کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
6411019 1332887 2015 11 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
A recursive multi-scaling approach to regional flood frequency analysis
ترجمه فارسی عنوان
رویکرد مقیاس پذیر چندگانه به تجزیه و تحلیل فرکانس سیلاب منطقه ای
کلمات کلیدی
تجزیه و تحلیل فرکانس سیلاب منطقه ای، مقیاس ساده چند پوسته شدن، ایالت ایالت ایالت، رویکرد رویکرد منطقه ای،
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات فرآیندهای سطح زمین
چکیده انگلیسی


- Recursive multi-scaling (RMS) approach to regional frequency analysis is proposed.
- RMS approach is shown to be effective by application to watersheds in USA.
- RMS outperforms widely used simple-, multi-scaling and index-flood approaches.

SummaryScaling approaches are widely used by hydrologists for Regional Frequency Analysis (RFA) of floods at ungauged/sparsely gauged site(s) in river basins. This paper proposes a Recursive Multi-scaling (RMS) approach to RFA that overcomes limitations of conventional simple- and multi-scaling approaches. The approach involves identification of a separate set of attributes corresponding to each of the sites (being considered in the study area/region) in a recursive manner according to their importance, and utilizing those attributes to construct effective regional regression relationships to estimate statistical raw moments (SMs) of peak flows. The SMs are then utilized to arrive at parameters of flood frequency distribution and quantile estimate(s) corresponding to target return period(s). Effectiveness of the RMS approach in arriving at flood quantile estimates for ungauged sites is demonstrated through leave-one-out cross-validation experiment on watersheds in Indiana State, USA. Results indicate that the approach outperforms index-flood based Region-of-Influence approach, simple- and multi-scaling approaches and a multiple linear regression method.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Journal of Hydrology - Volume 529, Part 1, October 2015, Pages 373-383
نویسندگان
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