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Understanding the Way Machines Simulate Hydrological Processes-A Case Study of Predicting Fine-Scale Watershed Response on a Distributed Framework

Authors
Kim, DongkyunLee, Yong OhJun, ChanghyunKang, Seokkoo
Issue Date
Jun-2023
Publisher
IEEE-INST ELECTRICAL ELECTRONICS ENGINEERS INC
Keywords
Deep learning; distributed hydrologic model; hydrology; long short-term memory (LSTM); machine learning; radar precipitation
Citation
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING, v.61, pp.1 - 18
Indexed
SCIE
SCOPUS
Journal Title
IEEE TRANSACTIONS ON GEOSCIENCE AND REMOTE SENSING
Volume
61
Start Page
1
End Page
18
URI
https://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/189423
DOI
10.1109/TGRS.2023.3285540
ISSN
0196-2892
Abstract
This study developed a deep neural network (DNN)-based distributed hydrologic model for an urban watershed in the Republic of Korea. The developed model is composed of multiple long short-term memory (LSTM) hidden units connected by a fully connected layer. To examine the study area using the developed model, time series of 10-min radar-gauge composite precipitation data and 10-min temperature data at 239 model grid cells with 1-km resolution is used as inputs to simulate 10-min watershed flow discharge as an output. The model performed well for the calibration period (2013-2016) and the validation period (2017-2019), with Nash-Sutcliffe efficiency coefficient values being 0.99 and 0.67, respectively. Further in-depth analyses were performed to derive the following conclusions: 1) the map of runoff-precipitation ratios produced using the developed DNN model resembled imperviousness ratio map of the study area from the land cover data, revealing that the DNN successfully deep-learned the precipitation partitioning processes only with the input and output data without depending on any priori information about hydrology; 2) the model successfully reproduced the soil moisture-dependent runoff process, an essential prerequisite of continuous hydrologic models; and 3) each LSTM unit has a different temporal sensitivity to the precipitation stimulus, with fast-response LSTM units having greater output weight factors near the watershed outlet, which implies that the developed model has a mechanism to separately consider the hydrological components with distinct response time such as direct runoff and the groundwater-driven baseflow.
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COLLEGE OF ENGINEERING (DEPARTMENT OF CIVIL AND ENVIRONMENTAL ENGINEERING)
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