[102] |
Zalnezhad et al., 2022 |
ANFIS(FCM) * ANFIS(SC) ANFIS(GP) QRT |
A, I, MAR, SF, MAE, SDEN, S1085, FOR |
Q2–100 |
181 Stations 40–89 Year |
Water |
Australia |
50.88 |
RRMSE = 0.78 |
NA |
[97] |
Desai and Ouarda, 2021 |
CCA-RFR * PFR CCA-GAM EANN ANN CCA-MLR CCA-Kriging CCA-EANN CCA-ANN |
A, MBS, FAL, AMP, AMD |
Q10–100 |
151 stations, ≥15 year |
Journal of Hydrology |
Canada (Quebec) |
0.05 |
NASH = 0.57 RRMSE = 29.44 |
NA |
[96] |
Linh et al., 2021 |
WNN * ANN |
SLP, SST |
Max monthly discharge (MAD) |
3 stations, 37 years |
Acta Geophysica |
Iran (Golestan Dam, Madarsoo) |
0.68 |
NASH = 0.99 |
0.99 |
[59] |
Allahbakhshian-Farsani et al., 2020 |
SVR * MARS BRT PPR NLR |
A, AA, AMP, MXP, NDP, CC, CR, TC, P, SL, DD, SS, MBS, PF, SDT, RA, BL, FLA, FOR, RLA, DA, WA, EL, MXEL, MNEL |
Q2–200 |
54 stations, 19 years |
Water Resources Management |
Iran (Karun and Karkhe River) |
50.70 |
NASH = 0.94 RRMSE = 63.93 |
0.96 |
[95] |
Kordrostami et al., 2020 |
ANN |
A, AEV, AMP, FOR, I, SS, SF and DD |
Q5–100 |
88 stations, 25–82 years |
Geosciences |
Australia (New South Wales) |
NA |
RRMSE = 0.48 |
0.74 |
[65] |
Haddad and Rahman, 2020 |
MDS-SVR * MDS-BGLSR |
A, AEV, SF, DD, SS, FOR, I and AMP |
Q2–100 |
202 stations, 25–82 years |
Natural Hazards |
Australia (New South Wales and Victoria) |
NA |
RRMSE = 56 |
0.78 |
[112] |
Vafakhah and Khosrobeigi Bozchaloei, 2020 |
SVR * ANN NLR |
A, AA, AEV, P, MBS, MXEL, MNEL, EL, SL, DD, SS, AMP, T, PF, RLA, BL, GA, RA |
Q2–90 |
33 Stations, 20 years |
Water Resources Management |
Iran (Namak Lake) |
0.11 |
NASH = 0.91 RRMSE = 1.45 |
0.96 |
[111] |
Ghaderi et al., 2019 |
SVM * ANFIS GEP |
A, P, MBS, EL, L, SL, SS, DD, MXSO, FF, L, CR, CC, AMP, MXP, BL, FOR |
Q50 |
47 stations, 21 years |
Arabian Journal of Geosciences |
Iran (South-west) |
239.94 |
NASH = 0.75 |
0.76 |
[110] |
Sharifi Garmdareh et al., 2018 |
ANFIS * SVR ANN NLR |
A, AEV, P, DD, MXEL, MNEL, MBS, EL, SL, SS, T, AMP, |
Q2–100 |
55 stations, 20 years |
Hydrological Sciences Journal |
Iran (Namak Lake) |
8.40 |
NASH = 0.90 |
0.95 |
[67] |
Aziz et al., 2017 |
ANN * GEP * QRT |
A, AEV, AMP, SS, I |
Q2–100 |
452 stations, 25–75 years |
Stochastic Environmental Research and Risk Assessment |
Australia (New South Wales, Victoria, Queensland and Tasmania) |
Na |
NASH for ANN for smaller ARIs = 0.78 NASH for GEP for larger ARIs = 0.73 |
NA |
[92] |
Ouali et al., 2017 |
NLCCA-GAM * NLCCA-EANN CCA-ANN CCA-EANN NLCCA-ANN NLCCA-GAM/ STPW |
A, MBS, FAL, AMP, AMD |
Q10–100 |
151, 204 and 69 stations, ≥15 years |
Journal of Advances in Modeling Earth Systems |
Canada and United states (Quebec, Arkansas, Texas) |
NA |
RRMSE = 0.28 NASH > 0.8 |
NA |
[109] |
Gizaw and Gan, 2016 |
SVR * ANN |
A, SS, SL, TC, I, AMP |
Q10–100 |
26 and 23 stations, ≥15 years |
Journal of Hydrology |
Canada (British Columbia, Ontario) |
46.2 |
NA |
0.7 |
[106] |
Aziz et al., 2016 |
ANN * GAANN CANFIS GEP |
A, AEV, I, AMP, SS, |
Q2–100 |
452 Stations, 25–75 years |
Artificial Neural Network Modelling (Book) |
Australia (New South Wales, Victoria, Queensland and Tasmania) |
NA |
NASH = 0.69 |
NA |
[61] |
Kumar et al., 2015 |
FIS * ANN L-moments (PE3) |
A, AMP, SDT, EL |
Q2–1000 |
17 stations, 15–29 years |
Water Resources Management |
India (Godavari river) |
2.32 |
Na |
NA |
[114] |
Aziz et al., 2015 |
GAANN BPANN |
A, I |
Q2–100 |
452 stations, 25–75 years |
Natural Hazards |
Australia (New South Wales, Victoria, Queensland, and Tasmania) |
NA |
NA |
NA |
[105] |
Bozchaloei and Vafakhah, 2015 |
ANFIS * ANN NLR |
A, AA, AEV, P, MBS, MXEL, MNEL, EL, SL, DD, SS, AMP, T, PF, RLA, BL, GA, RA |
Q2–92 |
33 stations, 20 years |
Journal of Hydrologic Engineering |
Iran (Namak Lake) |
0.008 |
NASH = 0.92 |
0.99 |
[87] |
Durocher et al., 2015 |
PPR * |
A, SL, SS, MBS, FOR, FAL, AMP, AMPS, AMPL, MLS, AMD |
Q10–100 |
151 stations, ≥15 years |
Journal of Hydrometeorology |
Canada (Quebec) |
NA |
RRMSE = 0.40 |
NA |
[86] |
Alobaidi et al., 2015 |
G-EANN * EANN |
A, MBS, FAL, AMD, AMP |
Q10–100 |
151 stations, ≥15 years |
Advances in Water Resources |
Canada (Quebec) |
NA |
RRMSE = 0.34 |
NA |
[85] |
Aziz et al., 2014 |
ANN * QRT |
A, AEV, AMP, SS, I |
Q2–100 |
452 stations, 25–75 years |
Stochastic Environmental Research and Risk Assessment |
Australia (New South Wales, Victoria, Queensland, Tasmania) |
NA |
NA |
NA |
[103] |
Aziz et al., 2013 |
BGLS-QRT-ROI * CANFIS |
A and I |
Q2–100 |
452 stations, 25–75 years |
Journal of Hydrological Environment Resources |
Australia (New South Wales, Victoria, Queensland, and Tasmania) |
NA |
NA |
NA |
[84] |
Seckin et al., 2013 |
MLP * L-moment RBNN GRNN MLR MNLR |
A, EL, LAT, LON, and RP |
Q1.111–1000 |
13 stations, 10-39 years |
Water Resources Management |
Turkey (East Mediterranean River) |
0.173 |
NA |
0.84 |
[113] |
Seckin and Guven, 2012 |
GEP * LGP LR |
A, EL, LAT, LON, and RP |
Q25.7–174.3 |
543 stations, ≥15 years |
Water Resource Management |
Turkey (Rivers across the country) |
NA |
NA |
0.57 |
[83] |
Singh et al., 2010 |
BNN * M5 |
A, MRD, AMP, RP, MBS and FOR |
Q2.33 |
93 stations, 10–83 years |
Water Resources Management |
India (Catchments across the country) |
NA |
NA |
NA |
[82] |
Ouarda and Shu, 2009 |
ANN * Multiple regression model |
A, FAL, FOR, AMD, AMPL, NT27, CN |
Q2–10 |
134 stations, ≥10 years |
Water Resources Research |
Canada (Quebec) |
27.33 |
NASH = 0.96, RRMSE = 36.17 |
NA |
[55] |
Shu and Ouarda, 2008 |
ANFIS * ANN NLR NLR-R |
A, MBS, FAL, AMP, AMD, HDB, TOPO |
Q10–100 |
151 stations- ≥15 years |
Journal of Hydrology |
Canada (Quebec) |
316 |
NASH = 0.85 RRMSE = 57 |
NA |
[49] |
Srinivas et al., 2008 |
SOFM * CCA Regional regression |
A, SS, SRC, SSC, AMP, SL, EL, FOR, R24h |
Q2–100 |
11 stations, 6–42 years |
Journal of Hydrology |
United states (Indiana) |
NA |
RRMSE = 0.276 |
NA |
[56] |
Shu and Ouarda, 2007 |
ANN * ANN-CCA |
A, AMD, AMP, FAL, MBS |
Q10–50 |
151 stations, ≥15 year |
Water Resources Research |
Canada (Quebec) |
0.053 |
NASH = 0.82 RRMSE = 38 |
NA |
[81] |
Dawson et al., 2006 |
ANN * MLR |
A, AMP, L, DA, IF |
Q10, 20, 30 |
850 stations, 20 years |
Journal of Hydrology |
United kingdom (Catchment across the UK) |
NA |
NA |
NA |
[80] |
Jingyi and Hall, 2004 |
ANN * Cluster analysis |
A, AMP, MXP, SL, SS, EL, GFI and PLN |
Q50 |
86 stations 15–36 years |
Journal of Hydrology |
China (Jiangxi and Fujian, Gan and Ming rivers) |
47 |
NA |
NA |
[51] |
(Shu and Burn, 2004) |
ANN * Ordinary least squares regression (REG_OLS) Non-linear regression (REG_NONLINEAR) |
A, AMP, SDT, FARL |
Q10 |
404 stations 29 years |
Water Resources Management |
United Kingdom (England, Scotland, and Wales) |
NA |
NA |
NA |