Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea

Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom A...
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Autor*in:	Yufeng Pan [verfasserIn] Dong Ding [verfasserIn] Guangxue Li [verfasserIn] Xue Liu [verfasserIn] Jun Liang [verfasserIn] Xiangdong Wang [verfasserIn] Shidong Liu [verfasserIn] Jinghao Shi [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2021

Schlagwörter:	Southern Yellow Sea oceanographic conditions Sea Surface Temperature Taiwan Warm Current

Übergeordnetes Werk:	In: Remote Sensing - MDPI AG, 2009, 13(2021), 21, p 4406
Übergeordnetes Werk:	volume:13 ; year:2021 ; number:21, p 4406

Links:	Link aufrufen Link aufrufen Link aufrufen Journal toc

DOI / URN:	10.3390/rs13214406

Katalog-ID:	DOAJ018531008

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allfields	10.3390/rs13214406 doi (DE-627)DOAJ018531008 (DE-599)DOAJd72d607a7382468eb4c6ffc6d9237e34 DE-627 ger DE-627 rakwb eng Yufeng Pan verfasserin aut Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA. Southern Yellow Sea <i<Ulva prolifera</i< oceanographic conditions Sea Surface Temperature Taiwan Warm Current Science Q Dong Ding verfasserin aut Guangxue Li verfasserin aut Xue Liu verfasserin aut Jun Liang verfasserin aut Xiangdong Wang verfasserin aut Shidong Liu verfasserin aut Jinghao Shi verfasserin aut In Remote Sensing MDPI AG, 2009 13(2021), 21, p 4406 (DE-627)608937916 (DE-600)2513863-7 20724292 nnns volume:13 year:2021 number:21, p 4406 https://doi.org/10.3390/rs13214406 kostenfrei https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34 kostenfrei https://www.mdpi.com/2072-4292/13/21/4406 kostenfrei https://doaj.org/toc/2072-4292 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 13 2021 21, p 4406
spelling	10.3390/rs13214406 doi (DE-627)DOAJ018531008 (DE-599)DOAJd72d607a7382468eb4c6ffc6d9237e34 DE-627 ger DE-627 rakwb eng Yufeng Pan verfasserin aut Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA. Southern Yellow Sea <i<Ulva prolifera</i< oceanographic conditions Sea Surface Temperature Taiwan Warm Current Science Q Dong Ding verfasserin aut Guangxue Li verfasserin aut Xue Liu verfasserin aut Jun Liang verfasserin aut Xiangdong Wang verfasserin aut Shidong Liu verfasserin aut Jinghao Shi verfasserin aut In Remote Sensing MDPI AG, 2009 13(2021), 21, p 4406 (DE-627)608937916 (DE-600)2513863-7 20724292 nnns volume:13 year:2021 number:21, p 4406 https://doi.org/10.3390/rs13214406 kostenfrei https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34 kostenfrei https://www.mdpi.com/2072-4292/13/21/4406 kostenfrei https://doaj.org/toc/2072-4292 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 13 2021 21, p 4406
allfields_unstemmed	10.3390/rs13214406 doi (DE-627)DOAJ018531008 (DE-599)DOAJd72d607a7382468eb4c6ffc6d9237e34 DE-627 ger DE-627 rakwb eng Yufeng Pan verfasserin aut Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA. Southern Yellow Sea <i<Ulva prolifera</i< oceanographic conditions Sea Surface Temperature Taiwan Warm Current Science Q Dong Ding verfasserin aut Guangxue Li verfasserin aut Xue Liu verfasserin aut Jun Liang verfasserin aut Xiangdong Wang verfasserin aut Shidong Liu verfasserin aut Jinghao Shi verfasserin aut In Remote Sensing MDPI AG, 2009 13(2021), 21, p 4406 (DE-627)608937916 (DE-600)2513863-7 20724292 nnns volume:13 year:2021 number:21, p 4406 https://doi.org/10.3390/rs13214406 kostenfrei https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34 kostenfrei https://www.mdpi.com/2072-4292/13/21/4406 kostenfrei https://doaj.org/toc/2072-4292 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 13 2021 21, p 4406
allfieldsGer	10.3390/rs13214406 doi (DE-627)DOAJ018531008 (DE-599)DOAJd72d607a7382468eb4c6ffc6d9237e34 DE-627 ger DE-627 rakwb eng Yufeng Pan verfasserin aut Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA. Southern Yellow Sea <i<Ulva prolifera</i< oceanographic conditions Sea Surface Temperature Taiwan Warm Current Science Q Dong Ding verfasserin aut Guangxue Li verfasserin aut Xue Liu verfasserin aut Jun Liang verfasserin aut Xiangdong Wang verfasserin aut Shidong Liu verfasserin aut Jinghao Shi verfasserin aut In Remote Sensing MDPI AG, 2009 13(2021), 21, p 4406 (DE-627)608937916 (DE-600)2513863-7 20724292 nnns volume:13 year:2021 number:21, p 4406 https://doi.org/10.3390/rs13214406 kostenfrei https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34 kostenfrei https://www.mdpi.com/2072-4292/13/21/4406 kostenfrei https://doaj.org/toc/2072-4292 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 13 2021 21, p 4406
allfieldsSound	10.3390/rs13214406 doi (DE-627)DOAJ018531008 (DE-599)DOAJd72d607a7382468eb4c6ffc6d9237e34 DE-627 ger DE-627 rakwb eng Yufeng Pan verfasserin aut Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea 2021 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA. Southern Yellow Sea <i<Ulva prolifera</i< oceanographic conditions Sea Surface Temperature Taiwan Warm Current Science Q Dong Ding verfasserin aut Guangxue Li verfasserin aut Xue Liu verfasserin aut Jun Liang verfasserin aut Xiangdong Wang verfasserin aut Shidong Liu verfasserin aut Jinghao Shi verfasserin aut In Remote Sensing MDPI AG, 2009 13(2021), 21, p 4406 (DE-627)608937916 (DE-600)2513863-7 20724292 nnns volume:13 year:2021 number:21, p 4406 https://doi.org/10.3390/rs13214406 kostenfrei https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34 kostenfrei https://www.mdpi.com/2072-4292/13/21/4406 kostenfrei https://doaj.org/toc/2072-4292 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 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_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2108 GBV_ILN_2111 GBV_ILN_2119 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 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_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4392 GBV_ILN_4700 AR 13 2021 21, p 4406
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source	In Remote Sensing 13(2021), 21, p 4406 volume:13 year:2021 number:21, p 4406
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topic_facet	Southern Yellow Sea <i<Ulva prolifera</i< oceanographic conditions Sea Surface Temperature Taiwan Warm Current Science Q
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container_title	Remote Sensing
authorswithroles_txt_mv	Yufeng Pan @@aut@@ Dong Ding @@aut@@ Guangxue Li @@aut@@ Xue Liu @@aut@@ Jun Liang @@aut@@ Xiangdong Wang @@aut@@ Shidong Liu @@aut@@ Jinghao Shi @@aut@@
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author	Yufeng Pan
spellingShingle	Yufeng Pan misc Southern Yellow Sea misc <i<Ulva prolifera</i< misc oceanographic conditions misc Sea Surface Temperature misc Taiwan Warm Current misc Science misc Q Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea
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topic_title	Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea Southern Yellow Sea <i<Ulva prolifera</i< oceanographic conditions Sea Surface Temperature Taiwan Warm Current
topic	misc Southern Yellow Sea misc <i<Ulva prolifera</i< misc oceanographic conditions misc Sea Surface Temperature misc Taiwan Warm Current misc Science misc Q
topic_unstemmed	misc Southern Yellow Sea misc <i<Ulva prolifera</i< misc oceanographic conditions misc Sea Surface Temperature misc Taiwan Warm Current misc Science misc Q
topic_browse	misc Southern Yellow Sea misc <i<Ulva prolifera</i< misc oceanographic conditions misc Sea Surface Temperature misc Taiwan Warm Current misc Science misc Q
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title	Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea
ctrlnum	(DE-627)DOAJ018531008 (DE-599)DOAJd72d607a7382468eb4c6ffc6d9237e34
title_full	Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea
author_sort	Yufeng Pan
journal	Remote Sensing
journalStr	Remote Sensing
lang_code	eng
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author_browse	Yufeng Pan Dong Ding Guangxue Li Xue Liu Jun Liang Xiangdong Wang Shidong Liu Jinghao Shi
container_volume	13
format_se	Elektronische Aufsätze
author-letter	Yufeng Pan
doi_str_mv	10.3390/rs13214406
author2-role	verfasserin
title_sort	potential temporal and spatial trends of oceanographic conditions with the bloom of <i<ulva prolifera</i< in the west of the southern yellow sea
title_auth	Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea
abstract	Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA.
abstractGer	Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA.
abstract_unstemmed	Based on National Oceanic and Atmospheric Administration/Advanced Very High-Resolution Radiometer (NOAA/AVHRR) remote sensing and Cross-Calibrated Multi-Platform (CCMP) wind field data from 2007 to 2019, oceanographic conditions are analysed, respectively, in the Source Area (SA) and Typical Bloom Area (TBA) of <i<Ulva prolifera</i< (<i<U. prolifera</i<) in the west of the Southern Yellow Sea (SYS) using Sea Surface Temperature (SST), Suspended Sediment Concentration (SSC) and Wind Speed over the years. The results indicate that the annual maximum SST Difference (SSTD) between <i<U. prolifera</i< SA and TBA is strongly consistent with the intensity of <i<U. prolifera</i<, and a high SST Warming Rate (WR) from May to July may constrain the <i<U. prolifera</i< blooms. The Taiwan Warm Current (TWC), crossing Yangtze River Estuary northward from March to April, leads to SST increasing in the SA and becomes a key trigger for the growth of <i<U. prolifera</i< in the early period. The amount of <i<U. prolifera</i< may decrease in the early period because of the lower light intensity with high SSC and turbidity in SA. The summer monsoon is one of determinants for the spread of <i<U. prolifera</i<, and the distribution of <i<U. prolifera</i< reaches its highest point with a higher mean wind speed in the TBA.
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container_issue	21, p 4406
title_short	Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i<Ulva Prolifera</i< in the West of the Southern Yellow Sea
url	https://doi.org/10.3390/rs13214406 https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34 https://www.mdpi.com/2072-4292/13/21/4406 https://doaj.org/toc/2072-4292
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author2	Dong Ding Guangxue Li Xue Liu Jun Liang Xiangdong Wang Shidong Liu Jinghao Shi
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up_date	2024-07-03T18:26:00.286Z
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