English

A neural network-based scale-adaptive cloud-fraction scheme for GCMs

Atmospheric and Oceanic Physics 2023-06-21 v2

Abstract

Cloud fraction significantly affects the short- and long-wave radiation. Its realistic representation in general circulation models (GCMs) still poses great challenges in modeling the atmosphere. Here, we present a neural network-based diagnostic scheme that uses the grid-mean temperature, pressure, liquid and ice water mixing ratios, and relative humidity to simulate the sub-grid cloud fraction. The scheme, trained using CloudSat data with explicit consideration of grid sizes, realistically simulates the observed cloud fraction with a correlation coefficient (r) > 0.9 for liquid-, mixed-, and ice-phase clouds. The scheme also captures the observed non-monotonic relationship between cloud fraction and relative humidity and is computationally efficient, and robust for GCMs with a variety of horizontal and vertical resolutions. For illustrative purposes, we conducted comparative analyses of the 2006-2019 climatological-mean cloud fractions among CloudSat, and simulations from the new scheme and the Xu-Randall scheme (optimized the same way as the new scheme). The network-based scheme improves not only the spatial distribution of the total cloud fraction but also the cloud vertical structure (r > 0.99). For example, the biases of too-many high-level clouds over the tropics and too-many low-level clouds over regions around 60{\deg}S and 60{\deg}N in the Xu-Randall scheme are significantly reduced. These improvements are also found to be insensitive to the spatio-temporal variability of large-scale meteorology conditions, implying that the scheme can be used in different climate regimes.

Keywords

Cite

@article{arxiv.2304.01879,
  title  = {A neural network-based scale-adaptive cloud-fraction scheme for GCMs},
  author = {Guoxing Chen and Wei-Chyung Wang and Shixi Yang and Yixin Wang and Feng Zhang and Kun Wu},
  journal= {arXiv preprint arXiv:2304.01879},
  year   = {2023}
}
R2 v1 2026-06-28T09:49:10.919Z