2019
DOI: 10.3390/atmos10080466
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Modeling Streamflow Enhanced by Precipitation from Atmospheric River Using the NOAA National Water Model: A Case Study of the Russian River Basin for February 2004

Abstract: This study aims to address hydrological processes and impacts of an atmospheric river (AR) event that occurred during 15–18 February 2004 in the Russian River basin in California. The National Water Model (NWM), a fully distributed hydrologic model, was used to evaluate the hydrological processes including soil moisture flux, overland flow, and streamflow. Observed streamflow and volumetric soil water content data were used to evaluate the performance of the NWM using various error metrics. The simulation resu… Show more

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Cited by 21 publications
(9 citation statements)
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“…However, the NWM utilizes a physically nonexplicit conceptual module for simulating baseflow (Knebl et al 2005). Although there have been studies involving the NWM (Souffront Alcantara et al 2017; Han et al 2019), to date no study has evaluated the NWM for its baseflow simulating capabilities.…”
Section: Introductionmentioning
confidence: 99%
“…However, the NWM utilizes a physically nonexplicit conceptual module for simulating baseflow (Knebl et al 2005). Although there have been studies involving the NWM (Souffront Alcantara et al 2017; Han et al 2019), to date no study has evaluated the NWM for its baseflow simulating capabilities.…”
Section: Introductionmentioning
confidence: 99%
“…장단기 메모리(long short-term memory, LSTM)는 순환 신경망(recurrent neural network, RNN) 기법의 하나로 셀 (cell), 입력 게이트(input gate), 출력 게이트(output gate), 망각 게이트(forget gate)를 이용해 기존 순환 신경망(RNN) 의 단점인 기울기 소멸 문제(vanishing gradient problem)를 방지하도록 개발되었다 (Hochreiter and Schmidhuber, 1997;Agmls et al, 2009). 장단기 메모리는 순환 신경망의 일종이 지만 단점을 보완하여, 입력 자료에 대한 정보를 더욱 장기적 으로 기억하기 위해, 은닉층에 셀 상태(cell state)구조를 추가한 것이다 (Han et al, 2019;Le et al, 2019;Fig. 4).…”
Section: 장단기 메모리unclassified
“…The Russian River basin is located on the west coast of the United States with an average annual precipitation of 1180 mm and more than 80% of its annual precipitation was observed during wet season (from November to March). The Russian River basin is affected by various meteorological factors such as extratropical cyclones, jet streams, and atmospheric rivers from the Pacific oceans [46]. For runoff forecasting at outlet point, hourly runoff data were obtained from five United States Geological Survey (USGS) stations (Station ID: 11461500; 11462500; 11463000; 11464000; and 11467000) for the period from 2015 to 2019.…”
Section: Study Area and Datamentioning
confidence: 99%