Year |
Citation |
Score |
2023 |
Gomaa E, Zerouali B, Difi S, El-Nagdy KA, Santos CAG, Abda Z, Ghoneim SSM, Bailek N, Silva RMD, Rajput J, Ali E. Assessment of hybrid machine learning algorithms using TRMM rainfall data for daily inflow forecasting in Três Marias Reservoir, eastern Brazil. Heliyon. 9: e18819. PMID 37593632 DOI: 10.1016/j.heliyon.2023.e18819 |
0.333 |
|
2023 |
Zerouali B, Santos CAG, de Farias CAS, Muniz RS, Difi S, Abda Z, Chettih M, Heddam S, Anwar SA, Elbeltagi A. Artificial intelligent systems optimized by metaheuristic algorithms and teleconnection indices for rainfall modeling: The case of a humid region in the mediterranean basin. Heliyon. 9: e15355. PMID 37128305 DOI: 10.1016/j.heliyon.2023.e15355 |
0.398 |
|
2020 |
Freire PKdMM, Santos CAG. Optimal level of wavelet decomposition for daily inflow forecasting Earth Science Informatics. 13: 1163-1173. DOI: 10.1007/s12145-020-00496-z |
0.311 |
|
2012 |
Santos C, Freire P, Mishra S. CUCKOO SEARCH VIA LÉVY FLIGHTS FOR OPTIMIZATION OF A PHYSICALLY-BASED RUNOFF-EROSION MODEL Journal of Urban and Environmental Engineering. 6: 123-131. DOI: 10.4090/Juee.2012.V6N2.123131 |
0.482 |
|
2010 |
Santos C, Pinto L, De Macedo Machado Freire P, Mishra S. Application of a particle swarm optimization to a physically-based erosion model Annals of Warsaw University of Life Sciences - Sggw. Land Reclamation. 42: 39-49. DOI: 10.2478/V10060-008-0063-9 |
0.471 |
|
2003 |
Santos CAG, Srinivasan VS, Suzuki K, Watanabe M. Application of an optimization technique to a physically based erosion model Hydrological Processes. 17: 989-1003. DOI: 10.1002/HYP.1176 |
0.429 |
|
2000 |
SANTOS CAG, SUZUKI K, WATANABE M. IMPROVEMENT IN A GENETIC ALGORITHM FOR OPTIMIZATION OF RUNOFF-EROSION MODELS Proceedings of Hydraulic Engineering. 44: 705-710. DOI: 10.2208/PROHE.44.705 |
0.303 |
|
1999 |
SANTOS CAG, SUZUKI K, WATANABE M, SRINIVASAN VS. OPTIMIZATION OF A RUNOFF-EROSION MODEL THROUGH A GENETIC ALGORITHM Proceedings of Hydraulic Engineering. 43: 557-561. DOI: 10.2208/PROHE.43.557 |
0.307 |
|
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