Pan Tao, Wu Shaohong, Liu Yujie
Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; Center for System Integration and Sustainability, Michigan State University, East Lansing, MI 48823, USA.
Key Laboratory of Land Surface Pattern and Simulation, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
PLoS One. 2015 Apr 23;10(4):e0123793. doi: 10.1371/journal.pone.0123793. eCollection 2015.
There is increasing evidence of environmental change impacts on ecosystem processes and services, yet poor understanding of the relative contributions of land use and climate change to ecosystem services variations. Based on detailed meteorological, hydrological records and satellite data over the Yellow River Source Area (YRSA) in Tibetan Plateau from 1980s to 2008, together with a water-yield module of Integrated Valuation of Ecosystem Services and Tradeoffs (InVEST) model and also a Residual Trends (RESTREND) method, we assessed the water supply variations in YRSA during the past three decades and disentangled the relative contributions of land use and climate change. Results show that water supply significantly decreased from 1980 to 2005 and then increased from 2005 to 2008. The quantity slightly decreased from 283.01 mm in 1980 to 276.95 mm in 1995, 270.12 mm in 2000 and 267.97 mm in 2005, and it then rebounded slightly to 275.26 mm in 2008. The water supply variation ranged from 283.01 mm to 267.97 mm. Climate change contributed dominantly to water supply decrease from 1980 to 1995, which accounts for approximately 64% of the decrease. During 1995 to 2000, land use contributed more and about 58% to the water supply decrease as the intense human activities. From 2000 to 2005, climate change became a positive contribution to the water supply as the increased precipitation, but the land use still contributed negatively. From 2005 to 2008, both climate and land use have positive impacts, but land use contributed about 61% to the water supply increase. The implementation of the Three Rivers Source Area Ecological Protection Project has greatly improved the vegetation coverage conditions and the water retention ability during this period. We recommend that the implementation of ecological projects, grazing policies and artificial improvement of degraded grassland would help to conserve the water retention ability and increase water supply.
有越来越多的证据表明环境变化对生态系统过程和服务产生影响,但对于土地利用和气候变化对生态系统服务变化的相对贡献了解不足。基于20世纪80年代至2008年青藏高原黄河源区(YRSA)详细的气象、水文记录以及卫星数据,结合生态系统服务与权衡综合评估(InVEST)模型的产水量模块和残差趋势(RESTREND)方法,我们评估了过去三十年黄河源区的供水变化,并厘清了土地利用和气候变化的相对贡献。结果表明,1980年至2005年供水显著减少,然后在2005年至2008年增加。水量从1980年的283.01毫米略微下降至1995年的276.95毫米、2000年的270.12毫米和2005年的267.97毫米,然后在2008年略微反弹至275.26毫米。供水变化范围为283.01毫米至267.97毫米。1980年至1995年气候变化是供水减少的主要原因,约占减少量的64%。1995年至2000年,由于人类活动强烈,土地利用对供水减少的贡献更大,约占58%。2000年至2005年,随着降水量增加,气候变化对供水产生了积极贡献,但土地利用仍有负面影响。2005年至2008年,气候和土地利用都有积极影响,但土地利用对供水增加的贡献约为61%。在此期间,三江源区生态保护工程的实施极大地改善了植被覆盖状况和蓄水能力。我们建议实施生态工程、放牧政策以及人工改良退化草地,将有助于保护蓄水能力并增加供水量。