Shi et al. (2025) The Effects of Sea‐State‐Dependent Surface Fluxes on CESM2 Climate Simulations
⚠️ Warning: This summary was generated from the abstract only, as the full text was not available.
Identification
- Journal: Journal of Advances in Modeling Earth Systems
- Year: 2025
- Date: 2025-12-01
- Authors: Xiaoming Shi, Qing Li, Diah Valentina Lestari, Shangfei Lin, Hui Su
- DOI: 10.1029/2025ms005284
Research Groups
- Community Earth System Model (CESM) development team (likely National Center for Atmospheric Research - NCAR)
- WAVEWATCH III development community
Short Summary
This study implements and evaluates a sea-state-dependent surface flux scheme, incorporating prognostic ocean waves via WAVEWATCH III, into CESM2, demonstrating significant improvements in mean atmospheric circulation and upper ocean biases.
Objective
- To implement and document a sea-state-dependent surface flux scheme, considering wave effects on ocean surface roughness and sea spray on sensible and latent heat, within the Community Earth System Model version 2 (CESM2) by integrating WAVEWATCH III.
- To evaluate the impacts of this new scheme on the climate mean state, atmospheric circulation, and upper ocean properties, and assess its ability to reduce existing model biases.
Study Configuration
- Spatial Scale: Global (with specific mentions of Southern Ocean, eastern boundary currents, eastern and central Pacific)
- Temporal Scale: Climate mean state and variability, recent decades
Methodology and Data
- Models used: Community Earth System Model version 2 (CESM2), WAVEWATCH III (prognostic ocean surface wave model)
- Data sources: Implied comparison with observational and/or reanalysis data for model validation and bias assessment.
Main Results
- The new sea-state-dependent surface flux scheme significantly impacts mean atmospheric circulation and the upper ocean.
- Errors in mean atmospheric circulation and surface temperature patterns are reduced.
- The modified surface flux lowers the eddy-driven jet speed and weakens the Hadley circulation.
- Global sea surface temperature (SST) warm bias is reduced, particularly due to cooling in the Southern Ocean and eastern boundary currents.
- A weak cooling trend is simulated in parts of the eastern and central Pacific for recent decades, which reduces an existing SST trend bias in CESM2.
Contributions
- First implementation and documentation of a sea-state-dependent surface flux scheme, incorporating prognostic ocean waves, within a major Earth System Model (CESM2).
- Demonstrates the critical importance of representing ocean surface waves for accurate simulation of air-sea momentum, heat, and water exchange in climate models.
- Significantly reduces long-standing biases in atmospheric circulation and sea surface temperature patterns in CESM2, improving its fidelity for climate simulations.
Funding
- Not specified in the abstract.
Citation
@article{Shi2025Effects,
author = {Shi, Xiaoming and Li, Qing and Lestari, Diah Valentina and Lin, Shangfei and Su, Hui},
title = {The Effects of Sea‐State‐Dependent Surface Fluxes on CESM2 Climate Simulations},
journal = {Journal of Advances in Modeling Earth Systems},
year = {2025},
doi = {10.1029/2025ms005284},
url = {https://doi.org/10.1029/2025ms005284}
}
Original Source: https://doi.org/10.1029/2025ms005284