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Impacts of Max-Stable Process Areal Exceedance Calculations to Study Area Sampling Density, Surface Network Precipitation Gage Extent and Density, and Model Fitting Method
Max-stable process (MSP) models can be fit to data collected over a spatial domain to estimate areal-based exceedances while accounting for spatial dependence in extremes. They have theoretical grounding within the framework of extreme value theory (EVT). In this work, we fit MSP models to three-day...
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Published in: | Hydrology 2023-06, Vol.10 (6), p.121 |
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description | Max-stable process (MSP) models can be fit to data collected over a spatial domain to estimate areal-based exceedances while accounting for spatial dependence in extremes. They have theoretical grounding within the framework of extreme value theory (EVT). In this work, we fit MSP models to three-day duration cool season precipitation maxima in the Willamette River Basin (WRB) of Oregon and to 48 h mid-latitude cyclone precipitation annual maxima in the Upper Trinity River Basin (TRB) of Texas. In total, 14 MSP models were fit (seven based on the WRB data and seven based on the TRB data). These MSP model fits were developed and applied to explore how user choices of study area sampling density, gage extent, and model fitting method impact areal precipitation-frequency calculations. The impacts of gage density were also evaluated. The development of each MSP involved the application of a recently introduced trend surface modeling methodology. Significant reductions in computing times were achieved, with little loss in accuracy, applying random sample subsets rather than the entire grid when calculating areal exceedances for the Cougar dam study area in the WRB. Explorations of gage extent revealed poor consistency among the TRB MSPs with modeling the generalized extreme value (GEV) marginal distribution scale parameter. The gauge density study revealed the robustness of the trend surface modeling methodology. Regardless of the fitting method, the final GEV shape parameter estimates for all fourteen MSPs were greater than their prescribed initial values which were obtained from spatial GEV fits that assumed independence among the extremes. When two MSP models only differed by their selected fitting method, notable differences were observed with their dependence and trend surface parameter estimates and resulting areal exceedances calculations. |
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Significant reductions in computing times were achieved, with little loss in accuracy, applying random sample subsets rather than the entire grid when calculating areal exceedances for the Cougar dam study area in the WRB. Explorations of gage extent revealed poor consistency among the TRB MSPs with modeling the generalized extreme value (GEV) marginal distribution scale parameter. The gauge density study revealed the robustness of the trend surface modeling methodology. Regardless of the fitting method, the final GEV shape parameter estimates for all fourteen MSPs were greater than their prescribed initial values which were obtained from spatial GEV fits that assumed independence among the extremes. When two MSP models only differed by their selected fitting method, notable differences were observed with their dependence and trend surface parameter estimates and resulting areal exceedances calculations.</description><identifier>ISSN: 2306-5338</identifier><identifier>EISSN: 2306-5338</identifier><identifier>DOI: 10.3390/hydrology10060121</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Annual precipitation ; areal exceedance ; Areal precipitation ; Basins ; Cool season ; Cyclones ; Dams ; Data collection ; Datasets ; Density ; Electronic data processing ; Estimates ; extreme precipitation ; Extreme value theory ; Extreme values ; Extreme weather ; Floods ; Hydrology ; Levees & battures ; Mathematical models ; max-stable process ; Maxima ; Methods ; Modelling ; Parameter estimation ; Precipitation ; Precipitation (Meteorology) ; Random sampling ; River basins ; Rivers ; Sampling ; Seasons ; spatial dependence ; trend surface</subject><ispartof>Hydrology, 2023-06, Vol.10 (6), p.121</ispartof><rights>COPYRIGHT 2023 MDPI AG</rights><rights>2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). 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They have theoretical grounding within the framework of extreme value theory (EVT). In this work, we fit MSP models to three-day duration cool season precipitation maxima in the Willamette River Basin (WRB) of Oregon and to 48 h mid-latitude cyclone precipitation annual maxima in the Upper Trinity River Basin (TRB) of Texas. In total, 14 MSP models were fit (seven based on the WRB data and seven based on the TRB data). These MSP model fits were developed and applied to explore how user choices of study area sampling density, gage extent, and model fitting method impact areal precipitation-frequency calculations. The impacts of gage density were also evaluated. The development of each MSP involved the application of a recently introduced trend surface modeling methodology. Significant reductions in computing times were achieved, with little loss in accuracy, applying random sample subsets rather than the entire grid when calculating areal exceedances for the Cougar dam study area in the WRB. Explorations of gage extent revealed poor consistency among the TRB MSPs with modeling the generalized extreme value (GEV) marginal distribution scale parameter. The gauge density study revealed the robustness of the trend surface modeling methodology. Regardless of the fitting method, the final GEV shape parameter estimates for all fourteen MSPs were greater than their prescribed initial values which were obtained from spatial GEV fits that assumed independence among the extremes. When two MSP models only differed by their selected fitting method, notable differences were observed with their dependence and trend surface parameter estimates and resulting areal exceedances calculations.</description><subject>Annual precipitation</subject><subject>areal exceedance</subject><subject>Areal precipitation</subject><subject>Basins</subject><subject>Cool season</subject><subject>Cyclones</subject><subject>Dams</subject><subject>Data collection</subject><subject>Datasets</subject><subject>Density</subject><subject>Electronic data processing</subject><subject>Estimates</subject><subject>extreme precipitation</subject><subject>Extreme value theory</subject><subject>Extreme values</subject><subject>Extreme weather</subject><subject>Floods</subject><subject>Hydrology</subject><subject>Levees & battures</subject><subject>Mathematical models</subject><subject>max-stable process</subject><subject>Maxima</subject><subject>Methods</subject><subject>Modelling</subject><subject>Parameter estimation</subject><subject>Precipitation</subject><subject>Precipitation (Meteorology)</subject><subject>Random sampling</subject><subject>River basins</subject><subject>Rivers</subject><subject>Sampling</subject><subject>Seasons</subject><subject>spatial dependence</subject><subject>trend surface</subject><issn>2306-5338</issn><issn>2306-5338</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNplkt1uEzEQhVcIJKrSB-DOErdsGdub_bmMQlsiNQUpcL2atcdbh8062F7RfSZeEidBBQnNxYxH53w6kifL3nK4lrKBD4-z9m5w_cwBSuCCv8guhIQyX0hZv_xnfp1dhbADAMF5XQBcZL_W-wOqGJgzbINP-TZiNxD74p2iENjSEw7s5kkRaRwVsRUOahowWjcGFh3bxknPJxnb4v4w2LFnH2kMNs7v2XbyBpPpgeJP578nKil7sPFkZ3fYU0JHGiPDUf-1HR8bp2lgtzbGI3FD8dHpN9krg0Ogqz_9Mvt2e_N19Sm__3y3Xi3vc1UIHnPdFA2VKKQBQaIosJKIhWokdB2qDhZkJKhOaTCEKJQ0TVXVHU9lFqhreZmtz1ztcNcevN2jn1uHtj0tnO9b9NGqgVqsgauSV7KSvOBaoizrRnZdJUsSDUBivTuzDt79mCjEducmP6b4rahFU6efKGVSXZ9VPSaoHY2LHlUqTXur3EjGpv2yWtSiLpryGJGfDcq7EDyZ55gc2uNNtP_dhPwNQ_utow</recordid><startdate>20230601</startdate><enddate>20230601</enddate><creator>Skahill, Brian</creator><creator>Smith, Cole Haden</creator><creator>Russell, Brook T.</creator><creator>England, John F.</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7X2</scope><scope>8FE</scope><scope>8FH</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H98</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M0K</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>DOA</scope><orcidid>https://orcid.org/0000-0002-2164-0301</orcidid></search><sort><creationdate>20230601</creationdate><title>Impacts of Max-Stable Process Areal Exceedance Calculations to Study Area Sampling Density, Surface Network Precipitation Gage Extent and Density, and Model Fitting Method</title><author>Skahill, Brian ; Smith, Cole Haden ; Russell, Brook T. ; England, John F.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c421t-d949e6a23f02e244a73aa4c930bbacb05ef30cbcd0feaa2c3f9778b1b1bf5ad83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Annual precipitation</topic><topic>areal exceedance</topic><topic>Areal precipitation</topic><topic>Basins</topic><topic>Cool season</topic><topic>Cyclones</topic><topic>Dams</topic><topic>Data collection</topic><topic>Datasets</topic><topic>Density</topic><topic>Electronic data processing</topic><topic>Estimates</topic><topic>extreme precipitation</topic><topic>Extreme value theory</topic><topic>Extreme values</topic><topic>Extreme weather</topic><topic>Floods</topic><topic>Hydrology</topic><topic>Levees & battures</topic><topic>Mathematical models</topic><topic>max-stable process</topic><topic>Maxima</topic><topic>Methods</topic><topic>Modelling</topic><topic>Parameter estimation</topic><topic>Precipitation</topic><topic>Precipitation (Meteorology)</topic><topic>Random sampling</topic><topic>River basins</topic><topic>Rivers</topic><topic>Sampling</topic><topic>Seasons</topic><topic>spatial dependence</topic><topic>trend surface</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Skahill, Brian</creatorcontrib><creatorcontrib>Smith, Cole Haden</creatorcontrib><creatorcontrib>Russell, Brook T.</creatorcontrib><creatorcontrib>England, John F.</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Agricultural Science Collection</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Natural Science Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni)</collection><collection>ProQuest Central</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Aquaculture Abstracts</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Agriculture Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>DOAJ Directory of Open Access Journals</collection><jtitle>Hydrology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Skahill, Brian</au><au>Smith, Cole Haden</au><au>Russell, Brook T.</au><au>England, John F.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Impacts of Max-Stable Process Areal Exceedance Calculations to Study Area Sampling Density, Surface Network Precipitation Gage Extent and Density, and Model Fitting Method</atitle><jtitle>Hydrology</jtitle><date>2023-06-01</date><risdate>2023</risdate><volume>10</volume><issue>6</issue><spage>121</spage><pages>121-</pages><issn>2306-5338</issn><eissn>2306-5338</eissn><abstract>Max-stable process (MSP) models can be fit to data collected over a spatial domain to estimate areal-based exceedances while accounting for spatial dependence in extremes. They have theoretical grounding within the framework of extreme value theory (EVT). In this work, we fit MSP models to three-day duration cool season precipitation maxima in the Willamette River Basin (WRB) of Oregon and to 48 h mid-latitude cyclone precipitation annual maxima in the Upper Trinity River Basin (TRB) of Texas. In total, 14 MSP models were fit (seven based on the WRB data and seven based on the TRB data). These MSP model fits were developed and applied to explore how user choices of study area sampling density, gage extent, and model fitting method impact areal precipitation-frequency calculations. The impacts of gage density were also evaluated. The development of each MSP involved the application of a recently introduced trend surface modeling methodology. Significant reductions in computing times were achieved, with little loss in accuracy, applying random sample subsets rather than the entire grid when calculating areal exceedances for the Cougar dam study area in the WRB. Explorations of gage extent revealed poor consistency among the TRB MSPs with modeling the generalized extreme value (GEV) marginal distribution scale parameter. The gauge density study revealed the robustness of the trend surface modeling methodology. Regardless of the fitting method, the final GEV shape parameter estimates for all fourteen MSPs were greater than their prescribed initial values which were obtained from spatial GEV fits that assumed independence among the extremes. When two MSP models only differed by their selected fitting method, notable differences were observed with their dependence and trend surface parameter estimates and resulting areal exceedances calculations.</abstract><cop>Basel</cop><pub>MDPI AG</pub><doi>10.3390/hydrology10060121</doi><orcidid>https://orcid.org/0000-0002-2164-0301</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Annual precipitation areal exceedance Areal precipitation Basins Cool season Cyclones Dams Data collection Datasets Density Electronic data processing Estimates extreme precipitation Extreme value theory Extreme values Extreme weather Floods Hydrology Levees & battures Mathematical models max-stable process Maxima Methods Modelling Parameter estimation Precipitation Precipitation (Meteorology) Random sampling River basins Rivers Sampling Seasons spatial dependence trend surface |
title | Impacts of Max-Stable Process Areal Exceedance Calculations to Study Area Sampling Density, Surface Network Precipitation Gage Extent and Density, and Model Fitting Method |
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