中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Touching the classical scaling in penetrative convection

文献类型:期刊论文

作者Ouyang, Zhen1; Wang Q(王淇)2; Li K(李凯)3; Wen, Baole4; Ding ZJ(丁子敬)1,3
刊名PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA
出版日期2025-02-01
卷号122期号:6
关键词penetrative turbulence scaling law coherent rolls Enceladus
ISSN号0027-8424
DOI10.1073/pnas.2418468122
英文摘要The Cassini missions have identified the tiger stripes on Enceladus as the source of both thermal emission and plume jets. The hot spots in the tiger stripes are highly localized, and the plumes suggest active hydrothermal processes within the subglacial ocean of Enceladus. However, understanding the mechanism responsible for the heat anomalies in the tiger stripes remains a challenge. About 60 y ago, geoscientist George Veronis proposed a model for cold water oceans, along with the classical notion of a 1/3 scaling relationship between vertical heat transfer and the Rayleigh number (Ra), a dimensionless number representing the strength of buoyancy driving the convection within the fluid body. In this study, by delving into the steady coherent rolls arising in Veronis' model, we first confirm the existence of the classical scaling as proposed. We identify two distinct pathways, characterized by different flow patterns, that converge to the unified classical scaling. In scenarios where stratification resulting from the density's nonlinear temperature dependence is insignificant, convection rolls with fixed (width-to-height) aspect ratios achieve the classical scaling as Ra approaches infinity. Conversely, under high stratification levels, convection rolls with a heat-transport- maximizing aspect ratio achieve the classical scaling. This investigation also reveals a notable correspondence between optimal coherent rolls and turbulent flow patterns. Based on these coherent rolls, we offer insights into the formation of heat anomalies in the tiger stripes. The predicted heat flux through the ocean and the lateral flow length, are consistent with the measurements obtained by the Cassini spacecraft.
分类号二类/Q1
WOS研究方向Multidisciplinary Sciences ; Science & Technology - Other Topics
语种英语
WOS记录号WOS:001434123200006
资助机构Z.O., K.L., and Z.D. are supported by National Key R&D Program of China (Grant No. 2022YFF0503501) , Z.O. and Z.D. are supported by Investigation into Turbulence Transport in Spheres under Multiphysics Fields (Grant No. KJZ-YY-NLT0604) and the National Natural Science Foundation of China (Grant No. 52176065) and Q.W. is supported by the National Natural Science Foundation of China (Grant No. 42350002) .
其他责任者丁子敬
源URL[http://dspace.imech.ac.cn/handle/311007/101441]  
专题力学研究所_国家微重力实验室
作者单位1.Harbin Institute of Technology;
2.Southern University of Science & Technology;
3.Institute of Mechanics, CAS;
4.New York Institute Technology
推荐引用方式
GB/T 7714
Ouyang, Zhen,Wang Q,Li K,et al. Touching the classical scaling in penetrative convection[J]. PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,2025,122(6).
APA Ouyang, Zhen,王淇,李凯,Wen, Baole,&丁子敬.(2025).Touching the classical scaling in penetrative convection.PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA,122(6).
MLA Ouyang, Zhen,et al."Touching the classical scaling in penetrative convection".PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA 122.6(2025).

入库方式: OAI收割

来源:力学研究所

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