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DOI | 10.1175/JHM-D-15-0216.1 |
Effects of Urbanization and Climate Change on Peak Flows over the San Antonio River Basin, Texas | |
Zhao, Gang; Gao, Huilin; Cuo, Lan | |
通讯作者 | Gao, HL (通讯作者) |
发表日期 | 2016 |
ISSN | 1525-755X |
EISSN | 1525-7541 |
起始页码 | 2371 |
结束页码 | 2389 |
卷号 | 17期号:9 |
英文摘要 | A thorough understanding of the peak flows under urbanization and climate change-with the associated uncertainties-is indispensable for mitigating the negative social, economic, and environmental impacts from flooding. In this paper, a case study was conducted by applying the Distributed Hydrology Soil Vegetation Model (DHSVM) to the San Antonio River basin (SARB), Texas. Historical and future land-cover maps were assembled to represent the urbanization process. Future climate and its uncertainties were represented by a series of designed scenarios using the Change Factor (CF) method. The factors were calculated by comparing the model ensemble from phase 5 of the Coupled Model Intercomparison Project (CMIP5) with baseline historical climatology during two future periods (2020-49, period 1; 2070-99, period 2). It was found that with urban impervious areas increasing alone, annual peak flows may increase from 601 (period 1) to 885 m(3) s(-1) (period 2). With regard to climate change, annual peak flows driven by forcings from maximum, median, and minimum CFs under four representative concentration pathways (RCPs) were analyzed. While the median values of future annual peak flows-forced by the median CF values-are very similar to the baseline under all RCPs, in each case the uncertainty range (calculated as the difference between annual peak flows driven by the maximum and minimum CFs) is very large. When urbanization and climate change coevolve, these averaged annual peak flows from the four RCPs will increase from 447 (period 1) to 707 m(3) s(-1) (period 2), with the uncertainties associated with climate change more than 3 times greater than those from urbanization. |
关键词 | CONTERMINOUS UNITED-STATESLAND-COVER DATABASEUNCERTAINTY SOURCESVEGETATION MODELFLOOD FREQUENCYLARGE ENSEMBLECHANGE IMPACTSRUNOFFPRECIPITATIONEVENTS |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000385419800002 |
来源期刊 | JOURNAL OF HYDROMETEOROLOGY |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258671 |
推荐引用方式 GB/T 7714 | Zhao, Gang,Gao, Huilin,Cuo, Lan. Effects of Urbanization and Climate Change on Peak Flows over the San Antonio River Basin, Texas[J]. 中国科学院青藏高原研究所,2016,17(9). |
APA | Zhao, Gang,Gao, Huilin,&Cuo, Lan.(2016).Effects of Urbanization and Climate Change on Peak Flows over the San Antonio River Basin, Texas.JOURNAL OF HYDROMETEOROLOGY,17(9). |
MLA | Zhao, Gang,et al."Effects of Urbanization and Climate Change on Peak Flows over the San Antonio River Basin, Texas".JOURNAL OF HYDROMETEOROLOGY 17.9(2016). |
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