Water balance of Maninjau watershed with SWAT hydrological model

被引:2
|
作者
Ridwansyah, I [1 ]
Rustini, H. A. [1 ]
Yulianti, M. [1 ]
Apip [1 ]
Harsono, E.
机构
[1] Cibinong Sci Ctr Bot Garden, Res Ctr Limnol, Indonesian Inst Sci LIPI, Cibinong 16911, Indonesia
关键词
model; water balance; SWAT; hydrology;
D O I
10.1088/1755-1315/535/1/012035
中图分类号
S9 [水产、渔业];
学科分类号
0908 ;
摘要
Lake Maninjau was one of the international tourist destinations before the 2000s. Aside from being used as a source of 66 MW hydroelectric power built in 1972, currently, this caldera lake is also used for aquaculture. Lake Maninjau ecosystem, which consists of water bodies and watersheds, has an area of 23,729.3 Ha. The surface area of Lake Maninjau at +461.5 m asl is 9,737.5 Ha. Calculation of water balance in the Lake Maninjau watershed becomes a necessity because of its multi-functional status. Maninjau watershed water balance is estimated using SWAT (Soil and Water Assessment Tools) model. Rainfall data from Climate Hazard Group InfraRed Precipitation with Station (CHIRPS) was reanalyzed and compared with local rainfall data. The simulation conducted for 1981 - 2019 on the sub-watershed scale produced NSE and R-2 values of 0.61 and 0.7, respectively. The simulation was scaled up for the entire catchment of Lake Maninjau. Simulation results showed that an average annual rainfall of 2,483.9 mm/year produced a surface flow, interflow, base flow, and recharge to aquifer of 7.8 mm/year, 1397.4 mm/year, 273.4 mm/year and 14.7 mm/year, respectively.
引用
收藏
页数:11
相关论文
共 50 条
  • [41] Assessment of hydrological water balance in Lower Nzoia Sub-catchment using SWAT-model: towards improved water governace in Kenya
    Juma, Lilian A.
    Nkongolo, Nsalambi, V
    Raude, James M.
    Kiai, Caroline
    [J]. HELIYON, 2022, 8 (07)
  • [42] Performance of WASMOD and SWAT on hydrological simulation in Yingluoxia watershed in northwest of China
    Li, Zhanling
    Xu, Zongxue
    Li, Zhanjie
    [J]. HYDROLOGICAL PROCESSES, 2011, 25 (13) : 2001 - 2008
  • [43] Impacts of Hydrological Processes on Stream Temperature in a Cold Region Watershed Based on the SWAT Equilibrium Temperature Model
    Du, Xinzhong
    Goss, Greg
    Faramarzi, Monireh
    [J]. WATER, 2020, 12 (04)
  • [44] Hydrological simulation and evaluation of drought conditions in the ungauged watershed Parishan lake Iran, using the SWAT model
    Ansarifard, Sara
    Ghorbanifard, Mahdi
    Boustani, Fardin
    Abdolazimi, Hadi
    [J]. JOURNAL OF WATER AND CLIMATE CHANGE, 2024, : 4666 - 4698
  • [45] Simulation of Mountainous Watershed Hydrological Process Responses on the Land Cover and Climate Changes Based on SWAT Model
    Lu Ying
    Buchanan, Sam
    He Daming
    Liu Jiang
    [J]. PROGRESS IN ENVIRONMENTAL SCIENCE AND TECHNOLOGY, VOL II, PTS A AND B, 2009, : 124 - 127
  • [46] Understanding the effects of soil data quality on SWAT model performance and hydrological processes in Tamedroust watershed (Morocco)
    Bouslihim, Yassine
    Rochdi, Aicha
    El Amrani Paaza, Namira
    Liuzzo, Lorena
    [J]. JOURNAL OF AFRICAN EARTH SCIENCES, 2019, 160
  • [47] Impacts of hydrological processes on stream temperature in a cold region watershed based on the SWAT equilibrium temperature model
    Du, Xinzhong
    Goss, Greg
    Faramarzi, Monireh
    [J]. Faramarzi, Monireh (faramarz@ualberta.ca), 1600, MDPI AG (12):
  • [48] Efficient flow calibration method for accurate estimation of baseflow using a watershed scale hydrological model (SWAT)
    Jang, Won Seok
    Engel, Bernard
    Ryu, Jichul
    [J]. ECOLOGICAL ENGINEERING, 2018, 125 : 50 - 67
  • [49] Sediment Balance Estimation of the 'Cuvette Centrale' of the Congo River Basin Using the SWAT Hydrological Model
    Datok, Pankyes
    Sauvage, Sabine
    Fabre, Clement
    Laraque, Alain
    Ouillon, Sylvain
    N'kaya, Guy Moukandi
    Sanchez-Perez, Jose-Miguel
    [J]. WATER, 2021, 13 (10)
  • [50] A BASE MODEL FOR WATER BALANCE OF MESTA RIVER WATERSHED
    Kirilov, Leoneed
    Bournaski, Emil
    Iliev, Rossen
    [J]. COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES, 2022, 75 (12): : 1796 - 1804