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Title: Intercomparison of the Cloud Water Phase among Global Climate Models

Abstract

Mixed-phase clouds (clouds that consist of both cloud droplets and ice crystals) are frequently present in the Earth’s atmosphere and influence the Earth’s energy budget through their radiative properties, which are highly dependent on the cloud water phase. In this study, the phase partitioning of cloud water is compared among six global climate models (GCMs) and with Cloud and Aerosol Lidar with Orthogonal Polarization retrievals. It is found that the GCMs predict vastly different distributions of cloud phase for a given temperature, and none of them are capable of reproducing the spatial distribution or magnitude of the observed phase partitioning. While some GCMs produced liquid water paths comparable to satellite observations, they all failed to preserve sufficient liquid water at mixed-phase cloud temperatures. Our results suggest that validating GCMs using only the vertically integrated water contents could lead to amplified differences in cloud radiative feedback. The sensitivity of the simulated cloud phase in GCMs to the choice of heterogeneous ice nucleation parameterization is also investigated. The response to a change in ice nucleation is quite different for each GCM, and the implementation of the same ice nucleation parameterization in all models does not reduce the spread in simulated phase amongmore » GCMs. The results suggest that processes subsequent to ice nucleation are at least as important in determining phase and should be the focus of future studies aimed at understanding and reducing differences among the models.« less

Authors:
; ; ; ; ; ; ; ;
Publication Date:
Research Org.:
Pacific Northwest National Lab. (PNNL), Richland, WA (United States)
Sponsoring Org.:
USDOE
OSTI Identifier:
1158984
Report Number(s):
PNNL-SA-103695
KP1703020
DOE Contract Number:  
AC05-76RL01830
Resource Type:
Journal Article
Journal Name:
Journal of Geophysical Research. D. (Atmospheres), 119(6):3372–3400
Additional Journal Information:
Journal Name: Journal of Geophysical Research. D. (Atmospheres), 119(6):3372–3400
Country of Publication:
United States
Language:
English
Subject:
intercomparison; cloud water phase; global climate models

Citation Formats

Komurcu, Muge, Storelvmo, Trude, Tan, Ivy, Lohmann, U., Yun, Yuxing, Penner, Joyce E., Wang, Yong, Liu, Xiaohong, and Takemura, T. Intercomparison of the Cloud Water Phase among Global Climate Models. United States: N. p., 2014. Web. doi:10.1002/2013JD021119.
Komurcu, Muge, Storelvmo, Trude, Tan, Ivy, Lohmann, U., Yun, Yuxing, Penner, Joyce E., Wang, Yong, Liu, Xiaohong, & Takemura, T. Intercomparison of the Cloud Water Phase among Global Climate Models. United States. https://doi.org/10.1002/2013JD021119
Komurcu, Muge, Storelvmo, Trude, Tan, Ivy, Lohmann, U., Yun, Yuxing, Penner, Joyce E., Wang, Yong, Liu, Xiaohong, and Takemura, T. 2014. "Intercomparison of the Cloud Water Phase among Global Climate Models". United States. https://doi.org/10.1002/2013JD021119.
@article{osti_1158984,
title = {Intercomparison of the Cloud Water Phase among Global Climate Models},
author = {Komurcu, Muge and Storelvmo, Trude and Tan, Ivy and Lohmann, U. and Yun, Yuxing and Penner, Joyce E. and Wang, Yong and Liu, Xiaohong and Takemura, T.},
abstractNote = {Mixed-phase clouds (clouds that consist of both cloud droplets and ice crystals) are frequently present in the Earth’s atmosphere and influence the Earth’s energy budget through their radiative properties, which are highly dependent on the cloud water phase. In this study, the phase partitioning of cloud water is compared among six global climate models (GCMs) and with Cloud and Aerosol Lidar with Orthogonal Polarization retrievals. It is found that the GCMs predict vastly different distributions of cloud phase for a given temperature, and none of them are capable of reproducing the spatial distribution or magnitude of the observed phase partitioning. While some GCMs produced liquid water paths comparable to satellite observations, they all failed to preserve sufficient liquid water at mixed-phase cloud temperatures. Our results suggest that validating GCMs using only the vertically integrated water contents could lead to amplified differences in cloud radiative feedback. The sensitivity of the simulated cloud phase in GCMs to the choice of heterogeneous ice nucleation parameterization is also investigated. The response to a change in ice nucleation is quite different for each GCM, and the implementation of the same ice nucleation parameterization in all models does not reduce the spread in simulated phase among GCMs. The results suggest that processes subsequent to ice nucleation are at least as important in determining phase and should be the focus of future studies aimed at understanding and reducing differences among the models.},
doi = {10.1002/2013JD021119},
url = {https://www.osti.gov/biblio/1158984}, journal = {Journal of Geophysical Research. D. (Atmospheres), 119(6):3372–3400},
number = ,
volume = ,
place = {United States},
year = {Thu Mar 27 00:00:00 EDT 2014},
month = {Thu Mar 27 00:00:00 EDT 2014}
}