Deep ice - Deep learning. Artificial intelligence revealing the oldest ice climate signals

HORIZON.1.1HORIZON-ERCID: 101088125
EC Contribution
€19,810
Consortium Size
2 orgs
Summary

We are missing a central piece in the puzzle to understanding our Earth’s climate: Its dynamics fundamentally changed during the “Mid-Pleistocene Transition”, when some 1.2 million years ago the oscillation between warm periods and ice ages shifted its periodicity from 41 to 100 ka. A key set of information about this change was archived in the snow that fell at that time in Antarctica. At unique locations, that snow is still preserved today in the deepest ice layers– but does it still contain its original message? AiCE will answer this key question specifically using chemical impurity signals which make up a large part of the ice core record about past atmospheric conditions. For this purpose, we take a new approach to study the oldest and highly thinned layers at unprecedented detail. While conventional meltwater analysis delivers 1D cm-resolution signals, we go into 2D by imaging the chemical impurity distribution at micro-metric scale in the solid ice core. This way, we can retrieve crucial information that is inevitably lost by melting: The same ice matrix preserving the climatic record can act on it and ultimately destroy it through various processes, causing impurities to relocate away from their original layer. Hence, the goal is to identify the original layering, by detecting post-depositional change through analyzing highly-dimensional chemical images. However, human observers have clear limitations in detecting all the important details in such complex visual datasets. This is why AiCE will add deep learning to deep ice: Artificial intelligence (Ai) image analysis will be established through a comprehensive understanding of the chemical image features and their connection to post-depositional processes. With this, we can address the fundamental climate questions through deciphering deep ice – in Antarctica and elsewhere. Ultimately, AiCE could revolutionize how we interpret the oldest paleoclimate signals in ice cores and other archives.

Consortium (2)

Project Results (8)

Source: CORDIS, the EU research results database.

Publications (8)
Single particle ICP-TOFMS on previously characterised EGRIP ice core samples: new approaches, limitations, and challenges
The Cryosphere· 2026DOI
Nicolas Stoll, David Clases, Raquel Gonzalez de Vega, Matthias Elinkmann, Piers Larkman, Pascal Bohleber
Argon versus helium as carrier gas for LA-ICP-MS impurity mapping on ice cores
Talanta Open· 2025DOI
Pascal Bohleber, Kristina Mervič, Remi Dallmayr, Ciprian Stremtan, Martin Šala
Assessing the impact of common sample preparation strategies for single particle ICP-MS regarding recovery and size distribution of natural single particles
Journal of Analytical Atomic Spectrometry· 2025DOI
Lhiam Paton; Sandra Kiesel; Grit Steinhoefel; Matthias Elinkmann; Thebny Thaise Moro; Raquel Gonzalez de Vega; Pascal Bohleber; David Clases
Chemical and visual characterisation of EGRIP glacial ice and cloudy bands within
The Cryosphere· 2025DOI
Nicolas Stoll, Julien Westhoff, Pascal Bohleber, Anders Svensson, Dorthe Dahl-Jensen, Carlo Barbante, Ilka Weikusat
Faster chemical mapping assisted by computer vision: insights from glass and ice core samples
The Analyst· 2025DOI
Larkman, Piers; Vascon, Sebastiano; Šala, Martin; Stoll, Nicolas; Barbante, Carlo; Bohleber, Pascal
New evidence on the microstructural localization of sulfur and chlorine in polar ice cores with implications for impurity diffusion
The Cryosphere· 2025DOI
Pascal Bohleber; Nicolas Stoll; Piers Larkman; Rachael H. Rhodes; David Clases
δ(<sup>18</sup>O/<sup>16</sup>O) Determinations in Water Using Inductively Coupled Plasma–Tandem Mass Spectrometry
Analytical Chemistry· 2025DOI
Shaun T. Lancaster; Johanna Irrgeher; Remi Dallmayr; Elisa Conrad; Maria Hörhold; Pascal Bohleber; Melanie Behrens; Federica Camin; Klara Žagar; Polona Vreča; Thomas Prohaska
What does the impurity variability at the microscale represent in ice cores? Insights from a conceptual approach
The Cryosphere· 2024DOI
P. Larkman; R. H. Rhodes; N. Stoll; C. Barbante; C. Barbante; P. Bohleber; P. Bohleber