archives are the bed floor of the oceans or ice from polar regions and glaciers. Ice cores have provided us with some of the most pristine records of the Earth’s past climate. While the oldest Antarctic and Greenland cores date back to up to 800,000 and 125,000 year ago respectively and register variability of climate parameters at hemispheric scales, ice stored in glaciers and small ice caps located at lower latitudes typically contain a fingerprint or local to regional climate. Understanding climate variability is important to bring forward our knowledge of Earth system climate, understand the past and refine models to better constrain future scenarios. Different types of climate information can be trapped in ice cores and can be retrieved using many methods and analytical techniques. The climate proxies that have been targeted in this project are insoluble particles, i.e. visible particles that do not dissolve in water. The broad category of insoluble particles include mineral dust, volcanic particles, biological matter like pollen grains and marine particulates like diatoms and foraminifera. The investigation of these particles in ice cores allow to produce past climate records which scientific importance are far reaching. Dust records allow to investigate the Earth past aridity, vegetation cover and atmospheric circulation. Volcanic particles tell us about past volcanic eruptions thereby allowing to investigate past volcanic activity. Biological matter and marine particles tell climate scientists crucial information about past vegetation and sea level. At present, by far the most common technique deployed to find and classify insoluble particles in ice cores is manual microscopy. Despite bench microscopy can provide precise information to the operator, its use is extremely laborious, time consuming and a limited number of samples can be processed. The overall objective of the ICELEARNING project is to develop a methodology that would be able to support human researchers in finding and at the same time automatically classifying different types of insoluble particles in ice cores. We do so by deploying a Flow Imaging Microscope, called FlowCam, an instrument capable to continuously acquire images of particles in liquid ice core samples. The images are then processed by neural networks, specifically trained to recognize and count autonomously different types of particles at the same time. The developed methodology would not only benefit ice core scientists but would positively impact different branches of science where investigations by manual bench microscopy are still the standard approach. The scientific project objectives include: characterization of the FlowCam instrument for ice core samples, selection and acquisition of the training datasets necessary to train classification models, development and training of the models, application of the models to real ice core samples and comparison with human microscopy to access the potentials and limitations of the developed methodology.
Data: CORDIS, © European Union
Project objective
The detection of insoluble particles trapped in ice or sediment cores, like pollen grains, foraminiferal and diatom assemblages, volcanic and dust particles represents the basis for paleoresearch on the biosphere, volcanism and oceanic and atmospheric realms. To date, except for ice core dust, this analytical goal is achieved during years of particle observations by manual microscopy. Artificial Intelligence predictive models are already applied to several research fields within geoscience, but up to date its implementation to paleoclimate is missing. With ICELEARNING, I aim to develop a two-phase routine for the automatic quantification of insoluble particles trapped in ice cores. The routine is based on a commercial Flow Imaging Microscope producing particle images from within melted ice samples. The images are then analyzed by Pattern Recognition algorithms which will be developed for automatic particle classification and counting. The routine will be specifically developed in order to be implemented in Continuous Flow Analysis (CFA) systems, therefore surpassing the traditional methods by providing continuous particle records from ice cores. ICELEARNING methodology is suitable to any diluted sample, thus representing a ground-breaking analytical advancement from ice core science to marine geology. This innovative routine is automatic and non-destructive, imperative prerequisites for the future Antarctic ice core project analytical measurements, aiming to retrieve a continuous climatic and environmental record covering the last 1.5 Myr. ICELERNING will be developed at Ca’ Foscari University of Venice with Prof. Carlo Barbante, leading expert in trace and ultra-trace level impurity detections in ice cores and with the University of Bergen, a top institution in marine geology and paleoceanography. This unique synergy, in addition to the proposer’s knowledge of CFA systems and machine learning techniques will provide the best preconditions for the project success.
Original text from CORDIS.
Participants
- UNIVERSITA CA' FOSCARI VENEZIA · VeneziaCoordinatorItaly
Links
Data: CORDIS, © European Union
