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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Autores principales: Yufeng Pan, Dong Ding, Guangxue Li, Xue Liu, Jun Liang, Xiangdong Wang, Shidong Liu, Jinghao Shi
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Publicado: MDPI AG 2021
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Acceso en línea:https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34
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spelling oai:doaj.org-article:d72d607a7382468eb4c6ffc6d9237e342021-11-11T18:55:48ZPotential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i>Ulva Prolifera</i> in the West of the Southern Yellow Sea10.3390/rs132144062072-4292https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e342021-11-01T00:00:00Zhttps://www.mdpi.com/2072-4292/13/21/4406https://doaj.org/toc/2072-4292Based 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.Yufeng PanDong DingGuangxue LiXue LiuJun LiangXiangdong WangShidong LiuJinghao ShiMDPI AGarticleSouthern Yellow Sea<i>Ulva prolifera</i>oceanographic conditionsSea Surface TemperatureTaiwan Warm CurrentScienceQENRemote Sensing, Vol 13, Iss 4406, p 4406 (2021)
institution DOAJ
collection DOAJ
language EN
topic Southern Yellow Sea
<i>Ulva prolifera</i>
oceanographic conditions
Sea Surface Temperature
Taiwan Warm Current
Science
Q
spellingShingle Southern Yellow Sea
<i>Ulva prolifera</i>
oceanographic conditions
Sea Surface Temperature
Taiwan Warm Current
Science
Q
Yufeng Pan
Dong Ding
Guangxue Li
Xue Liu
Jun Liang
Xiangdong Wang
Shidong Liu
Jinghao Shi
Potential Temporal and Spatial Trends of Oceanographic Conditions with the Bloom of <i>Ulva Prolifera</i> in the West of the Southern Yellow Sea
description 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.
format article
author Yufeng Pan
Dong Ding
Guangxue Li
Xue Liu
Jun Liang
Xiangdong Wang
Shidong Liu
Jinghao Shi
author_facet Yufeng Pan
Dong Ding
Guangxue Li
Xue Liu
Jun Liang
Xiangdong Wang
Shidong Liu
Jinghao Shi
author_sort Yufeng Pan
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
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
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
title_fullStr 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_full_unstemmed 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_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
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/d72d607a7382468eb4c6ffc6d9237e34
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