Convective heat transfer of spring meltwater accelerates active layer phase change in Tibet permafrost areas

Yi Zhao,Zhuotong Nan,Lin Zhao,Hailong Ji

doi:10.5194/tc-16-825-2022

Abstract

Abstract. Convective heat transfer (CHT) is one of the important processes that control the near-ground surface heat transfer in permafrost areas. However, this process has often not been considered in most permafrost studies, and its influence on freezing–thawing processes in the active layer lacks quantitative investigation. The Simultaneous Heat and Water (SHAW) model, one of the few land surface models in which the CHT process is well incorporated into the soil heat–mass transport processes, was applied in this study to investigate the impacts of CHT on the thermal dynamics of the active layer at the Tanggula station, a typical permafrost site on the eastern Qinghai–Tibet Plateau with abundant meteorological and soil temperature and soil moisture observation data. A control experiment was carried out to quantify the changes in active layer temperature affected by vertical advection of liquid water. Three experimental setups were used: (1) the original SHAW model with full consideration of CHT, (2) a modified SHAW model that ignores CHT due to infiltration from the surface, and (3) a modified SHAW model that completely ignores CHT processes in the system. The results show that the CHT events occurred mainly during thaw periods in melted shallow (0–0.2 m) and intermediate (0.4–1.3 m) soil depths, and their impacts on soil temperature at shallow depths were significantly greater during spring melting periods than summer. The impact was minimal during freeze periods and in deep soil layers. During thaw periods, temperatures at the shallow and intermediate soil depths simulated under the scenario considering CHT were on average about 0.9 and 0.4 ∘C higher, respectively, than under the scenarios ignoring CHT. The ending dates of the zero-curtain effect were substantially advanced when CHT was considered due to its heating effect. However, the opposite cooling effect was also present but not as frequently as heating due to upward liquid fluxes and thermal differences between soil layers. In some periods, the advection flow from the cold layer reduced the shallow and intermediate depth temperatures by an average of about −1.0 and −0.4 ∘C, respectively. The overall annual effect of CHT due to liquid flux is to increase soil temperature in the active layer and favor thawing of frozen ground at the study site.

Highlights

Permafrost is defined as the ground that remains frozen consecutively for more than 2 years (Zhao et al, 2010) and is mainly distributed at high latitudes and cold alpine areas, such as the Antarctic, Arctic, and Qinghai–Tibet Plateau (QTP) (Zhang et al, 1999)
In the Simultaneous Heat and Water (SHAW) model, we found that the simulated direction of vapor flux did not match well the real vapor cycle, so the convection associated with the vapor remained intact in the three setups to exclude the impacts of vapor convective heat transfer (CHT) in this analysis
By contrasting Control–No surface CHT (NoSurf) with Control–NoConv, we found many cooling events occurring at intermediate depths (0.4–1.3 m) within the soils and associated with upward water migration driven by the hydraulic gradient, resulting in higher simulated soil temperature simulated in NoConv than in Control

Summary

Introduction

Permafrost is defined as the ground that remains frozen consecutively for more than 2 years (Zhao et al, 2010) and is mainly distributed at high latitudes and cold alpine areas, such as the Antarctic, Arctic, and Qinghai–Tibet Plateau (QTP) (Zhang et al, 1999). Y. Zhao et al.: Convective heat transfer of spring meltwater the thermal and hydrological processes in the soil in frozen ground regions. During spring snowmelt and summer rainfall, a rapid temperature increase of about 2 to 4 ◦C is observed in the uppermost soil layer, indicating a heating effect of liquid CHT (Hinkel et al, 1996, 1997; Kane et al, 1991). Residual water convection could ensue, and the CHT of liquid water is relatively modest but still works because the freezing process occurring in the active layer increases the pore fluid density and van der Waals forces on the ice particles surface (Fisher et al, 2020; Kane and Stein, 1983)

Methods

Results

Discussion

Conclusion