$ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models
Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and...
Ausführliche Beschreibung
Autor*in: |
Chu, Hone-Jay [verfasserIn] Bilal, Muhammad [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2018 |
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Übergeordnetes Werk: |
Enthalten in: Environmental science and pollution research - Berlin : Springer, 1994, 26(2018), 2 vom: 20. Nov., Seite 1902-1910 |
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Übergeordnetes Werk: |
volume:26 ; year:2018 ; number:2 ; day:20 ; month:11 ; pages:1902-1910 |
Links: |
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DOI / URN: |
10.1007/s11356-018-3763-7 |
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Katalog-ID: |
SPR018865119 |
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100 | 1 | |a Chu, Hone-Jay |e verfasserin |4 aut | |
245 | 1 | 0 | |a $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models |
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520 | |a Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. | ||
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650 | 4 | |a Taiwan |7 (dpeaa)DE-He213 | |
700 | 1 | |a Bilal, Muhammad |e verfasserin |4 aut | |
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10.1007/s11356-018-3763-7 doi (DE-627)SPR018865119 (SPR)s11356-018-3763-7-e DE-627 ger DE-627 rakwb eng 333.7 690 ASE 43.00 bkl 43.50 bkl 58.50 bkl Chu, Hone-Jay verfasserin aut $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. GTWR (dpeaa)DE-He213 RANSAC (dpeaa)DE-He213 PM (dpeaa)DE-He213 AOD (dpeaa)DE-He213 DTB (dpeaa)DE-He213 Taiwan (dpeaa)DE-He213 Bilal, Muhammad verfasserin aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 26(2018), 2 vom: 20. Nov., Seite 1902-1910 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:26 year:2018 number:2 day:20 month:11 pages:1902-1910 https://dx.doi.org/10.1007/s11356-018-3763-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 43.00 ASE 43.50 ASE 58.50 ASE AR 26 2018 2 20 11 1902-1910 |
spelling |
10.1007/s11356-018-3763-7 doi (DE-627)SPR018865119 (SPR)s11356-018-3763-7-e DE-627 ger DE-627 rakwb eng 333.7 690 ASE 43.00 bkl 43.50 bkl 58.50 bkl Chu, Hone-Jay verfasserin aut $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. GTWR (dpeaa)DE-He213 RANSAC (dpeaa)DE-He213 PM (dpeaa)DE-He213 AOD (dpeaa)DE-He213 DTB (dpeaa)DE-He213 Taiwan (dpeaa)DE-He213 Bilal, Muhammad verfasserin aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 26(2018), 2 vom: 20. Nov., Seite 1902-1910 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:26 year:2018 number:2 day:20 month:11 pages:1902-1910 https://dx.doi.org/10.1007/s11356-018-3763-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 43.00 ASE 43.50 ASE 58.50 ASE AR 26 2018 2 20 11 1902-1910 |
allfields_unstemmed |
10.1007/s11356-018-3763-7 doi (DE-627)SPR018865119 (SPR)s11356-018-3763-7-e DE-627 ger DE-627 rakwb eng 333.7 690 ASE 43.00 bkl 43.50 bkl 58.50 bkl Chu, Hone-Jay verfasserin aut $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. GTWR (dpeaa)DE-He213 RANSAC (dpeaa)DE-He213 PM (dpeaa)DE-He213 AOD (dpeaa)DE-He213 DTB (dpeaa)DE-He213 Taiwan (dpeaa)DE-He213 Bilal, Muhammad verfasserin aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 26(2018), 2 vom: 20. Nov., Seite 1902-1910 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:26 year:2018 number:2 day:20 month:11 pages:1902-1910 https://dx.doi.org/10.1007/s11356-018-3763-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 43.00 ASE 43.50 ASE 58.50 ASE AR 26 2018 2 20 11 1902-1910 |
allfieldsGer |
10.1007/s11356-018-3763-7 doi (DE-627)SPR018865119 (SPR)s11356-018-3763-7-e DE-627 ger DE-627 rakwb eng 333.7 690 ASE 43.00 bkl 43.50 bkl 58.50 bkl Chu, Hone-Jay verfasserin aut $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. GTWR (dpeaa)DE-He213 RANSAC (dpeaa)DE-He213 PM (dpeaa)DE-He213 AOD (dpeaa)DE-He213 DTB (dpeaa)DE-He213 Taiwan (dpeaa)DE-He213 Bilal, Muhammad verfasserin aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 26(2018), 2 vom: 20. Nov., Seite 1902-1910 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:26 year:2018 number:2 day:20 month:11 pages:1902-1910 https://dx.doi.org/10.1007/s11356-018-3763-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 43.00 ASE 43.50 ASE 58.50 ASE AR 26 2018 2 20 11 1902-1910 |
allfieldsSound |
10.1007/s11356-018-3763-7 doi (DE-627)SPR018865119 (SPR)s11356-018-3763-7-e DE-627 ger DE-627 rakwb eng 333.7 690 ASE 43.00 bkl 43.50 bkl 58.50 bkl Chu, Hone-Jay verfasserin aut $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models 2018 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. GTWR (dpeaa)DE-He213 RANSAC (dpeaa)DE-He213 PM (dpeaa)DE-He213 AOD (dpeaa)DE-He213 DTB (dpeaa)DE-He213 Taiwan (dpeaa)DE-He213 Bilal, Muhammad verfasserin aut Enthalten in Environmental science and pollution research Berlin : Springer, 1994 26(2018), 2 vom: 20. Nov., Seite 1902-1910 (DE-627)320517926 (DE-600)2014192-0 1614-7499 nnns volume:26 year:2018 number:2 day:20 month:11 pages:1902-1910 https://dx.doi.org/10.1007/s11356-018-3763-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_381 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2360 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 43.00 ASE 43.50 ASE 58.50 ASE AR 26 2018 2 20 11 1902-1910 |
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English |
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Enthalten in Environmental science and pollution research 26(2018), 2 vom: 20. Nov., Seite 1902-1910 volume:26 year:2018 number:2 day:20 month:11 pages:1902-1910 |
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Enthalten in Environmental science and pollution research 26(2018), 2 vom: 20. Nov., Seite 1902-1910 volume:26 year:2018 number:2 day:20 month:11 pages:1902-1910 |
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Environmental science and pollution research |
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Chu, Hone-Jay @@aut@@ Bilal, Muhammad @@aut@@ |
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2018-11-20T00:00:00Z |
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<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">SPR018865119</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20220111063314.0</controlfield><controlfield tag="007">cr uuu---uuuuu</controlfield><controlfield tag="008">201006s2018 xx |||||o 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11356-018-3763-7</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)SPR018865119</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(SPR)s11356-018-3763-7-e</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">333.7</subfield><subfield code="a">690</subfield><subfield code="q">ASE</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.00</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">43.50</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">58.50</subfield><subfield code="2">bkl</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Chu, Hone-Jay</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">$ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2018</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. 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|
author |
Chu, Hone-Jay |
spellingShingle |
Chu, Hone-Jay ddc 333.7 bkl 43.00 bkl 43.50 bkl 58.50 misc GTWR misc RANSAC misc PM misc AOD misc DTB misc Taiwan $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models |
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333 - Economics of land & energy 690 - Buildings |
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1614-7499 |
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333.7 690 ASE 43.00 bkl 43.50 bkl 58.50 bkl $ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models GTWR (dpeaa)DE-He213 RANSAC (dpeaa)DE-He213 PM (dpeaa)DE-He213 AOD (dpeaa)DE-He213 DTB (dpeaa)DE-He213 Taiwan (dpeaa)DE-He213 |
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ddc 333.7 bkl 43.00 bkl 43.50 bkl 58.50 misc GTWR misc RANSAC misc PM misc AOD misc DTB misc Taiwan |
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ddc 333.7 bkl 43.00 bkl 43.50 bkl 58.50 misc GTWR misc RANSAC misc PM misc AOD misc DTB misc Taiwan |
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ddc 333.7 bkl 43.00 bkl 43.50 bkl 58.50 misc GTWR misc RANSAC misc PM misc AOD misc DTB misc Taiwan |
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Elektronische Aufsätze Aufsätze Elektronische Ressource |
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Environmental science and pollution research |
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320517926 |
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Environmental science and pollution research |
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title |
$ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models |
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(DE-627)SPR018865119 (SPR)s11356-018-3763-7-e |
title_full |
$ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models |
author_sort |
Chu, Hone-Jay |
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Environmental science and pollution research |
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Environmental science and pollution research |
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Chu, Hone-Jay Bilal, Muhammad |
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Elektronische Aufsätze |
author-letter |
Chu, Hone-Jay |
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10.1007/s11356-018-3763-7 |
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$ pm_{2.5} $ mapping using integrated geographically temporally weighted regression (gtwr) and random sample consensus (ransac) models |
title_auth |
$ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models |
abstract |
Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. |
abstractGer |
Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. |
abstract_unstemmed |
Abstract An uncertainty in the relationship between aerosol optical depth (AOD) and fine particulate matter ($ PM_{2.5} $) comes from the uncertainty of AOD by aerosol models and the estimated surface reflectance, a mismatch in spatiotemporal resolution, integration of AOD and $ PM_{2.5} $ data, and data modeling. In this study, an integrated geographically temporally weighted regression (GTWR) and RANdom SAmple Consensus (RANSAC) models, which provide fine goodness-of-fit between observed $ PM_{2.5} $ and AOD data, were used for mapping of $ PM_{2.5} $ over Taiwan for the year 2014. For this, dark target (DT) AOD observations at 3-km resolution ($ DT_{3K} $) only for high-quality assurance flag (QA = 3) were obtained from the scientific data set (SDS) “Optical_Depth_Land_And_Ocean”. AOD observations were also obtained from the merged DT and DB (deep blue) product ($ DTB_{3K} $) which was generated using the simplified merge scheme (SMS), i.e., using an average of the DT and DB highest quality AOD retrievals or the available one. The GTWR model integrated with RANSAC can use the effective sampling and fitting to overcome the estimation problem of AOD-$ PM_{2.5} $ with the uncertainty and outliers of observation data. Results showed that the model dealing with spatiotemporal heterogeneity and uncertainty is a powerful tool to infer patterns of $ PM_{2.5} $ from a RANSAC subset samples. Moreover, spatial variability and hotspot analysis were applied after $ PM_{2.5} $ mapping. The hotspot and spatial variability of $ PM_{2.5} $ maps can give us a summary of the spatiotemporal patterns of $ PM_{2.5} $ variations. |
collection_details |
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container_issue |
2 |
title_short |
$ PM_{2.5} $ mapping using integrated geographically temporally weighted regression (GTWR) and random sample consensus (RANSAC) models |
url |
https://dx.doi.org/10.1007/s11356-018-3763-7 |
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Bilal, Muhammad |
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up_date |
2024-07-03T22:47:04.805Z |
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|
score |
7.4000015 |