COPE

COnstraints on near-term warming ProjEctions via distributionally robust statistical and machine learning

Started
July 1, 2023
Status
In Progress
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Abstract

Climate model projections of 21st century warming are uncertain and some climate models predict very high warming rates over the next few decades. Recent research has attempted to narrow the uncertainty range of future warming based on historical temperature trends. However, key climate system uncertainties limit our confidence in such observations-based constraints: (i) the magnitude and phase of multidecadal internal variability, (ii) anthropogenic and volcanic aerosol forcing, and (iii) potential model biases in representing the climatological base state, the strength of pattern effects, unforced variability or forced response patterns.

Here, we propose to develop robust constraints on near-future projections of climate warming via integrating climate model simulations with observations using distributionally robust statistical and machine learning (StatML) methods. Previous work within the SDSC-funded DASH has led to an improved understanding and attribution of the past climate record, from identifying historical forced vs. internal climate variability, separation of specific forced responses, and towards employing the concept of distributional robustness to multidecadal variability, thus reducing climate model spread.

We propose to leverage these developments for constraining near-term future warming projections, and projections of future temperature and precipitation at the regional scale via dynamical adjustment. A key challenge is to incorporate the concept of distributional robustness in climate science, with the potential to achieve robustness towards model structural uncertainty that will facilitate the transfer across climate models and towards observations.

Overall, the project will narrow uncertainties in near-term future climate, and advance methods using distributional robustness that are likely to transfer to many fields within Earth system science where imperfect process-based models are used and combined with observational data.

People

Collaborators

SDSC Team:
Victor Cohen
Guillaume Obozinski

PI | Partners:

ETH Zurich, Climate Physics:

  • Gergana Gyuleva
  • Prof. Reto Knutti
  • Prof. Nicolai Meinshausen

More info

University of Leipzig, Climate attribution:

  • Prof. Sebastian Sippel

More info

description

Motivation

‍Existing climate models provide good insights for understanding temperature forecasting. Since they are based on different atmospheric assumptions, they provide different predictions. Leveraging the variety of climate models, the project aims at building machine learning models that are robust towards the uncertainty of the models. This raises the question of defining the statistical robustness in such a context.

Proposed Approach / Solution

‍SDSC role is to mathematically formulate this key idea of statistical robustness towards model uncertainty. The current work focuses on developing linear models with robust model weights. These linear models take anomalies as input (time series of maps) and return the spatial forced response (time series of maps). The goal is to learn a worst-case combination of weights assigned to climates models, which leads to robust prediction of forced response using the linear coefficients (see fingerprint in Figure 1). We evaluate the learned model by training on all except one climate models and then testing it on the remaining one. The evaluation shows that we can decrease the worst-case error.

Impact

‍The project will develop robust statistical models for the near future warming predictions at global and regional scales, with careful consideration of uncertainties, based on an improved understanding of the historical climate record. The project’s impact will be highly relevant for near-term climate policy, and for climate impact studies because of refined warming estimates at the regional scale.

‍

Figure 1: Linear regression model scheme where the spatial temperature pattern (anomalies) is multiplied by the learned fingerprint.

Gallery

Annexe

Cover image source: Adobe Stock

Additional resources

Bibliography

  1. Sippel, S., Meinshausen, N., Székely, E., Fischer, E., Pendergrass, A.G., Lehner, F. and Knutti, R., 2021b. Robust detection of forced warming in the presence of potentially large climate variability. Science advances, 7(43): eabh4429.
  2. Székely, E., Sippel, S., Knutti, R., Obozinski, G. and Meinshausen, N., 2019. A direct approach to detection and attribution of climate change. arXiv preprint arXiv:1910.03346.
  3. Székely, E., Sippel, S., Meinshausen, N., Obozinski, G. and Knutti, R., 2022. Robustness constraints for detection and attribution of climate change under uncertainty. in preparation.
  4. Sippel, S., Meinshausen, N., Székely, E., Fischer, E., Pendergrass, A., Lehner, F. and Knutti, R., 2021a. Robust detection of forced warming in the presence of potentially large climatevariability. Science Advances, In Review.
  5. Sippel, S., Fischer, E.M., Scherrer, S.C., Meinshausen, N. and Knutti, R., 2020a. Late 1980s abrupt cold season temperature change in Europe consistent with circulation variability and long-term warming. Environmental Research Letters, 15(9): 094056.
  6. Sippel, S., Meinshausen, N., Fischer, E.M., Székely, E. and Knutti, R., 2020b. Climate change now detectable from any single day of weather at global scale. Nature climate change, 10(1): 35-41.

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