# Maximizing simulated tropical cyclone intensity with action minimization

## TL;DR

This paper introduces an action minimization algorithm for high-resolution tropical cyclone simulations, enabling targeted intensification studies with significantly reduced computational costs and revealing new insights into intensification mechanisms.

## Contribution

The novel application of action minimization to weather models allows efficient, physically plausible intensification of tropical cyclones, facilitating detailed studies of rapid intensification processes.

## Key findings

- Ten-fold reduction in computational cost for intensification studies
- Preferential reduction of low-level shear in intensified TCs
- Asymmetric heating patterns can cause significant non-linear intensification

## Abstract

Direct computer simulation of intense tropical cyclones (TCs) in weather models is limited by computational expense. Intense TCs are rare and have small-scale structures, making it difficult to produce large ensembles of storms at high resolution. Further, models often fail to capture the process of rapid intensification, which is a distinguishing feature of many intense TCs. Understanding rapid intensification is especially important in the context of global warming, which may increase the frequency of intense TCs. To better leverage computational resources for the study of rapid intensification, we introduce an action minimization algorithm applied to the WRF and WRFPLUS models. Action minimization nudges the model into forming more intense TCs than it otherwise would; it does so via the maximum likelihood path in a stochastic formulation of the model, thereby allowing targeted study of intensification mechanisms. We apply action minimization to simulations of Hurricanes Danny (2015) and Fred (2009) at 6 km resolution to demonstrate that the algorithm consistently intensifies TCs via physically plausible pathways. We show an approximately ten-fold computational savings using action minimization to study the tail of the TC intensification distribution. Further, for Hurricanes Danny and Fred, action minimization produces perturbations that preferentially reduce low-level shear as compared to upper-level shear, at least above a threshold of approximately $4 \mathrm{\ m \ s^{-1}}$. We also demonstrate that asymmetric, time-dependent patterns of heating can cause significant TC intensification beyond symmetric, azimuthally-averaged heating and find a regime of non-linear response to asymmetric heating that has not been extensively studied in previous work.