WWF-India, 172 - B, Lodi Estate, New Delhi, 110003, India,
Environ Manage. 2014 Jan;53(1):120-34. doi: 10.1007/s00267-013-0196-4. Epub 2013 Nov 8.
The Sharda River creates and maintains the ecologically diverse remnant patches of rare Terai ecosystem in northern India. This study used repeat satellite imagery and geographic information system analysis to assess the planform dynamics along a 60 km length of the Sharda River between 1977 and 2001 to understand the altered dynamics and its plausible causes in this data-poor region. Analyses revealed that the Sharda River has undergone significant change corresponding to enhanced instability in terms of increased number of neck cut-offs and consistent occurrence of avulsions in subsequent shorter assessment periods. An increased channel area (8%), decreased sinuosity (15%), increased braiding intensity, and abrupt migrations were also documented. The river has migrated toward the east with its west bankline being more unstable. The maximum shifts were 2.85 km in 13 years (1977-1990), 2.33 km in next 9 years (1990-1999), and a substantial shift of 2.39 km in just 2 years (1999-2001). The altered dynamics is making the future of critical wildlife habitats in Kishanpur Wildlife Sanctuary and North Kheri Forest Division precarious and causing significant economic damage. Extensive deforestation and expansion of agriculture since the 1950s in the catchment area are presumed to have severely impacted the equilibrium of the river, which urgently needs a management plan including wildlife habitat conservation, control, and risk reduction. The present study provides a strong foundation for understanding channel changes in the Sharda River and the finding can serve as a valuable information base for effective management planning and ecological restoration.
沙尔达河在印度北部创造并维持着具有独特生态多样性的特莱稀树草原生态系统残余斑块。本研究利用重复卫星图像和地理信息系统分析,评估了 1977 年至 2001 年间沙尔达河 60 公里长的河道平面形态动态,以了解该数据匮乏地区变化的动态及其可能的原因。分析表明,沙尔达河发生了重大变化,表现在颈口切断的数量增加,突发性决口在随后较短的评估期内持续发生,从而增强了不稳定性。河道面积增加了 8%,弯曲度降低了 15%,辫状程度增强,河道还发生了突然迁移。该河向东迁移,西岸线更不稳定。最大的偏移量为 13 年内 2.85 公里(1977-1990 年),9 年内 2.33 公里(1990-1999 年),以及在短短 2 年内 2.39 公里的大幅偏移(1999-2001 年)。变化的动态使得基山普尔野生动物保护区和北凯瑞森林区的关键野生动物栖息地的未来变得不稳定,并造成了重大的经济损失。自 20 世纪 50 年代以来,集水区内的大规模森林砍伐和农业扩张,被认为严重影响了河流的平衡,迫切需要制定包括保护野生动物栖息地、控制和降低风险在内的管理计划。本研究为了解沙尔达河河道变化提供了坚实的基础,研究结果可为有效的管理规划和生态恢复提供有价值的信息基础。