TY - JOUR
T1 - Continuously sensing of water temperature in a lake using acoustic tomography method
AU - Huang, Haocai
AU - Xie, Xinyi
AU - Xu, Shijie
AU - Guo, Yong
AU - Liu, Shuo
AU - Zhu, Min
AU - Hu, Zhengliang
AU - Xu, Pan
AU - Li, Guangming
N1 - Publisher Copyright:
© 2021 Informa UK Limited, trading as Taylor & Francis Group.
PY - 2022
Y1 - 2022
N2 - Continuously sensing of water temperature is of critical importance to water environment, fluid dynamic and water resources researches. Coastal acoustic tomography (CAT) is a remote sensing technique in spatial temperature distribution estimating and has been widely used in many coastal regions. Continuous observations of water temperature in small-scale waters with distance less than 1 km are seldom conducted, as it is difficult to get high-resolution observation results. Here, a horizontal temperature field within 300 m distance was mapped in a sound transmission experiment with three 50 kHz CAT systems. The maximum inversion error temperature for the horizontal temperature field was 0.09°C. The root-mean-square error between the CAT-observed and range-averaged temperature that were calculated from one-way travel time data along three transmission paths were 0.03°C, 0.028°C and 0.043°C, respectively. The obtained results confirmed that CAT can be used in recovering the horizontal distributions of water temperature fields in lake.
AB - Continuously sensing of water temperature is of critical importance to water environment, fluid dynamic and water resources researches. Coastal acoustic tomography (CAT) is a remote sensing technique in spatial temperature distribution estimating and has been widely used in many coastal regions. Continuous observations of water temperature in small-scale waters with distance less than 1 km are seldom conducted, as it is difficult to get high-resolution observation results. Here, a horizontal temperature field within 300 m distance was mapped in a sound transmission experiment with three 50 kHz CAT systems. The maximum inversion error temperature for the horizontal temperature field was 0.09°C. The root-mean-square error between the CAT-observed and range-averaged temperature that were calculated from one-way travel time data along three transmission paths were 0.03°C, 0.028°C and 0.043°C, respectively. The obtained results confirmed that CAT can be used in recovering the horizontal distributions of water temperature fields in lake.
UR - http://www.scopus.com/inward/record.url?scp=85121723196&partnerID=8YFLogxK
U2 - 10.1080/2150704X.2021.2017506
DO - 10.1080/2150704X.2021.2017506
M3 - Article
AN - SCOPUS:85121723196
SN - 2150-704X
VL - 13
SP - 219
EP - 225
JO - Remote Sensing Letters
JF - Remote Sensing Letters
IS - 3
ER -