Xiao Bai

Dr. Xiao Bai

orcid

Research Focus & Metrics

Academic Career Length

11Years (2016-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

View All Publications
1 June 2020 in Journal of Hydrology
Verified
Journal Article
Closed access
XBXiao Bai
Xiao Bai
XJXiaoxu Jia
Xiaoxu Jia
YJYuhua Jia
Yuhua Jia
MSMing'An Shao
Ming'An Shao
WHWei Hu
Wei Hu

1 November 2016 in Agricultural Water Management
Verified
Journal Article
Closed access
YJYiwen Jiang
Yiwen Jiang
LZLanhui Zhang
Lanhui Zhang
BZBaoqing Zhang
Baoqing Zhang
CHChansheng He
Chansheng He
XJXin Jin
Xin Jin
XBXiao Bai
Xiao Bai

1 October 2021 in Agriculture, Ecosystems & Environment
Verified
Journal Article
Closed access
XBXiao Bai
Xiao Bai
XJXiaoxu Jia
Xiaoxu Jia
CZChunlei Zhao
Chunlei Zhao
MSMing’aN Shao
Ming’aN Shao

1 March 2022 in CATENA
Verified
Journal Article
Closed access
XBXiao Bai
Xiao Bai
MSMing'AN Shao
Ming'AN Shao
XJXiaoxu Jia
Xiaoxu Jia
CZChunlei Zhao
Chunlei Zhao

28 July 2020 in Remote Sensing
Verified
Journal Article
Open access
PDF file
XBXiao Bai
Xiao Bai
LZLanhui Zhang
Lanhui Zhang
Chansheng HeChansheng He
Chansheng He
YZYi Zhu
Yi Zhu
Temporal and spatial variability of soil moisture has an important impact on hydrological processes in mountainous areas. Understanding such variability requires soil moisture datasets at multiple temporal and spatial scales. Remote sensing is a very effective method to obtain surface (~5 cm depth) soil moisture at the regional scale but cannot directly measure soil moisture at deep soil layers (>5 cm depth) currently. This study chose the upstream of the Heihe River Watershed in the Qilian Mountain Ranges in Northwest China as the study area to estimate the profile soil moisture (0–70 cm depth) at the regional scale using satellite Vegetation Index (NDVI) and Land Surface Temperature (LST) products. The study area was divided into 31 zones according to the combination of altitude, vegetation and soil type. Long-term in situ soil moisture observation stations were set up at each of the zones. Soil moisture probe, ECH2O, was used to collect soil moisture at five layers (0–10, 10–20, 20–30, 30–50 and 50–70 cm) continuously. Multiple linear regression equations of time series MODIS (Moderate-resolution Imaging Spectroradiometer) NDVI, LST and soil moisture were developed for each of the five soil layers at the 31 zones to estimate the soil moisture (0–70 cm) on a regional scale with a spatial resolution of 1 km2 and a temporal resolution of 16-d from October, 2013 to September, 2016. The correlation coefficient R of the regression equations was between 0.47 and 0.94, the RMSE was 0.03, indicating that the estimation method based on the MODIS NDVI and LST data was suitable and could be applied to alpine mountainous areas with complex topography, soil and vegetation types. The overall pattern of soil moisture spatial distribution indicated that soil moisture was higher in the eastern region than in the western region, and the soil moisture content in the whole study area was 14.5%. The algorithm and results provide novel applications of remote sensing to support soil moisture data acquisition and hydrological research in mountainous areas.

19 December 2023 in Agriculture, Ecosystems & Environment
Verified
Journal Article
Closed access
XJXiaoxu Jia
Xiaoxu Jia
XBXiao Bai
Xiao Bai
CLChenggong Liu
Chenggong Liu
CZChunlei Zhao
Chunlei Zhao
MSMing’aN Shao
Ming’aN Shao
YPYanhui Pan
Yanhui Pan