Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological Simulation
The hydrology response was studied considering the established fact of land use change in Dapoling basin. The whole period was divided into two (1965−1985 and 1986−2012) according to the major land use and land cover change in this region. Xinanjiang model was used to simulate di...
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MDPI AG
2019-04-01
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| Series: | Water |
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| Online Access: | https://www.mdpi.com/2073-4441/11/4/866 |
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doaj-976fb675e53242d38c242f410332d6e82020-11-25T01:05:48ZengMDPI AGWater2073-44412019-04-0111486610.3390/w11040866w11040866Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological SimulationMinmin Zhou0Simin Qu1Xueqiu Chen2Peng Shi3Shijin Xu4Hongyu Chen5Huiyan Zhou6Jianfeng Gou7State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaState Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaState Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Hohai University, Nanjing 210098, ChinaHydrological Bureau, The Huai River Commission of the Ministry of Water Resources, Bengbu 233040, ChinaHydrological Bureau, The Huai River Commission of the Ministry of Water Resources, Bengbu 233040, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaCollege of Hydrology and Water Resources, Hohai University, Nanjing 210098, ChinaThe hydrology response was studied considering the established fact of land use change in Dapoling basin. The whole period was divided into two (1965−1985 and 1986−2012) according to the major land use and land cover change in this region. Xinanjiang model was used to simulate discharge data in the two periods. The hydrologic response to the change could be evaluated by inspecting the response of model parameters and flood elements. The results show that the lag time varied, and the hydrologic elements including the mean runoff depth, flood peak and kurtosis coefficient varied with the rainfall depth. This result is significant for studying the response of runoff characteristic from land use and land cover change.https://www.mdpi.com/2073-4441/11/4/866mean basin lag timeland use and land cover changerunoff characteristicsDapoling basin |
| collection |
DOAJ |
| language |
English |
| format |
Article |
| sources |
DOAJ |
| author |
Minmin Zhou Simin Qu Xueqiu Chen Peng Shi Shijin Xu Hongyu Chen Huiyan Zhou Jianfeng Gou |
| spellingShingle |
Minmin Zhou Simin Qu Xueqiu Chen Peng Shi Shijin Xu Hongyu Chen Huiyan Zhou Jianfeng Gou Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological Simulation Water mean basin lag time land use and land cover change runoff characteristics Dapoling basin |
| author_facet |
Minmin Zhou Simin Qu Xueqiu Chen Peng Shi Shijin Xu Hongyu Chen Huiyan Zhou Jianfeng Gou |
| author_sort |
Minmin Zhou |
| title |
Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological Simulation |
| title_short |
Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological Simulation |
| title_full |
Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological Simulation |
| title_fullStr |
Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological Simulation |
| title_full_unstemmed |
Impact Assessments of Rainfall–Runoff Characteristics Response Based on Land Use Change via Hydrological Simulation |
| title_sort |
impact assessments of rainfall–runoff characteristics response based on land use change via hydrological simulation |
| publisher |
MDPI AG |
| series |
Water |
| issn |
2073-4441 |
| publishDate |
2019-04-01 |
| description |
The hydrology response was studied considering the established fact of land use change in Dapoling basin. The whole period was divided into two (1965−1985 and 1986−2012) according to the major land use and land cover change in this region. Xinanjiang model was used to simulate discharge data in the two periods. The hydrologic response to the change could be evaluated by inspecting the response of model parameters and flood elements. The results show that the lag time varied, and the hydrologic elements including the mean runoff depth, flood peak and kurtosis coefficient varied with the rainfall depth. This result is significant for studying the response of runoff characteristic from land use and land cover change. |
| topic |
mean basin lag time land use and land cover change runoff characteristics Dapoling basin |
| url |
https://www.mdpi.com/2073-4441/11/4/866 |
| work_keys_str_mv |
AT minminzhou impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation AT siminqu impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation AT xueqiuchen impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation AT pengshi impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation AT shijinxu impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation AT hongyuchen impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation AT huiyanzhou impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation AT jianfenggou impactassessmentsofrainfallrunoffcharacteristicsresponsebasedonlandusechangeviahydrologicalsimulation |
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1725193095501316096 |