Improving daily precipitation estimates for the Qinghai‐Tibetan plateau based on environmental similarity

Due to the scarcity of gauge observations and inaccuracy of satellite estimation, obtaining reliable daily precipitation estimates over the Qinghai‐Tibetan Plateau (QTP) remains challenging. In this article, an integrated scheme is developed based on the assumption that in a specific climatic region...

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Veröffentlicht in:International journal of climatology 2020-10, Vol.40 (12), p.5368-5388
Hauptverfasser: Wang, Yudan, Kong, Yunfeng, Chen, Hao, Zhao, Lin
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creator Wang, Yudan
Kong, Yunfeng
Chen, Hao
Zhao, Lin
description Due to the scarcity of gauge observations and inaccuracy of satellite estimation, obtaining reliable daily precipitation estimates over the Qinghai‐Tibetan Plateau (QTP) remains challenging. In this article, an integrated scheme is developed based on the assumption that in a specific climatic region, the similarity of environmental conditions related to precipitation (SEP) in two locations is positively correlated to the similarities of occurrence and magnitude of precipitation between them. First, the QTP was divided into the northwestern arid, middle semi‐arid/semi‐humid, and southeastern humid climatic sub‐regions by grouping analysis. Second, based on modified weighted k‐nearest neighbour model, daily precipitation of target locations in these climatic sub‐regions were predicted by weighted regression of a group of gauge observations that have the largest SEP with the target locations. SEP was calculated by the following auxiliary environmental factors: longitude, latitude, elevation, Normalized Difference Vegetation Index, relative humidity, and CMORPH (Climate Prediction Center's morphing technique) daily precipitation estimates (original CMORPH). The validation results demonstrate the effectiveness of the proposed scheme. Compared with the original CMORPH and PDF‐calibrated CMORPH (CMORPH calibrated by probability density function matching plus optimal interpolation method) at daily, monthly, and yearly scales, the scheme improves the rain/no rain detection capacity and the accuracy of daily precipitation estimates. In addition, the daily precipitation estimates obtained from this scheme can present significant discrimination over specific geographic units, particularly the Qaidam Basin, the great bend of the Brahmaputra River, and Hengduan Mountain. Daily precipitation estimates derived from remote sensing or fused by gauge observation and remote sensing products are inaccurate over the Qinghai‐Tibet plateau (QTP) due to the low quality of remote sensing and the scarcity of gauge observations. Calibration model using auxiliary environmental factors, like regression models, can only be effective at monthly scale. Using a weighted k‐nearest neighbour model revised by the similarity of environmental conditions, an integrated scheme developed here can improve the daily precipitation estimates over the QTP.
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In this article, an integrated scheme is developed based on the assumption that in a specific climatic region, the similarity of environmental conditions related to precipitation (SEP) in two locations is positively correlated to the similarities of occurrence and magnitude of precipitation between them. First, the QTP was divided into the northwestern arid, middle semi‐arid/semi‐humid, and southeastern humid climatic sub‐regions by grouping analysis. Second, based on modified weighted k‐nearest neighbour model, daily precipitation of target locations in these climatic sub‐regions were predicted by weighted regression of a group of gauge observations that have the largest SEP with the target locations. SEP was calculated by the following auxiliary environmental factors: longitude, latitude, elevation, Normalized Difference Vegetation Index, relative humidity, and CMORPH (Climate Prediction Center's morphing technique) daily precipitation estimates (original CMORPH). The validation results demonstrate the effectiveness of the proposed scheme. Compared with the original CMORPH and PDF‐calibrated CMORPH (CMORPH calibrated by probability density function matching plus optimal interpolation method) at daily, monthly, and yearly scales, the scheme improves the rain/no rain detection capacity and the accuracy of daily precipitation estimates. In addition, the daily precipitation estimates obtained from this scheme can present significant discrimination over specific geographic units, particularly the Qaidam Basin, the great bend of the Brahmaputra River, and Hengduan Mountain. Daily precipitation estimates derived from remote sensing or fused by gauge observation and remote sensing products are inaccurate over the Qinghai‐Tibet plateau (QTP) due to the low quality of remote sensing and the scarcity of gauge observations. Calibration model using auxiliary environmental factors, like regression models, can only be effective at monthly scale. Using a weighted k‐nearest neighbour model revised by the similarity of environmental conditions, an integrated scheme developed here can improve the daily precipitation estimates over the QTP.</description><identifier>ISSN: 0899-8418</identifier><identifier>EISSN: 1097-0088</identifier><identifier>DOI: 10.1002/joc.6523</identifier><language>eng</language><publisher>Chichester, UK: John Wiley &amp; Sons, Ltd</publisher><subject>Arid regions ; Atmospheric precipitations ; Climate and vegetation ; Climate prediction ; Climatic indexes ; Daily ; Daily precipitation ; daily precipitation estimates ; Elevation ; Environmental conditions ; Environmental factors ; Environmental impact ; Estimates ; Humid climates ; Interpolation ; Locations (working) ; Morphing ; Mountains ; Normalized difference vegetative index ; Precipitation ; Precipitation estimation ; Probability density function ; Probability density functions ; Probability theory ; Rain ; Rainfall ; Regression analysis ; Relative humidity ; Satellite observation ; Similarity ; Statistical analysis ; the Qinghai‐Tibetan plateau ; Vegetation index</subject><ispartof>International journal of climatology, 2020-10, Vol.40 (12), p.5368-5388</ispartof><rights>2020 Royal Meteorological Society</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c2933-1a790302f9a9bf72dcbaf48c33aa0797fef81e648c39f3534a891e3ea052f8673</citedby><cites>FETCH-LOGICAL-c2933-1a790302f9a9bf72dcbaf48c33aa0797fef81e648c39f3534a891e3ea052f8673</cites><orcidid>0000-0002-3528-116X</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2Fjoc.6523$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2Fjoc.6523$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>315,781,785,1418,27926,27927,45576,45577</link.rule.ids></links><search><creatorcontrib>Wang, Yudan</creatorcontrib><creatorcontrib>Kong, Yunfeng</creatorcontrib><creatorcontrib>Chen, Hao</creatorcontrib><creatorcontrib>Zhao, Lin</creatorcontrib><title>Improving daily precipitation estimates for the Qinghai‐Tibetan plateau based on environmental similarity</title><title>International journal of climatology</title><description>Due to the scarcity of gauge observations and inaccuracy of satellite estimation, obtaining reliable daily precipitation estimates over the Qinghai‐Tibetan Plateau (QTP) remains challenging. In this article, an integrated scheme is developed based on the assumption that in a specific climatic region, the similarity of environmental conditions related to precipitation (SEP) in two locations is positively correlated to the similarities of occurrence and magnitude of precipitation between them. First, the QTP was divided into the northwestern arid, middle semi‐arid/semi‐humid, and southeastern humid climatic sub‐regions by grouping analysis. Second, based on modified weighted k‐nearest neighbour model, daily precipitation of target locations in these climatic sub‐regions were predicted by weighted regression of a group of gauge observations that have the largest SEP with the target locations. SEP was calculated by the following auxiliary environmental factors: longitude, latitude, elevation, Normalized Difference Vegetation Index, relative humidity, and CMORPH (Climate Prediction Center's morphing technique) daily precipitation estimates (original CMORPH). The validation results demonstrate the effectiveness of the proposed scheme. Compared with the original CMORPH and PDF‐calibrated CMORPH (CMORPH calibrated by probability density function matching plus optimal interpolation method) at daily, monthly, and yearly scales, the scheme improves the rain/no rain detection capacity and the accuracy of daily precipitation estimates. In addition, the daily precipitation estimates obtained from this scheme can present significant discrimination over specific geographic units, particularly the Qaidam Basin, the great bend of the Brahmaputra River, and Hengduan Mountain. Daily precipitation estimates derived from remote sensing or fused by gauge observation and remote sensing products are inaccurate over the Qinghai‐Tibet plateau (QTP) due to the low quality of remote sensing and the scarcity of gauge observations. Calibration model using auxiliary environmental factors, like regression models, can only be effective at monthly scale. Using a weighted k‐nearest neighbour model revised by the similarity of environmental conditions, an integrated scheme developed here can improve the daily precipitation estimates over the QTP.</description><subject>Arid regions</subject><subject>Atmospheric precipitations</subject><subject>Climate and vegetation</subject><subject>Climate prediction</subject><subject>Climatic indexes</subject><subject>Daily</subject><subject>Daily precipitation</subject><subject>daily precipitation estimates</subject><subject>Elevation</subject><subject>Environmental conditions</subject><subject>Environmental factors</subject><subject>Environmental impact</subject><subject>Estimates</subject><subject>Humid climates</subject><subject>Interpolation</subject><subject>Locations (working)</subject><subject>Morphing</subject><subject>Mountains</subject><subject>Normalized difference vegetative index</subject><subject>Precipitation</subject><subject>Precipitation estimation</subject><subject>Probability density function</subject><subject>Probability density functions</subject><subject>Probability theory</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Regression analysis</subject><subject>Relative humidity</subject><subject>Satellite observation</subject><subject>Similarity</subject><subject>Statistical analysis</subject><subject>the Qinghai‐Tibetan plateau</subject><subject>Vegetation index</subject><issn>0899-8418</issn><issn>1097-0088</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><recordid>eNp10M1KAzEQB_AgCtYq-AgBL1625mN3kxyl-FEpFKGel9ltYlO3u2uSVvbmI_iMPolZ69XTwPCbGf6D0CUlE0oIu9m01STPGD9CI0qUSAiR8hiNiFQqkSmVp-jM-w0hRCmaj9DbbNu5dm-bV7wCW_e4c7qynQ0QbNtg7YPdQtAem9bhsNb4OdI12O_Pr6UtdYAGd3UEsMMleL3Cw1Czt65ttroJUGNvt7YGZ0N_jk4M1F5f_NUxerm_W04fk_niYTa9nScVU5wnFIQinDCjQJVGsFVVgkllxTkAEUoYbSTV-dBRhmc8Bamo5hpIxozMBR-jq8PemOx9FyMUm3bnmniyYGkqRJ5ljER1fVCVa7132hSdi1ldX1BSDK-MU1UxvDLS5EA_bK37f13xtJj--h85FXfF</recordid><startdate>202010</startdate><enddate>202010</enddate><creator>Wang, Yudan</creator><creator>Kong, Yunfeng</creator><creator>Chen, Hao</creator><creator>Zhao, Lin</creator><general>John Wiley &amp; Sons, Ltd</general><general>Wiley Subscription Services, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0002-3528-116X</orcidid></search><sort><creationdate>202010</creationdate><title>Improving daily precipitation estimates for the Qinghai‐Tibetan plateau based on environmental similarity</title><author>Wang, Yudan ; Kong, Yunfeng ; Chen, Hao ; Zhao, Lin</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c2933-1a790302f9a9bf72dcbaf48c33aa0797fef81e648c39f3534a891e3ea052f8673</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Arid regions</topic><topic>Atmospheric precipitations</topic><topic>Climate and vegetation</topic><topic>Climate prediction</topic><topic>Climatic indexes</topic><topic>Daily</topic><topic>Daily precipitation</topic><topic>daily precipitation estimates</topic><topic>Elevation</topic><topic>Environmental conditions</topic><topic>Environmental factors</topic><topic>Environmental impact</topic><topic>Estimates</topic><topic>Humid climates</topic><topic>Interpolation</topic><topic>Locations (working)</topic><topic>Morphing</topic><topic>Mountains</topic><topic>Normalized difference vegetative index</topic><topic>Precipitation</topic><topic>Precipitation estimation</topic><topic>Probability density function</topic><topic>Probability density functions</topic><topic>Probability theory</topic><topic>Rain</topic><topic>Rainfall</topic><topic>Regression analysis</topic><topic>Relative humidity</topic><topic>Satellite observation</topic><topic>Similarity</topic><topic>Statistical analysis</topic><topic>the Qinghai‐Tibetan plateau</topic><topic>Vegetation index</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Wang, Yudan</creatorcontrib><creatorcontrib>Kong, Yunfeng</creatorcontrib><creatorcontrib>Chen, Hao</creatorcontrib><creatorcontrib>Zhao, Lin</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><jtitle>International journal of climatology</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Wang, Yudan</au><au>Kong, Yunfeng</au><au>Chen, Hao</au><au>Zhao, Lin</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Improving daily precipitation estimates for the Qinghai‐Tibetan plateau based on environmental similarity</atitle><jtitle>International journal of climatology</jtitle><date>2020-10</date><risdate>2020</risdate><volume>40</volume><issue>12</issue><spage>5368</spage><epage>5388</epage><pages>5368-5388</pages><issn>0899-8418</issn><eissn>1097-0088</eissn><abstract>Due to the scarcity of gauge observations and inaccuracy of satellite estimation, obtaining reliable daily precipitation estimates over the Qinghai‐Tibetan Plateau (QTP) remains challenging. In this article, an integrated scheme is developed based on the assumption that in a specific climatic region, the similarity of environmental conditions related to precipitation (SEP) in two locations is positively correlated to the similarities of occurrence and magnitude of precipitation between them. First, the QTP was divided into the northwestern arid, middle semi‐arid/semi‐humid, and southeastern humid climatic sub‐regions by grouping analysis. Second, based on modified weighted k‐nearest neighbour model, daily precipitation of target locations in these climatic sub‐regions were predicted by weighted regression of a group of gauge observations that have the largest SEP with the target locations. SEP was calculated by the following auxiliary environmental factors: longitude, latitude, elevation, Normalized Difference Vegetation Index, relative humidity, and CMORPH (Climate Prediction Center's morphing technique) daily precipitation estimates (original CMORPH). The validation results demonstrate the effectiveness of the proposed scheme. Compared with the original CMORPH and PDF‐calibrated CMORPH (CMORPH calibrated by probability density function matching plus optimal interpolation method) at daily, monthly, and yearly scales, the scheme improves the rain/no rain detection capacity and the accuracy of daily precipitation estimates. In addition, the daily precipitation estimates obtained from this scheme can present significant discrimination over specific geographic units, particularly the Qaidam Basin, the great bend of the Brahmaputra River, and Hengduan Mountain. Daily precipitation estimates derived from remote sensing or fused by gauge observation and remote sensing products are inaccurate over the Qinghai‐Tibet plateau (QTP) due to the low quality of remote sensing and the scarcity of gauge observations. Calibration model using auxiliary environmental factors, like regression models, can only be effective at monthly scale. Using a weighted k‐nearest neighbour model revised by the similarity of environmental conditions, an integrated scheme developed here can improve the daily precipitation estimates over the QTP.</abstract><cop>Chichester, UK</cop><pub>John Wiley &amp; Sons, Ltd</pub><doi>10.1002/joc.6523</doi><tpages>21</tpages><orcidid>https://orcid.org/0000-0002-3528-116X</orcidid></addata></record>
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subjects Arid regions
Atmospheric precipitations
Climate and vegetation
Climate prediction
Climatic indexes
Daily
Daily precipitation
daily precipitation estimates
Elevation
Environmental conditions
Environmental factors
Environmental impact
Estimates
Humid climates
Interpolation
Locations (working)
Morphing
Mountains
Normalized difference vegetative index
Precipitation
Precipitation estimation
Probability density function
Probability density functions
Probability theory
Rain
Rainfall
Regression analysis
Relative humidity
Satellite observation
Similarity
Statistical analysis
the Qinghai‐Tibetan plateau
Vegetation index
title Improving daily precipitation estimates for the Qinghai‐Tibetan plateau based on environmental similarity
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