Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulations

<p>Ice clouds play an important role in the atmospheric radiation budget, both by reflecting shortwave radiation and by absorbing or emitting longwave radiation. These effects can modulate the cloud radiative heating (CRH) rate, which in turn influences circulation and precipitation. Ice cloud...

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Main Authors: E. I. Sepulveda Araya, S. C. Sullivan, A. Voigt
Format: Article
Language:English
Published: Copernicus Publications 2025-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/25/8943/2025/acp-25-8943-2025.pdf
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author E. I. Sepulveda Araya
S. C. Sullivan
S. C. Sullivan
A. Voigt
author_facet E. I. Sepulveda Araya
S. C. Sullivan
S. C. Sullivan
A. Voigt
author_sort E. I. Sepulveda Araya
collection DOAJ
description <p>Ice clouds play an important role in the atmospheric radiation budget, both by reflecting shortwave radiation and by absorbing or emitting longwave radiation. These effects can modulate the cloud radiative heating (CRH) rate, which in turn influences circulation and precipitation. Ice cloud radiative properties depend on the size, shape (or habit), and complexity, including surface roughness or hollowness, of in-cloud ice crystals. To better predict ice cloud radiative effects, there has been a continuous effort to account for more ice crystal habits and complexity in current radiative transfer calculations. Here, we conduct a series of idealized single-column radiative transfer calculations to study how ice CRH responds to including ice crystal complexity. We evaluate four ice optical schemes for a range of ice cloud formation temperatures or altitudes, geometrical depths, ice water paths (IWPs), and ice crystal effective radii. In addition, we present a heating rate sensitivity matrix as a condensed visualization of the CRH response across a broad parameter space. We find that including ice complexity in cold thin clouds with high IWPs can diminish the net in-cloud heating and cloud-top cooling by 2.5 and 15 K d<span class="inline-formula"><sup>−1</sup></span>, respectively. Furthermore, while temperature-based schemes behave similarly to other schemes at warmer temperatures, they predict net CRH at the cloud bottom more than 10 K d<span class="inline-formula"><sup>−1</sup></span> higher than size-dependent schemes at the coldest temperatures. Either weakening of CRH by ice complexity or strengthening by temperature-dependent schemes can alter anvil cloud lifetime and evolution, as well as large-scale atmospheric circulation.</p>
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spelling doaj-art-8fb6f95e52ab45ee83a82b47e88f0abc2025-08-20T04:01:58ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242025-08-01258943895810.5194/acp-25-8943-2025Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulationsE. I. Sepulveda Araya0S. C. Sullivan1S. C. Sullivan2A. Voigt3Department of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ 85721, USADepartment of Chemical and Environmental Engineering, University of Arizona, Tucson, AZ 85721, USADepartment of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ 85721, USADepartment of Meteorology and Geophysics, University of Vienna, 1090 Vienna, Austria<p>Ice clouds play an important role in the atmospheric radiation budget, both by reflecting shortwave radiation and by absorbing or emitting longwave radiation. These effects can modulate the cloud radiative heating (CRH) rate, which in turn influences circulation and precipitation. Ice cloud radiative properties depend on the size, shape (or habit), and complexity, including surface roughness or hollowness, of in-cloud ice crystals. To better predict ice cloud radiative effects, there has been a continuous effort to account for more ice crystal habits and complexity in current radiative transfer calculations. Here, we conduct a series of idealized single-column radiative transfer calculations to study how ice CRH responds to including ice crystal complexity. We evaluate four ice optical schemes for a range of ice cloud formation temperatures or altitudes, geometrical depths, ice water paths (IWPs), and ice crystal effective radii. In addition, we present a heating rate sensitivity matrix as a condensed visualization of the CRH response across a broad parameter space. We find that including ice complexity in cold thin clouds with high IWPs can diminish the net in-cloud heating and cloud-top cooling by 2.5 and 15 K d<span class="inline-formula"><sup>−1</sup></span>, respectively. Furthermore, while temperature-based schemes behave similarly to other schemes at warmer temperatures, they predict net CRH at the cloud bottom more than 10 K d<span class="inline-formula"><sup>−1</sup></span> higher than size-dependent schemes at the coldest temperatures. Either weakening of CRH by ice complexity or strengthening by temperature-dependent schemes can alter anvil cloud lifetime and evolution, as well as large-scale atmospheric circulation.</p>https://acp.copernicus.org/articles/25/8943/2025/acp-25-8943-2025.pdf
spellingShingle E. I. Sepulveda Araya
S. C. Sullivan
S. C. Sullivan
A. Voigt
Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulations
Atmospheric Chemistry and Physics
title Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulations
title_full Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulations
title_fullStr Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulations
title_full_unstemmed Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulations
title_short Ice crystal complexity leads to weaker ice cloud radiative heating in idealized single-column simulations
title_sort ice crystal complexity leads to weaker ice cloud radiative heating in idealized single column simulations
url https://acp.copernicus.org/articles/25/8943/2025/acp-25-8943-2025.pdf
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AT avoigt icecrystalcomplexityleadstoweakericecloudradiativeheatinginidealizedsinglecolumnsimulations