Water and heat coupling processes and its simulation in frozen soils: Current status and future research directions

IF 6.6 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Catena Pub Date : 2023-03-01 Epub Date: 2022-12-21 DOI:10.1016/j.catena.2022.106844
Guojie Hu , Lin Zhao , Ren Li , Hotaek Park , Xiaodong Wu , Youqi Su , Georg Guggenberger , Tonghua Wu , Defu Zou , Xiaofan Zhu , Wenxin Zhang , Yifan Wu , Junming Hao
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引用次数: 2

Abstract

To date, most studies on coupled-water-and-heat processes in frozen soils haves focused on the mechanism of changes in frozen soil and the contribution of climate change, hydrological processes, and ecosystems in cold regions. Several studies have demonstrated considerable improvements in the accuracy of simulating water and heat transfer processes in cold regions. However, substantial differences remain among the different models and parameterizations because of the lack of observations and in-depth understanding of the water and heat transfer processes. Hence, it is necessary to summarize recent advances in the simulation of water-and-heat-coupling processes and challenges for further research. Therefore, we present a theory-focused summary of progress in this field considering the aspects of water flow and coupled-water-and-heat transfer. The simulation progress is discussed in terms of physical process models; one type of model only considers the heat conduction transfer processes without water flow, and the other considers coupled-water-and-heat transfer processes. Aspects of model deficiencies related to non-conductive heat transfer and soil water transfer processes in the frozen soil are also summarized. Moreover, the major parameterizations are reviewed, including phase changes, freeze–thaw fronts, thermal conductivity, hydraulic conductivity, snow processes, surface parameterization schemes, ground ice, and lower boundary conditions. While models and parameterizations can suitably capture local-scale water and heat transfer processes in frozen soil, their applications are spatiotemporally constrained, requiring further improvement. We provide a theoretical basis for further studying water and heat transfer processes in frozen soil and suggest that future research should enhance the accuracy of frozen soil parameterization and improve the understanding of the coupling of water and heat transfer processes based on improved observation techniques and high-resolution data.

冻土水热耦合过程及其模拟:现状与未来研究方向
迄今为止,大多数关于冻土水热耦合过程的研究都集中在冻土变化的机制以及气候变化、水文过程和寒冷地区生态系统的贡献上。几项研究表明,在寒冷地区模拟水和热传递过程的准确性有了显著提高。然而,由于缺乏对水和热传递过程的观察和深入了解,不同的模型和参数化之间仍然存在很大差异。因此,有必要总结水热耦合过程模拟的最新进展和进一步研究的挑战。因此,考虑到水流和水与热的耦合传递,我们对该领域的进展进行了理论上的总结。从物理过程模型的角度讨论了模拟的进展;一种模型只考虑了无水流的热传导过程,另一种模型考虑了水与热的耦合过程。还总结了与冻土中非传导传热和土壤水分传递过程有关的模型缺陷。此外,还回顾了主要的参数化,包括相变、冻融锋、热导率、导水率、雪过程、表面参数化方案、地面冰和下边界条件。虽然模型和参数化可以适当地捕捉冻土中的局部尺度水和热传递过程,但它们的应用受到时空限制,需要进一步改进。我们为进一步研究冻土中的水热传递过程提供了理论基础,并建议未来的研究应基于改进的观测技术和高分辨率数据,提高冻土参数化的准确性,提高对水热传递耦合过程的理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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