National Institute of Hydrology, North Eastern Regional Centre, Guwahati-781006, India.
National Institute of Hydrology, Roorkee-247667, India.
Environ Monit Assess. 2024 Feb 22;196(3):294. doi: 10.1007/s10661-024-12433-4.
The current study investigates the joint impact of projected land use/land cover change (LULCC) and climate change on the discharge of river Puthimari using Soil and Water Assessment Tool (SWAT). Puthimari, flowing through part of Bhutan and the northeastern region of India, earns its significance by contributing a fairly huge amount of discharge to the mainstream Brahmaputra causing frequent floods downstream, specifically in the monsoon season. The analysis was carried out from 2025 to 2099, by dividing this entire period into three sub-periods, 2025‒2049, 2050‒2074, and 2075‒2099, each of 25 years duration. To evaluate the impact of climate change, this study considered future climate data of five different CMIP5 (Coupled Model Intercomparison Project) climate models and their ensemble for RCP4.5 and RCP8.5 (Representative Concentration Pathways). The changes in LULC were incorporated by projecting the future LULC for 2035, 2065, and 2085 for each of the periods using the CA (Cellular Automata)-Markov model. SWAT performed well for both calibration and validation. The respective Nash-Sutcliffe efficiency (NSE) values for calibration and validation were found to be 0.74 and 0.77. Also, 0.75 and 0.79 coefficient of determination (R) values were obtained for calibration and validation, respectively. The analyses reveal a 19.76% increase in rural settlement, and a 6.30%, 16.45%, and 8.76% decrease in forest, cropland, and waterbodies in the watershed by the end of this century. The average monsoon rainfall would increase by 14.16% and 38.92%, with a corresponding increase in discharge by 34.27% and 64.67%, under RCP 4.5 and RCP 8.5, respectively. This comprehensive study represents a pioneering effort to thoroughly analyze the future hydrological dynamics of the Puthimari River. This research serves as a vital resource for policymakers and government agencies, offering valuable insights to guide both structural and non-structural measures aimed at safeguarding the river from potential flood devastation. Additionally, it provides essential information to support the implementation of effective watershed management practices.
本研究利用土壤和水评估工具(SWAT),调查土地利用/土地覆被变化(LULCC)和气候变化对普提马里河排放量的联合影响。普提马里河发源于不丹部分地区和印度东北部,其支流众多,为主流雅鲁藏布江提供了相当大的径流量,导致下游特别是季风季节经常发生洪水。该分析从 2025 年到 2099 年进行,整个时间段分为三个子时间段,每个子时间段持续 25 年,分别为 2025-2049 年、2050-2074 年和 2075-2099 年。为了评估气候变化的影响,本研究考虑了五个不同的 CMIP5(耦合模型比较计划)气候模型的未来气候数据及其代表浓度路径 4.5 和 8.5(RCP)的集合。利用 CA(元胞自动机)-马尔可夫模型,对每个时间段的 2035 年、2065 年和 2085 年的未来土地利用/土地覆被进行预测,从而纳入土地利用/土地覆被变化。SWAT 在校准和验证方面表现良好。校准和验证的纳什-苏特克里夫效率(NSE)值分别为 0.74 和 0.77。此外,校准和验证的决定系数(R)值分别为 0.75 和 0.79。分析表明,本世纪末,流域内农村住区增加 19.76%,森林、耕地和水体分别减少 6.30%、16.45%和 8.76%。在 RCP4.5 和 RCP8.5 下,季风降雨平均增加 14.16%和 38.92%,相应的径流量增加 34.27%和 64.67%。本综合研究代表了对普提马里河未来水文动态进行彻底分析的开创性努力。这项研究为政策制定者和政府机构提供了宝贵的资源,为保护河流免受潜在洪水破坏提供了有价值的见解,指导采取结构性和非结构性措施。此外,它还提供了实施有效流域管理实践的重要信息。