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DOI | 10.1175/JCLI-D-20-0163.1 |
The impact of warm and moist airmass perturbations on arctic mixed-phase stratocumulus | |
Eirund G.K.; Possner A.; Lohmann U. | |
发表日期 | 2020 |
ISSN | 0894-8755 |
起始页码 | 9615 |
结束页码 | 9628 |
卷号 | 33期号:22 |
英文摘要 | The Arctic is known to be particularly sensitive to climate change. This Arctic amplification has partially been attributed to poleward atmospheric heat transport in the form of airmass intrusions. Locally, such airmass intrusions can introduce moisture and temperature perturbations. The effect of airmass perturbations on boundary layer and cloud changes and their impact on the surface radiative balance has received increased attention, especially over sea ice with regard to sea ice melt. Utilizing cloud-resolving model simulations, this study addresses the impact of airmass perturbations occurring at different altitudes on stratocumulus clouds for open-ocean conditions. It is shown that warm and moist airmass perturbations substantially affect the boundary layer and cloud properties, even for the relatively moist environmental conditions over the open ocean. The cloud response is driven by temperature inversion adjustments and strongly depends on the perturbation height. Boundary layer perturbations weaken and raise the inversion, which destabilizes the lower troposphere and involves a transition from stratocumulus to cumulus clouds. In contrast, perturbations occurring in the lower free troposphere lead to a lowering but strengthening of the temperature inversion, with no impact on cloud fraction. In simulations where free-tropospheric specific humidity is further increased, multilayer mixed-phase clouds form. Regarding energy balance changes, substantial surface longwave cooling arises out of the stratocumulus break-up simulated for boundary layer perturbations. Meanwhile, the net surface longwave warming increases resulting from thicker clouds for airmass perturbations occurring in the lower free troposphere. © 2020 American Meteorological Society. |
英文关键词 | Atmospheric humidity; Atmospheric movements; Atmospheric temperature; Climate change; Clouds; Sea ice; Troposphere; Cloud-resolving model simulations; Environmental conditions; Lower troposphere; Mixed-phase cloud; Specific humidity; Stratocumulus clouds; Temperature inversions; Temperature perturbations; Boundary layers; air mass; altitude; climate modeling; open ocean; perturbation; radiative transfer; stratocumulus; temperature inversion; Arctic |
语种 | 英语 |
来源期刊 | Journal of Climate
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/171015 |
作者单位 | Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland; Institute for Atmospheric and Environmental Sciences, Goethe-University Frankfurt, Frankfurt, Germany; Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland |
推荐引用方式 GB/T 7714 | Eirund G.K.,Possner A.,Lohmann U.. The impact of warm and moist airmass perturbations on arctic mixed-phase stratocumulus[J],2020,33(22). |
APA | Eirund G.K.,Possner A.,&Lohmann U..(2020).The impact of warm and moist airmass perturbations on arctic mixed-phase stratocumulus.Journal of Climate,33(22). |
MLA | Eirund G.K.,et al."The impact of warm and moist airmass perturbations on arctic mixed-phase stratocumulus".Journal of Climate 33.22(2020). |
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