首页> 外文期刊>Hydrological ProcHydrological Processesrnesses >Hydrologic‐response simulations for the North Fork of Caspar Creek: second‐growth, clear‐cut, new‐growth, and cumulative watershed effect scenarios
【24h】

Hydrologic‐response simulations for the North Fork of Caspar Creek: second‐growth, clear‐cut, new‐growth, and cumulative watershed effect scenarios

机译:卡斯珀河北叉的水文响应模拟:二次生长,明晰切割,新增长和累积分水岭影响情景

获取原文
获取原文并翻译 | 示例
           

摘要

This study demonstrates that comprehensive hydrologic-response simulation can be a useful tool for studying . The simulations reported here were conducted with the Integrated Hydrology Model (InHM). The location of the 473 ha study site is the North Fork of the Caspar Creek Experimental Watershed, near Fort Bragg, California. Existing information from a long-term monitoring programme and new soil-hydraulic property measurements made for this study were used to parameterize InHM. Long-term continuous wet-season simulations were conducted for the North Fork catchments and main stem for second-growth, clear-cut and new-growth scenarios. The simulation results show that the increases and decreases, respectively, for throughfall and potential evapotranspiration related to clear-cutting had quantifiable impacts on the simulated hydrologic response at both the catchment and watershed scales. Model performance was best for the new-growth simulation scenarios. To improve upon the simulations reported here would require additional soil-hydraulic property information from across the study area. Although principally focused on the integrated hydrologic response, the effort reported here demonstrates the potential for characterizing distributed responses with physics-based simulation. The search for a comprehensive understanding of hydrologic response will require both data-intensive discovery and concept-development simulation, from both integrated and distributed perspectives. Copyright © 2013 John Wiley & Sons, Ltd.
机译:这项研究表明,综合的水文响应模拟可以成为研究的有用工具。此处报告的模拟是使用综合水文模型(InHM)进行的。 473公顷研究场地位于加利福尼亚州布拉格堡附近的卡斯珀河实验分水岭的北叉。来自长期监测计划的现有信息以及为此研究而进行的新的土壤-水力性质测量均用于参数化InHM。对北叉集水区和主干进行了长期连续的湿季模拟,以模拟第二次生长,明确和新生长的情况。模拟结果表明,与径流有关的穿透力和潜在蒸散量的增加和减少分别对集水区和集水区尺度的模拟水文响应产生了可量化的影响。对于新增长的模拟场景,模型性能最佳。为了改进此处报告的模拟,需要来自研究区域的其他土壤-水力特性信息。尽管主要集中于综合水文响应,但此处报道的工作证明了利用基于物理的模拟表征分布式响应的潜力。寻求对水文响应的全面了解,需要从综合和分布式的角度进行数据密集型发现和概念发展模拟。版权所有©2013 John Wiley&Sons,Ltd.

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号