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Kidoo Park, Yeongjeong Seong, Younghun Jung, Ilro Youn and Cheon Kyu Choi
The methods for improving the accuracy of water level prediction were proposed in this study by selecting the Gated Recurrent Unit (GRU) model, which is effective for multivariate learning at the Paldang Bridge station in Han River, South Korea, where th...
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Kidoo Park, Younghun Jung, Yeongjeong Seong and Sanghyup Lee
Since predicting rapidly fluctuating water levels is very important in water resource engineering, Long Short-Term Memory (LSTM) and Gated Recurrent Unit (GRU) were used to evaluate water-level-prediction accuracy at Hangang Bridge Station in Han River, ...
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Stavroula Dimitriadou and Konstantinos G. Nikolakopoulos
The present study develops ArcMap models to implement the following three methods: FAO-56 Penman?Monteith (FAO PM), Hargreaves?Samani (HS) and Hansen, with the former used as a reference. Moreover, three models implementing statistical indices (RMSD, MB,...
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Héctor Navarro-Barboza,Aldo Moya-Álvarez,Ana Luna,Octavio Fashé-Raymundo
Pág. 71 - 86
This study assesses the influence of PM10 on the optical thickness of aerosols in the central Andes of Peru, in addition to analyzing and establishing their circulation patterns from July to October 2017. This particular period is considered herein becau...
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Getnet Feyissa, Gete Zeleke, Woldeamlak Bewket and Ephrem Gebremariam
One of the recent advances in climate science research is the development of global general circulation models (GCMs) to simulate changes in climatic elements of the present and future, which helps us to determine consequences earlier and prepare for nec...
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Chrissa Georgakis and Mattheos Santamouris
The present study aims to present all the findings of micro-climate measurements that were performed by the University of Athens in the center of Athens, during the summer period. The extended experimental campaign aimed to collect thermal and air flow m...
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J. L. LABAJO SALAZAR,F. DE PABLO,E. L. GARCÍA
This work is directed to establish how the linear relation h2 ? h1 = -0,03 - 3,586(T2 ? T1), which is suppose to be valid at any point on the Earth and time of the year, and whose coefficients are obtained using synchronous series of three hourly data...
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