Identifying Spatiotemporal Patterns of Hillslope Subsurface Flow in an Alpine Critical Zone on the Qinghai‐Tibetan Plateau Based on Three‐Year, High‐Resolution Field Observations-Reference-Cited by-同舟云学术

Identifying Spatiotemporal Patterns of Hillslope Subsurface Flow in an Alpine Critical Zone on the Qinghai‐Tibetan Plateau Based on Three‐Year, High‐Resolution Field Observations

Published:2022-11 Issue:11 Volume:58 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resources Research

Author:

Hu Guangrong¹²³,Li Xiaoyan¹²⁴⁵^ORCID,Yang Xiaofan¹²^ORCID,Shi Fangzhong¹²,Sun Haoran¹²,Cui Baoshan³⁶

Affiliation:

1. Zhuhai Branch of State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science Beijing Normal University Zhuhai China

2. School of Natural Resources Faculty of Geographical Science Beijing Normal University Beijing China

3. Research and Development Center for Watershed Environmental EcoEngineering, Advanced Institute of Natural Science Beijing Normal University Zhuhai China

4. Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation Ministry of Education Qinghai Normal University Xining China

5. Academy of Plateau Science and Sustainability Qinghai Normal University Xining China

6. State Key Joint Laboratory of Environmental Simulation and Pollution Control School of Environment Beijing Normal University Beijing China

Funder

National Natural Science Foundation of China

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022WR032098

Reference59 articles.

1. Rock damage and regolith transport by frost: an example of climate modulation of the geomorphology of the critical zone

2. The evolving perceptual model of streamflow generation at the Panola Mountain Research Watershed

3. Slope, aspect and climate: Spatially explicit and implicit models of topographic microclimate in chalk grassland

4. Repeated Subsurface Thermal Profiling to Reveal Temporal Variability in Deep Groundwater Flow Conditions

5. From hillslope to stream: methods to investigate subsurface connectivity

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