Simulated runoff responses to land use in the middle and upstream reaches of Taoerhe River basin, Northeast China, in wet, average and dry years
文献类型：期刊论文
| 作者 | Li, Lijuan1; Jiang, Dejuan2 ; Hou, Xiyong2; Li, Jiuyi1
|
| 刊名 | HYDROLOGICAL PROCESSES
 |
| 出版日期 | 2013-11-29 |
| 卷号 | 27期号:24页码:3484-3494 |
| 关键词 | runoff land use change climate conditions precipitation SWAT |
| ISSN号 | 0885-6087 |
| 产权排序 | [Li, Lijuan; Li, Jiuyi] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China; [Jiang, Dejuan; Hou, Xiyong] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Shandong, Peoples R China |
| 通讯作者 | Jiang, DJ (reprint author), Chinese Acad Sci, Yantai Inst Coastal Zone Res, Chunhui Rd 17, Yantai 264003, Shandong, Peoples R China. djjiang@yic.ac.cn |
| 中文摘要 | Study on runoff variations and responses can lay a foundation for flood control, water allocation and integrated river basin management. This study applied the Soil and Water Assessment Tool model to simulate the effects of land use on annual and monthly runoff in the Middle and Upstream Reaches of Taoerhe River basin, Northeast China, under the wet, average and dry climate conditions through scenario analysis. The results showed that from the early 1970s to 2000, land use change with an increase in farmland (17.0%) and decreases in forest (10.6%), grassland (4.6%) and water body (3.1%) caused increases in annual and monthly runoff. This effect was more distinct in the wet season or in the wet year, suggesting that land use change from the early 1970s to 2000 may increase the flood potential in the wet season. Increases in precipitation and air temperature from the average to wet year led to annual and monthly (March and from June to December) runoff increases, while a decrease in precipitation and an increase in air temperature from the average to dry year induced decreases in annual and monthly (all months except March) runoff, and moreover, these effects were more remarkable in the wet season than those in the dry season. Due to the integrated effects of changing land use and climate conditions, the annual runoff increased (decreased) by 70.1mm (25.2mm) or 197.4% (71.0%) from the average to wet (dry) year. In conclusion, climate conditions, especially precipitation, played an important role in runoff variations while land use change was secondary over the study area, and furthermore, the effects of changes in land use and/or climate conditions on monthly runoff were larger in the wet season. Copyright (c) 2012 John Wiley & Sons, Ltd. |
| 英文摘要 | Study on runoff variations and responses can lay a foundation for flood control, water allocation and integrated river basin management. This study applied the Soil and Water Assessment Tool model to simulate the effects of land use on annual and monthly runoff in the Middle and Upstream Reaches of Taoerhe River basin, Northeast China, under the wet, average and dry climate conditions through scenario analysis. The results showed that from the early 1970s to 2000, land use change with an increase in farmland (17.0%) and decreases in forest (10.6%), grassland (4.6%) and water body (3.1%) caused increases in annual and monthly runoff. This effect was more distinct in the wet season or in the wet year, suggesting that land use change from the early 1970s to 2000 may increase the flood potential in the wet season. Increases in precipitation and air temperature from the average to wet year led to annual and monthly (March and from June to December) runoff increases, while a decrease in precipitation and an increase in air temperature from the average to dry year induced decreases in annual and monthly (all months except March) runoff, and moreover, these effects were more remarkable in the wet season than those in the dry season. Due to the integrated effects of changing land use and climate conditions, the annual runoff increased (decreased) by 70.1mm (25.2mm) or 197.4% (71.0%) from the average to wet (dry) year. In conclusion, climate conditions, especially precipitation, played an important role in runoff variations while land use change was secondary over the study area, and furthermore, the effects of changes in land use and/or climate conditions on monthly runoff were larger in the wet season. Copyright (c) 2012 John Wiley & Sons, Ltd. |
| 学科主题 | Water Resources |
| 研究领域[WOS] | Water Resources |
| 关键词[WOS] | CLIMATE-CHANGE ; SWAT MODEL ; HYDROLOGICAL RESPONSE ; UNCERTAINTY ANALYSIS ; NORTHWEST CHINA ; COVER CHANGES ; STORM-RUNOFF ; CATCHMENT ; IMPACTS ; VARIABILITY |
| 收录类别 | SCI |
| 资助信息 | National Natural Science Foundation of China [40571029] |
| 原文出处 | http://dx.doi.org/10.1002/hyp.9481 |
| 语种 | 英语 |
| WOS记录号 | WOS:000325989300011 |
| 公开日期 | 2014-07-08 |
| 源URL | [http://ir.yic.ac.cn/handle/133337/6999]  |
| 专题 | 烟台海岸带研究所_海岸带信息集成与综合管理实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China 2.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Shandong, Peoples R China |
| 推荐引用方式 GB/T 7714 | Li, Lijuan,Jiang, Dejuan,Hou, Xiyong,et al. Simulated runoff responses to land use in the middle and upstream reaches of Taoerhe River basin, Northeast China, in wet, average and dry years[J]. HYDROLOGICAL PROCESSES,2013,27(24):3484-3494. |
| APA | Li, Lijuan,Jiang, Dejuan,Hou, Xiyong,&Li, Jiuyi.(2013).Simulated runoff responses to land use in the middle and upstream reaches of Taoerhe River basin, Northeast China, in wet, average and dry years.HYDROLOGICAL PROCESSES,27(24),3484-3494. |
| MLA | Li, Lijuan,et al."Simulated runoff responses to land use in the middle and upstream reaches of Taoerhe River basin, Northeast China, in wet, average and dry years".HYDROLOGICAL PROCESSES 27.24(2013):3484-3494. |
入库方式： OAI收割
来源：烟台海岸带研究所
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