Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments

For effective planning, design, and management of water resources engineering, the probability distribution of annual streamflow is necessary. The method of L-moments is applied to identify the probability distribution type of annual streamflow in different climatic regions of Canada. In the Pacific...

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Main Authors: Sheng Yue, Chun Wang
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://hdl.handle.net/10.1023/B:WARM.0000049145.37577.87
id ftrepec:oai:RePEc:spr:waterr:v:18:y:2004:i:5:p:425-438
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spelling ftrepec:oai:RePEc:spr:waterr:v:18:y:2004:i:5:p:425-438 2023-05-15T15:06:32+02:00 Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments Sheng Yue Chun Wang http://hdl.handle.net/10.1023/B:WARM.0000049145.37577.87 unknown http://hdl.handle.net/10.1023/B:WARM.0000049145.37577.87 article ftrepec 2020-12-04T13:31:38Z For effective planning, design, and management of water resources engineering, the probability distribution of annual streamflow is necessary. The method of L-moments is applied to identify the probability distribution type of annual streamflow in different climatic regions of Canada. In the Pacific and southern British Columbia mountains (regions 1 and 2), the generalized extreme value (GEV) distribution fits the observations best with the 3-parameter lognormal (LN3) and log Pearson type III (LP3) as potential candidates. In Yukon and northern British Columbia (region 3), the LN3 distribution corresponds to observations best with the LP3 and P3 as potential candidates. In the northwestern forest (region 5), the LP3 distribution matches observations best with the P3 and GEV as potential candidates. In Arctic Tundra (region 10), the 3-parameter Weibull (W3) is the best one with the LN3 and P3 as potential candidates. The P3 distribution provides a best-fit to observations in the Prairies (region 4), northeastern forest (region 6), great Lakes and St. Lawrence (region 7), Atlantic (region 8), and Mackenzie (region 9) with the LN3, LP3, and GEV as potential candidates. Copyright Kluwer Academic Publishers 2004 annual streamflow, discordancy, L-moments, regional frequency analysis, regional hydrology, statistical hydrology Article in Journal/Newspaper Arctic Tundra Yukon RePEc (Research Papers in Economics) Arctic British Columbia ENVELOPE(-125.003,-125.003,54.000,54.000) Canada Columbia Mountains ENVELOPE(-63.852,-63.852,-70.197,-70.197) Pacific Yukon
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description For effective planning, design, and management of water resources engineering, the probability distribution of annual streamflow is necessary. The method of L-moments is applied to identify the probability distribution type of annual streamflow in different climatic regions of Canada. In the Pacific and southern British Columbia mountains (regions 1 and 2), the generalized extreme value (GEV) distribution fits the observations best with the 3-parameter lognormal (LN3) and log Pearson type III (LP3) as potential candidates. In Yukon and northern British Columbia (region 3), the LN3 distribution corresponds to observations best with the LP3 and P3 as potential candidates. In the northwestern forest (region 5), the LP3 distribution matches observations best with the P3 and GEV as potential candidates. In Arctic Tundra (region 10), the 3-parameter Weibull (W3) is the best one with the LN3 and P3 as potential candidates. The P3 distribution provides a best-fit to observations in the Prairies (region 4), northeastern forest (region 6), great Lakes and St. Lawrence (region 7), Atlantic (region 8), and Mackenzie (region 9) with the LN3, LP3, and GEV as potential candidates. Copyright Kluwer Academic Publishers 2004 annual streamflow, discordancy, L-moments, regional frequency analysis, regional hydrology, statistical hydrology
format Article in Journal/Newspaper
author Sheng Yue
Chun Wang
spellingShingle Sheng Yue
Chun Wang
Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments
author_facet Sheng Yue
Chun Wang
author_sort Sheng Yue
title Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments
title_short Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments
title_full Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments
title_fullStr Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments
title_full_unstemmed Possible Regional Probability Distribution Type of Canadian Annual Streamflow by L-moments
title_sort possible regional probability distribution type of canadian annual streamflow by l-moments
url http://hdl.handle.net/10.1023/B:WARM.0000049145.37577.87
long_lat ENVELOPE(-125.003,-125.003,54.000,54.000)
ENVELOPE(-63.852,-63.852,-70.197,-70.197)
geographic Arctic
British Columbia
Canada
Columbia Mountains
Pacific
Yukon
geographic_facet Arctic
British Columbia
Canada
Columbia Mountains
Pacific
Yukon
genre Arctic
Tundra
Yukon
genre_facet Arctic
Tundra
Yukon
op_relation http://hdl.handle.net/10.1023/B:WARM.0000049145.37577.87
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