HydroThermal Dynamics of Frozen Soils on the Tibetan Plateau during 2015-2016
Datacite citation style:
Yu, Lianyu; Zeng, Y. (Yijian); Su, Z. (Bob); Wen, J. (Jun) (2018): HydroThermal Dynamics of Frozen Soils on the Tibetan Plateau during 2015-2016. Version 1. 4TU.ResearchData. dataset. https://doi.org/10.4121/uuid:cc69b7f2-2448-4379-b638-09327012ce9b
Other citation styles (APA, Harvard, MLA, Vancouver, Chicago, IEEE) available at Datacite
Dataset
The hydrothermal dynamics of frozen soil were monitored at a typical meadow ecosystem on the Tibetan Plateau. Soil temperature/moisture profiles were automatically measured at a 30-min. interval by 5TM ECH2O probes (Decagon Devices, Inc., USA) installed at the following depths: 5 cm, 10 cm, 20 cm, 40cm, and 80 cm. The turbulent heat fluxes were measured by an eddy-covariance (EC) system (LI-COR 7500, Campbell Scientific). STEMMUS-FT (Simultaneous Transfer of Energy, Mass and Momentum in Unsaturated Soil with Freeze-Thaw process) model, with two control experiments (Ctrl1 for Van Genuchten hydraulic scheme and Ctrl2 for Clapp and Hornberger hydraulic scheme), was employed to reproduce the simultaneous movement of soil moisture and heat flow in the frozen soil. With the aid of physically based STEMMUS-FT model and in situ measurements, we can investigate the underlying mechanisms of the water and heat transfer in frozen soils.
history
- 2018-06-21 first online, published, posted
publisher
University of Twente
format
media types: application/vnd.openxmlformats-officedocument.spreadsheetml.sheet, text/plain
references
organizations
University of Twente, Faculty of Geo-Information Science and Earth Observation, Department of Water Resources
DATA
files (2)
- 2,271 bytesMD5:
db24db5a46e6618924ac4c8c8c40e351
README.txt - 1,340,680 bytesMD5:
96d815044f4d00f4ebd3a945f9e1df7f
HydroThermalDynamicsDataFrozenSoilsMaquTPMeasuredIn2015-2016.xlsx -
download all files (zip)
1,342,951 bytes unzipped