A land model with groundwater lateral flow, water use, and soil freeze-thaw front dynamics

A land model with groundwater lateral flow, water use, and soil freeze-thaw front dynamics
Schematic diagram of the land model CAS-LSM with groundwater lateral flow (GLF), human water use (HWR) and soil freeze-thaw fronts (FTFs). The main calculation process in CAS-LSM and its coupling with GLF, HWR and FTFs: the content in the black dashed box displays the main calculation process in CAS-LSM; the details in the blue dashed box show how the scheme of FTFs is coupled with the soil temperature module; the details in the orange dashed box show how the schemes of GLF and HWR are coupled with the soil hydrology module. Credit: XIE ZHENGHUI

Human water regulation, groundwater lateral flow and the movement of soil frost and thaw fronts affect water and thermal processes, as well as energy and water exchanges between the land surface and atmosphere. Reasonable representation of these processes in land surface models is very important to improving the understanding of terrestrial eco-hydrological processes and land-atmosphere interactions.

Recently, scientists from CAS institute, Xie Zhenghui, Zeng Yujin, Liu Shuang and their co-authors in LASG/Institute of Atmospheric Physics synchronously incorporated the schemes of anthropogenic water regulation, groundwater lateral flow and the movement of soil frost and thaw fronts into a , which is then named the Land Surface Model for Chinese Academy of Sciences (CAS-LSM). Meanwhile, they devised and implemented the schemes describing model resolution conversion between groundwater flow module and the land surface model simulate in parallel the large-scale and high-resolution groundwater flow and its impacts.

Simulations using CAS-LSM were conducted for both Heihe River Basin in China and the globe, respectively, to investigate the impacts of anthropogenic water regulation and groundwater lateral flow on land processes and the response of frozen soil to climate change. Compared with observations, CAS-LSM reproduced the distributions of groundwater, evapotranspiration and permafrost reasonably, and well matched the temporal changes in ground temperature, heat fluxes and soil frost and thaw fronts. The results show that water use raised the latent heat flux and reduced the sensible heat flux, net ecosystem exchange and streamflow recharging to an eco-fragile region, and the active layer thickness increased 8.63 mm/year for permafrost in Heihe River Basin. Global lateral flow significantly modified the equilibrium water table patterns in North Africa, the Arabian Peninsula, central Asia and southern Australia, deepening the water tables by more than 6 m. Results suggested that CAS-LSM is a potential tool for studying land surface processes.

A land model with groundwater lateral flow, water use, and soil freeze-thaw front dynamics
Validations for evapotranspiration, heat flux, groundwater, frozen soil and total water storage. Credit: XIE ZHENGHUi

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More information: Zhenghui Xie et al, A High-Resolution Land Model With Groundwater Lateral Flow, Water Use, and Soil Freeze-Thaw Front Dynamics and its Applications in an Endorheic Basin, Journal of Geophysical Research: Atmospheres (2018). DOI: 10.1029/2018JD028369
Citation: A land model with groundwater lateral flow, water use, and soil freeze-thaw front dynamics (2018, August 13) retrieved 24 June 2019 from https://phys.org/news/2018-08-groundwater-lateral-soil-freeze-thaw-front.html
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