湖冰和冰下层的水温和界面热通量动力学

IF 2.7 4区 环境科学与生态学 Q2 Environmental Science
Jingbo Huo, Xiaohong Shi, Shengnan Zhao, Biao Sun, Guohua Li, Haifeng Yu, Shihuan Wang
{"title":"湖冰和冰下层的水温和界面热通量动力学","authors":"Jingbo Huo, Xiaohong Shi, Shengnan Zhao, Biao Sun, Guohua Li, Haifeng Yu, Shihuan Wang","doi":"10.2166/nh.2023.013","DOIUrl":null,"url":null,"abstract":"\n The purpose of this study is to understand the temperature dynamics of ice and lake water under ice during ice growth. A vertical temperature monitoring system for ice and water under ice was employed for the first time in Wuliangsuhai Lake from 20 December 2016 to 15 March 2017 to obtain continuous monitoring temperature data necessary for calculating the heat flux density at the ice–water interface. During the ice growth period, the ice body temperature and the water body temperature under the ice show an obvious rising trend from the upper layer to the lower layer. As the ice body enters the melting period, the ice temperature and the water temperature under the ice begin to change rapidly. In the presence of snow over the ice, the fluctuations of ice temperature and water temperature under the ice remain stable. According to the experimental data, the analytical equation derived from the Stefan condition is used to calculate the heat flux at the intersection boundary of ice body and water body under ice, which varies from 1.73 to 19.6 W/m2. The dynamic change of ice thickness is significantly influenced by the temperature of ice and water and the heat flux density at the ice–water interface.","PeriodicalId":55040,"journal":{"name":"Hydrology Research","volume":" ","pages":""},"PeriodicalIF":2.7000,"publicationDate":"2023-07-14","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Dynamics of water temperature and interfacial heat flux in lake ice and under-ice layers\",\"authors\":\"Jingbo Huo, Xiaohong Shi, Shengnan Zhao, Biao Sun, Guohua Li, Haifeng Yu, Shihuan Wang\",\"doi\":\"10.2166/nh.2023.013\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"\\n The purpose of this study is to understand the temperature dynamics of ice and lake water under ice during ice growth. A vertical temperature monitoring system for ice and water under ice was employed for the first time in Wuliangsuhai Lake from 20 December 2016 to 15 March 2017 to obtain continuous monitoring temperature data necessary for calculating the heat flux density at the ice–water interface. During the ice growth period, the ice body temperature and the water body temperature under the ice show an obvious rising trend from the upper layer to the lower layer. As the ice body enters the melting period, the ice temperature and the water temperature under the ice begin to change rapidly. In the presence of snow over the ice, the fluctuations of ice temperature and water temperature under the ice remain stable. According to the experimental data, the analytical equation derived from the Stefan condition is used to calculate the heat flux at the intersection boundary of ice body and water body under ice, which varies from 1.73 to 19.6 W/m2. The dynamic change of ice thickness is significantly influenced by the temperature of ice and water and the heat flux density at the ice–water interface.\",\"PeriodicalId\":55040,\"journal\":{\"name\":\"Hydrology Research\",\"volume\":\" \",\"pages\":\"\"},\"PeriodicalIF\":2.7000,\"publicationDate\":\"2023-07-14\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Hydrology Research\",\"FirstCategoryId\":\"93\",\"ListUrlMain\":\"https://doi.org/10.2166/nh.2023.013\",\"RegionNum\":4,\"RegionCategory\":\"环境科学与生态学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"Environmental Science\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrology Research","FirstCategoryId":"93","ListUrlMain":"https://doi.org/10.2166/nh.2023.013","RegionNum":4,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"Environmental Science","Score":null,"Total":0}
引用次数: 0

摘要

本研究的目的是了解冰生长过程中冰和冰下湖水的温度动态。2016年12月20日至2017年3月15日,在乌梁素海首次采用冰下冰和水的垂直温度监测系统,以获得计算冰-水界面热通量密度所需的连续监测温度数据。在冰生长期,冰体温度和冰下水体温度从上层向下层呈明显上升趋势。随着冰体进入融化期,冰的温度和冰下的水温开始迅速变化。在冰上有雪的情况下,冰温度和冰下水温的波动保持稳定。根据实验数据,利用Stefan条件导出的解析方程计算了冰下水体与冰体相交边界处的热通量,其变化范围为1.73~19.6W/m2。冰厚度的动态变化受到冰和水的温度以及冰-水界面处的热通量密度的显著影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dynamics of water temperature and interfacial heat flux in lake ice and under-ice layers
The purpose of this study is to understand the temperature dynamics of ice and lake water under ice during ice growth. A vertical temperature monitoring system for ice and water under ice was employed for the first time in Wuliangsuhai Lake from 20 December 2016 to 15 March 2017 to obtain continuous monitoring temperature data necessary for calculating the heat flux density at the ice–water interface. During the ice growth period, the ice body temperature and the water body temperature under the ice show an obvious rising trend from the upper layer to the lower layer. As the ice body enters the melting period, the ice temperature and the water temperature under the ice begin to change rapidly. In the presence of snow over the ice, the fluctuations of ice temperature and water temperature under the ice remain stable. According to the experimental data, the analytical equation derived from the Stefan condition is used to calculate the heat flux at the intersection boundary of ice body and water body under ice, which varies from 1.73 to 19.6 W/m2. The dynamic change of ice thickness is significantly influenced by the temperature of ice and water and the heat flux density at the ice–water interface.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Hydrology Research
Hydrology Research Environmental Science-Water Science and Technology
CiteScore
5.30
自引率
7.40%
发文量
70
审稿时长
17 weeks
期刊介绍: Hydrology Research provides international coverage on all aspects of hydrology in its widest sense, and welcomes the submission of papers from across the subject. While emphasis is placed on studies of the hydrological cycle, the Journal also covers the physics and chemistry of water. Hydrology Research is intended to be a link between basic hydrological research and the practical application of scientific results within the broad field of water management.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信