Hydrological Drought Analysis for Bolu City with Streamflow Drought Index

Hydrological drought refers to the decrease in the amount of water found in surface or groundwater resources and monitoring of this natural disaster is very important due to causing serious problems in drinking and irrigation water supply and hydroelectric energy production. In this study, hydrological drought analysis was made for two streams in Bolu city located in the Western Black Sea Region in the north of Turkey and 3, 6 and 12 month streamflow drought indices were calculated by using the Streamflow Drought Index method. For this aim, the streamflow data of Bolu stream - Beşdeğirmen and Ulusu - Afatlar streamflow monitoring stations were used. According to the results, extreme and severedroughts were determined for two stream flow stations and it is seen that drought periods varied between 1 and 9 years. The most severe and longest droughts were detected for Bolu stream - Beşdeğirmen station. Mild droughts are much higher than moderate, severe and extreme droughts. It has been observed that the severity and number of drought for Bolu stream - Beşdeğirmen station have increased in recent years. In order to reduce the effects of hydrological drought, hydrological drought should be monitored continuously and necessary precautions should be taken regarding the management of water resources. People should be informed about water consumption and so waste should be prevented. Interms of irrigation water, drip irrigation method should be used instead of flood irrigation or sprinkler irrigation methods. For this aim, farmers should be made aware of this issue. Alternative renewable energy sources or other energy sources should be used for reductions in hydroelectric energy production. 

Hydrological Drought Analysis for Bolu City with Streamflow Drought Index

Hydrological drought refers to the decrease in the amount of water found in surface or groundwater resources. Hydrological drought causes serious problems in drinking and irrigation water supply and hydroelectric energy production. In this study, hydrological drought analysis was made for two streams in Bolu city located in the Western Black Sea Region in the north of Turkey. For this purpose, 3, 6 and 12 month flow drought indices were calculated using the Streamflow Drought Index method and the streamflow data of two streamflow monitoring stations. According to the results, extreme and severe droughts were determined for two stream flow stations and it is seen that drought periods varied between 1 and 9 years. The most severe and longest droughts were detected for Bolu stream - Beşdeğirmen station. Mild droughts are much higher than moderate, severe and extreme droughts. It has been observed that the severity and number of drought for Bolu stream - Beşdeğirmen station have increased in recent years. In order to reduce the effects of hydrological drought, hydrological drought should be monitored continuously and necessary precautions should be taken regarding the management of water resources. People should be informed about water consumption and so waste should be prevented. In terms of irrigation water, drip irrigation method should be used instead of flood irrigation or sprinkler irrigation methods. For this aim, farmers should be made aware of this issue. Alternative renewable energy sources or other energy sources should be used for reductions in hydroelectric energy production.

___

  • [1] H. Tabari, J. Nikbakht, P. Hosseinzadeh Talaee, P., “Hydrological Drought Assessment in Northwestern Iran Based on Streamflow Drought Index (SDI),’’ Water Resources Management, vol. 27, no. 1, pp. 137-151, 2013.
  • [2] L. Zhao, A. Lyu, J. Wu, M. Hayes, Z. Tang, B. He, M. and Lıu, “Impact of Meteorological Drought on Streamflow Drought in Jinghe River Basin of China,’’ Chinese Geographical Science, vol. 24, no. 6, pp. 694–705, 2014.
  • [3] X. Hong, S. Guo, Y. Zhou, L. and Xiong, “Uncertainties in assessing hydrological drought using streamflow drought index for the upper Yangtze River basin,” Stochastic Environmental Research and Risk Assessment, vol. 29, no. 4, pp. 1235-1247, 2014.
  • [4] H. Akbarı, G. R. Rakhshandehroo, A. H. Sharıfloo, and E. Ostadzadeh, “Drought Analysis Based on Standardized Precipitation Index (SPI) and Streamflow Drought Index (SDI) in Chenar Rahdar River Basin, Southern Iran,” In Proceedings of the Watershed Management Symposium, 2015, pp. 11-22.
  • [5] Wu. Zhıyong, Lın. Qıngxıa, Lu. Guıhua, He. Haı, J. Qu John, J. “Analysis of Hydrological Drought Frequency For The Xijiang River Basin in South China Using Observed Streamflow Data,’’ Nat Hazards, vol. 77, no. 1, pp. 655–1677, 2015.
  • [6] K. J. Won, S. H. Kım, E. S. Chung, S. U., Kım and M. W. Son, “Drought Analysis of Cheongmicheon in Korea Based on Various Drought Idices,’’ in 5. Proceedings of the 3rd International Conference on Civil, Offshore and Environmental Engineering, 2016. pp. 311-315.
  • [7] M. Fendeková, T. Gauster, L. Labudová, D., Vrablíková, Z., Danáčová, M., Fendek and P. Pekárová, “Analysing 21st century meteorological and hydrological drought events in Slovakia,’’ Journal of Hydrology and Hydromechanics, vol. 66, no. 4, pp. 393-403, 2018.
  • [8] V. Gümüş, “Hydrological Drought Analysis of Asi River Basin with Streamflow Drought Index,’’ GU J Sci, Part C, vol. 5, no.1, pp. 65-73, 2017.
  • [9] V. Gumus, and H. M. Algin, “Meteorological and hydrological drought analysis of the Seyhan−Ceyhan River Basins, Turkey,’’ Meteorological Applications, vol. 24, no. 1, pp. 62-73, 2017.
  • [10] M. Özfidander, D. S. Ucan, F. Topaloglu, “Hydrological Drought Analysis of Streamflow Data in Seyhan Basin,’’ Toprak Su Dergisi, vol. 7, no. 1, pp. 57-64, 2018.
  • [11] M. S. Yıldız, “Akım Kuraklık İndeksi Yöntemi İle Fırat Havzasının Hidrolojik Kuraklık Analizi,’’ Harran Üniversitesi Fen Bilimleri Enstitüsü, Yüksek Lisans Tezi, 129 sayfa, 2019.
  • [12] T. A. Eroglouer, H. Apaydin, “Estimation of Drought by Streamflow Drought Index (SDI) and Artificial Neural Networks (ANNs) in Ankara-Nallihan Region,’’ Turkish Journal of Agriculture - Food Science and Technology, vol. 8, no. 2, pp. 348-357, 2020.
  • [13] T.C. Bolu ValiliğiÇevre ve Şehircilik İl Müdürlüğü. (12 Ağustos 2021). Bolu İli 2019 Yılı Çevre Durum Raporu. Erişim adresi https://webdosya.csb.gov.tr/db/ced/icerikler/bolu_-cdr2019-20200624102754.pdf.
  • [14] I. Nalbantis, I., “Evaluation of a hydrological drought index’’, Eur Water, vol. 23, no. 24, pp. 67-77, 2008.