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AI Agents Translate and Partially Improve Climate Model Cloud Physics in Minutes

November 4, 2026arXiv: 2611.03543v1

Scientists used large language model (LLM) agents to rewrite classic cloud‑physics equations, re‑implement recent machine‑learning closures, and propose new forms for warm‑rain collision–coalescence. The study shows that the agents can produce code that runs, differentiates, and conserves mass in a test box model. By comparing these agent‑generated closures with existing analytical schemes and neural‑network emulators, the researchers found that many retuned analytical models match or beat the learned closures while using far fewer floating‑point operations. The authors tested three workflows: an expert guiding the agent, a single‑shot call to an LLM, and an iterative call cycle with feedback. Retuning classical parameterizations reduced error to below 5 % of the high‑fidelity reference and lowered computational cost by up to 80 %. However, unattended performance varied with the specific LLM; only iterative refinement consistently improved structural validity, and accuracy gains were modest and model‑dependent. These results suggest that LLM agents can accelerate, but not yet replace, human expertise in developing Earth‑system model physics.

The paper’s Figure 1 illustrates the overall pipeline and the three agentic workflows, showing how the agents synthesize literature, code, and evaluate against a super‑droplet reference. Figure 2 compares mean rain‑conversion error and rollout error versus floating‑point operations per step, displaying that retuned classical schemes achieve comparable or lower errors than neural‐network closures at substantially lower computational cost.

Diagram of the agentic workflow pipeline, including expert‑in‑the‑loop, single‑shot API, and iterative API approaches, and the evaluation framework for climate model parameterizations.
Figure 1. Overview of the analysis and methodology. The figure shows the overall pipeline and the three agentic workflows used to translate historical schemes, reproduce machine‑learning baselines, and propose new closures.Lamb, Kara D. · arXiv:2611.03543v1 · Figure 1: · CC BY 4.0
Bar chart showing mean rain‑conversion error and MAPE plotted against floating‑point operations, illustrating the performance of retuned Classical schemes versus learned neural‑network closures.
Figure 2. Parameterization performance. (a) Mean error in rain‑conversion timescales for the four literature schemes, including publications and retuned coefficients. (b) Rain‑mass rollout MAPE versus floating‑point operations per model step, comparing Classical schemes and neural‑network closures. The figure demonstrates that retuned Classical schemes achieve comparable or lower errors at substantially lower computational cost.Lamb, Kara D. · arXiv:2611.03543v1 · Figure 2: · CC BY 4.0

Source paper

Can LLM Agents Improve Imperfect Earth System Model Parameterizations?

PhysicsMachine Learning
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