Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1371/journal.pone.0071297 |
Climate Change Impacts on Streamflow and Subbasin-Scale Hydrology in the Upper Colorado River Basin | |
Ficklin, Darren L.1; Stewart, Iris T.2; Maurer, Edwin P.3 | |
通讯作者 | Ficklin, Darren L. |
来源期刊 | PLOS ONE
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ISSN | 1932-6203 |
出版年 | 2013 |
卷号 | 8期号:8 |
英文摘要 | In the Upper Colorado River Basin (UCRB), the principal source of water in the southwestern U.S., demand exceeds supply in most years, and will likely continue to rise. While General Circulation Models (GCMs) project surface temperature warming by 3.5 to 5.6 degrees C for the area, precipitation projections are variable, with no wetter or drier consensus. We assess the impacts of projected 21st century climatic changes on subbasins in the UCRB using the Soil and Water Assessment Tool, for all hydrologic components (snowmelt, evapotranspiration, surface runoff, subsurface runoff, and streamflow), and for 16 GCMs under the A2 emission scenario. Over the GCM ensemble, our simulations project median Spring streamflow declines of 36% by the end of the 21 st century, with increases more likely at higher elevations, and an overall range of -100 to +68%. Additionally, our results indicated Summer streamflow declines with median decreases of 46%, and an overall range of -100 to +22%. Analysis of hydrologic components indicates large spatial and temporal changes throughout the UCRB, with large snowmelt declines and temporal shifts in most hydrologic components. Warmer temperatures increase average annual evapotranspiration by similar to 23%, with shifting seasonal soil moisture availability driving these increases in late Winter and early Spring. For the high-elevation water-generating regions, modest precipitation decreases result in an even greater water yield decrease with less available snowmelt. Precipitation increases with modest warming do not translate into the same magnitude of water-yield increases due to slight decreases in snowmelt and increases in evapotranspiration. For these basins, whether modest warming is associated with precipitation decreases or increases, continued rising temperatures may make drier futures. Subsequently, many subbasins are projected to turn from semi-arid to arid conditions by the 2080 s. In conclusion, water availability in the UCRB could significantly decline with adverse consequences for water supplies, agriculture, and ecosystem health. |
类型 | Article |
语种 | 英语 |
国家 | USA |
收录类别 | SCI-E |
WOS记录号 | WOS:000323425700035 |
WOS关键词 | SOUTHWESTERN NORTH-AMERICA ; WATER ASSESSMENT-TOOL ; UNITED-STATES ; SIERRA-NEVADA ; COUPLED MODEL ; WARMING CLIMATE ; CHANGE SCENARIO ; CALIFORNIA ; SIMULATIONS ; CIRCULATION |
WOS类目 | Multidisciplinary Sciences |
WOS研究方向 | Science & Technology - Other Topics |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/179410 |
作者单位 | 1.Indiana Univ, Dept Geog, Bloomington, IN 47405 USA; 2.Santa Clara Univ, Dept Environm Studies & Sci, Santa Clara, CA 95053 USA; 3.Santa Clara Univ, Dept Civil Engn, Santa Clara, CA 95053 USA |
推荐引用方式 GB/T 7714 | Ficklin, Darren L.,Stewart, Iris T.,Maurer, Edwin P.. Climate Change Impacts on Streamflow and Subbasin-Scale Hydrology in the Upper Colorado River Basin[J],2013,8(8). |
APA | Ficklin, Darren L.,Stewart, Iris T.,&Maurer, Edwin P..(2013).Climate Change Impacts on Streamflow and Subbasin-Scale Hydrology in the Upper Colorado River Basin.PLOS ONE,8(8). |
MLA | Ficklin, Darren L.,et al."Climate Change Impacts on Streamflow and Subbasin-Scale Hydrology in the Upper Colorado River Basin".PLOS ONE 8.8(2013). |
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