Climbing down Charney's ladder: Machine Learning and the post-Dennard era of computational climate science
V. Balaji

TL;DR
This paper discusses the impending end of Dennard scaling and explores how computational climate science may evolve by returning to pattern recognition or advancing mathematical models, marking a potential paradigm shift.
Contribution
It analyzes the impact of the end of Dennard scaling on climate modeling and proposes new directions combining physical knowledge, computation, and data.
Findings
End of Dennard scaling prompts a fundamental change in climate modeling approaches.
Potential shift towards pattern recognition and extrapolation methods.
Reevaluation of the role of mathematical equations in future climate science.
Abstract
The advent of digital computing in the 1950s sparked a revolution in the science of weather and climate. Meteorology, long based on extrapolating patterns in space and time, gave way to computational methods in a decade of advances in numerical weather forecasting. Those same methods also gave rise to computational climate science, studying the behaviour of those same numerical equations over intervals much longer than weather events, and changes in external boundary conditions. Several subsequent decades of exponential growth in computational power have brought us to the present day, where models ever grow in resolution and complexity, capable of mastery of many small-scale phenomena with global repercussions, and ever more intricate feedbacks in the Earth system. The current juncture in computing, seven decades later, heralds an end to what is called Dennard scaling, the physics…
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