4.6 Article

Calibrating an Ice Sheet Model Using High-Dimensional Binary Spatial Data

Journal

JOURNAL OF THE AMERICAN STATISTICAL ASSOCIATION
Volume 111, Issue 513, Pages 57-72

Publisher

AMER STATISTICAL ASSOC
DOI: 10.1080/01621459.2015.1108199

Keywords

Climate change; Computer experiments; Gaussian processes; Principal components; Spatial generalized linear mixed models

Funding

  1. National Science Foundation through NSF Statistical Methods in the Atmospheric Sciences Network [1106862, 1106974, 1107046]
  2. National Science Foundation [NSF-DMS-1418090, NSF-OPP-ANT-1043018]
  3. National Science Foundation through Network for Sustainable Climate Risk Management (SCRiM) under NSF cooperative agreement [GEO1240507]
  4. Direct For Mathematical & Physical Scien
  5. Division Of Mathematical Sciences [1418090, GRANTS:13778004, 1107046] Funding Source: National Science Foundation

Ask authors/readers for more resources

Rapid retreat of ice in the Amundsen Sea sector of West Antarctica may cause drastic sea level rise, posing significant risks to populations in low-lying coastal regions. Calibration of computer models representing the behavior of the West Antarctic Ice Sheet is key for informative projections of future sea level rise. However, both the relevant observations and the model output are high-dimensional binary spatial data; existing computer model calibration methods are unable to handle such data. Here we present a novel calibration method for computer models whose output is in the form of binary spatial data. To mitigate the computational and inferential challenges posed by our approach, we apply a generalized principal component based dimension reduction method. To demonstrate the utility of our method, we calibrate the PSU3D-ICE model by comparing the output from a 499-member perturbed-parameter ensemble with observations from the Amundsen Sea sector of the ice sheet. Our methods help rigorously characterize the parameter uncertainty even in the presence of systematic data-model discrepancies and dependence in the errors. Our method also helps inform environmental risk analyses by contributing to improved projections of sea level rise from the ice sheets. Supplementary materials for this article are available online.

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