Department of Geoinformatics, School of Natural Resource Management, Central University of Jharkhand, Ranchi, 835222, India.
Environ Monit Assess. 2024 Aug 27;196(9):849. doi: 10.1007/s10661-024-13041-y.
Climate change has a significant impact on the Ganga-Brahmaputra (GB) basin, the major food belt of India, which frequently experiences flooding and varied incidences of drought. The current study examines the changing trend of rainfall and temperature in the GB basin over a period of 30 years to identify areas at risk with an emphasis on the Paris Agreement's mandate to keep increasing temperatures below 2 °C. The maximum temperature anomaly in the middle Ganga plains recorded an increase of more than 1.5 °C year in 1999, 2005, and 2009. Some extreme events were observed in the Brahmaputra basin during 1999, 2009, and 2010, where a prominent temperature increase of 1.5 °C year was observed. The minimum temperature revealed an increasing trend for the G-B basin with an anomalous increase of 0.04 to 0.06 °C year. The rainfall variability across the Ganga basin shows a rising tendency over the lower Ganga region while the Brahmaputra basin showed a downward trend. To identify the statistical relation between the Global climatic oscillations and regional climate, Standardized Precipitation Index (SPI) and Niño 3.4 were used. The wet and dry period estimation shows a rise in flood conditions in the Ganga basin whereas, in the Brahmaputra basin, an increase in drought frequency was observed. The correlation based on Niño 3.4 and SPI3 presents a negative relation for the monsoon season in the G-B basin revealing a situation of drought occurrence (SPI3 below 0) with increased Nino 3.4 values (El Niño above + 0.4C).
气候变化对印度主要粮食产区恒河-布拉马普特拉(GB)流域产生了重大影响,该地区经常遭受洪水和不同程度的干旱。本研究考察了 30 年来 GB 流域降雨量和温度的变化趋势,以确定处于危险之中的地区,重点是《巴黎协定》将气温上升控制在 2°C 以下的任务。恒河中游平原的最高温度异常在 1999 年、2005 年和 2009 年记录的年增长率超过 1.5°C。在 1999 年、2009 年和 2010 年观察到了一些极端事件,其中观察到了 1.5°C 年的显著温度上升。GB 流域的最低温度呈现出上升趋势,异常增加了 0.04 到 0.06°C 年。恒河流域的降雨变化显示,较低恒河流域的上升趋势明显,而布拉马普特拉流域则呈下降趋势。为了确定全球气候振荡与区域气候之间的统计关系,使用了标准化降水指数(SPI)和 Niño 3.4。干湿期估计表明,恒河流域的洪水情况有所增加,而在布拉马普特拉河流域,干旱频率有所增加。基于 Niño 3.4 和 SPI3 的相关性显示,GB 流域季风季节存在负相关关系,表明出现了干旱情况(SPI3 低于 0),同时 Niño 3.4 值增加(厄尔尼诺现象超过+0.4°C)。