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

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dc.contributor.authorKim, Dongkyun-
dc.contributor.authorLee, Yong Oh-
dc.contributor.authorJun, Changhyun-
dc.contributor.authorKang, Seokkoo-
dc.date.accessioned2023-08-22T03:00:45Z-
dc.date.available2023-08-22T03:00:45Z-
dc.date.issued2023-06-
dc.identifier.issn0196-2892-
dc.identifier.issn1558-0644-
dc.identifier.urihttps://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/189423-
dc.description.abstractThis 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.-
dc.format.extent18-
dc.language영어-
dc.language.isoENG-
dc.publisherInstitute of Electrical and Electronics Engineers-
dc.titleUnderstanding the Way Machines Simulate Hydrological Processes-A Case Study of Predicting Fine-Scale Watershed Response on a Distributed Framework-
dc.typeArticle-
dc.publisher.location미국-
dc.identifier.doi10.1109/TGRS.2023.3285540-
dc.identifier.scopusid2-s2.0-85162692212-
dc.identifier.wosid001022708100003-
dc.identifier.bibliographicCitationIEEE Transactions on Geoscience and Remote Sensing, v.61, pp 1 - 18-
dc.citation.titleIEEE Transactions on Geoscience and Remote Sensing-
dc.citation.volume61-
dc.citation.startPage1-
dc.citation.endPage18-
dc.type.docTypeArticle-
dc.description.isOpenAccessN-
dc.description.journalRegisteredClassscie-
dc.description.journalRegisteredClassscopus-
dc.relation.journalResearchAreaGeochemistry & Geophysics-
dc.relation.journalResearchAreaEngineering-
dc.relation.journalResearchAreaRemote Sensing-
dc.relation.journalResearchAreaImaging Science & Photographic Technology-
dc.relation.journalWebOfScienceCategoryGeochemistry & Geophysics-
dc.relation.journalWebOfScienceCategoryEngineering, Electrical & Electronic-
dc.relation.journalWebOfScienceCategoryRemote Sensing-
dc.relation.journalWebOfScienceCategoryImaging Science & Photographic Technology-
dc.subject.keywordPlusRADAR RAINFALL-
dc.subject.keywordPlusMODEL-
dc.subject.keywordPlusSTREAMFLOW-
dc.subject.keywordPlusPRECIPITATION-
dc.subject.keywordPlusASSIMILATION-
dc.subject.keywordPlusCALIBRATION-
dc.subject.keywordPlusACCURACY-
dc.subject.keywordAuthorDeep learning-
dc.subject.keywordAuthordistributed hydrologic model-
dc.subject.keywordAuthorhydrology-
dc.subject.keywordAuthorlong short-term memory (LSTM)-
dc.subject.keywordAuthormachine learning-
dc.subject.keywordAuthorradar precipitation-
dc.identifier.urlhttps://ieeexplore.ieee.org/document/10153688-
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