Articles | Volume 12, issue 3
https://doi.org/10.5194/gmd-12-933-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gmd-12-933-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Methods for assessment of models
| 
12 Mar 2019
Methods for assessment of models |
| 12 Mar 2019
| 12 Mar 2019
ATAT 1.1, the Automated Timing Accordance Tool for comparing ice-sheet model output with geochronological data
Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK
Chris D. Clark
Department of Geography, University of Sheffield, Sheffield, S10 2TN, UK
David Small
Department of Geography, Durham University, Durham, DH1 3LE, UK
Richard C. A. Hindmarsh
British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK
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Cited
14 citations as recorded by crossref.
- Behavioural tendencies of the last British–Irish Ice Sheet revealed by data–model comparison J. Ely et al. 10.1002/jqs.3628
- Assessing ice sheet models against the landform record: The Likelihood of Accordant Lineations Analysis (LALA) tool R. Archer et al. 10.1002/esp.5658
- Ice sheet speed-dating: Using expert judgement to identify “good” simulations of the last glacial maximum North American ice sheets N. Gandy et al. 10.1016/j.quascirev.2024.108690
- Timing, pace and controls on ice sheet retreat: an introduction to the BRITICE‐CHRONO transect reconstructions of the British–Irish Ice Sheet C. Clark et al. 10.1002/jqs.3326
- Glacial trimlines to identify former ice margins and subglacial thermal boundaries: A review and classification scheme for trimline expression C. Rootes & C. Clark 10.1016/j.earscirev.2020.103355
- Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction C. Clark et al. 10.1111/bor.12594
- Modelling erratic dispersal accounting for shifting ice flow geometries: A new method and explanations of erratic dispersal of the British–Irish Ice Sheet R. Veness et al. 10.1002/jqs.3720
- Collapse of the Last Eurasian Ice Sheet in the North Sea Modulated by Combined Processes of Ice Flow, Surface Melt, and Marine Ice Sheet Instabilities N. Gandy et al. 10.1029/2020JF005755
- A Greenland-wide empirical reconstruction of paleo ice sheet retreat informed by ice extent markers: PaleoGrIS version 1.0 T. Leger et al. 10.5194/cp-20-701-2024
- An ensemble of Antarctic deglacial simulations constrained by geological observations M. Pittard et al. 10.1016/j.quascirev.2022.107800
- Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet J. Ely et al. 10.1002/jqs.3098
- GIS dataset: geomorphological record of terrestrial-terminating ice streams, southern sector of the Baltic Ice Stream Complex, last Scandinavian Ice Sheet, Poland I. Szuman et al. 10.5194/essd-13-4635-2021
- Antarctic Ice Sheet paleo-constraint database B. Lecavalier et al. 10.5194/essd-15-3573-2023
- Antarctic ice sheet palaeo-thinning rates from vertical transects of cosmogenic exposure ages D. Small et al. 10.1016/j.quascirev.2018.12.024
13 citations as recorded by crossref.
- Behavioural tendencies of the last British–Irish Ice Sheet revealed by data–model comparison J. Ely et al. 10.1002/jqs.3628
- Assessing ice sheet models against the landform record: The Likelihood of Accordant Lineations Analysis (LALA) tool R. Archer et al. 10.1002/esp.5658
- Ice sheet speed-dating: Using expert judgement to identify “good” simulations of the last glacial maximum North American ice sheets N. Gandy et al. 10.1016/j.quascirev.2024.108690
- Timing, pace and controls on ice sheet retreat: an introduction to the BRITICE‐CHRONO transect reconstructions of the British–Irish Ice Sheet C. Clark et al. 10.1002/jqs.3326
- Glacial trimlines to identify former ice margins and subglacial thermal boundaries: A review and classification scheme for trimline expression C. Rootes & C. Clark 10.1016/j.earscirev.2020.103355
- Growth and retreat of the last British–Irish Ice Sheet, 31 000 to 15 000 years ago: the BRITICE‐CHRONO reconstruction C. Clark et al. 10.1111/bor.12594
- Modelling erratic dispersal accounting for shifting ice flow geometries: A new method and explanations of erratic dispersal of the British–Irish Ice Sheet R. Veness et al. 10.1002/jqs.3720
- Collapse of the Last Eurasian Ice Sheet in the North Sea Modulated by Combined Processes of Ice Flow, Surface Melt, and Marine Ice Sheet Instabilities N. Gandy et al. 10.1029/2020JF005755
- A Greenland-wide empirical reconstruction of paleo ice sheet retreat informed by ice extent markers: PaleoGrIS version 1.0 T. Leger et al. 10.5194/cp-20-701-2024
- An ensemble of Antarctic deglacial simulations constrained by geological observations M. Pittard et al. 10.1016/j.quascirev.2022.107800
- Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet J. Ely et al. 10.1002/jqs.3098
- GIS dataset: geomorphological record of terrestrial-terminating ice streams, southern sector of the Baltic Ice Stream Complex, last Scandinavian Ice Sheet, Poland I. Szuman et al. 10.5194/essd-13-4635-2021
- Antarctic Ice Sheet paleo-constraint database B. Lecavalier et al. 10.5194/essd-15-3573-2023
1 citations as recorded by crossref.
Latest update: 30 May 2025
Short summary
During the last 2.6 million years, the Earth's climate has cycled between cold glacials and warm interglacials, causing the growth and retreat of ice sheets. These ice sheets can be independently reconstructed using numerical models or from dated evidence that they leave behind (e.g. sediments, boulders). Here, we present a tool for comparing numerical model simulations with dated ice-sheet material. We demonstrate the utility of this tool by applying it to the last British–Irish ice sheet.
During the last 2.6 million years, the Earth's climate has cycled between cold glacials and warm...
