Idealized tropical cyclone simulations under dry environmental environment

This data set contains the idealized WRF simulations that was used to study the role of moisture-induced radiative heating in tropical cyclone genesis. The concept that radiative heating can provide substantial energy for tropical cyclone intensification has been identified in numerical simulations and been observed in satellite measurements. However, how the distribution of greenhouse gas affects the evolution of tropical cyclone genesis remains unclear.
The radiative heating and tropical cyclone information provided here can be used to estimate how the environmental moisture interacting radiation affects the tropical cyclone intensification. These data are associated with the article: Wu, S.-N., Soden, B., “Radiative Feedbacks from Dry Environmental Air Accelerate Tropical Cyclogenesis”

本数据集包含用于探究水汽诱导辐射加热在热带气旋生成过程中所起作用的理想化WRF（Weather Research and Forecasting Model）模拟结果。辐射加热可为热带气旋增强提供可观能量这一学术观点，已通过数值模拟得到验证，并在卫星观测中被捕捉到。然而，温室气体的分布如何影响热带气旋生成的演化过程，目前仍不明确。
本数据集提供的辐射加热与热带气旋相关数据，可用于估算环境水汽与辐射的相互作用如何影响热带气旋的增强过程。本数据集关联下述研究论文：Wu, S.-N.、Soden, B. 所著《干燥环境空气的辐射反馈加速热带气旋生成》（"Radiative Feedbacks from Dry Environmental Air Accelerate Tropical Cyclogenesis"）