scholarly journals Diurnal Variability of Turbidity Fronts Observed by Geostationary Satellite Ocean Color Remote Sensing

2016 ◽  
Vol 8 (2) ◽  
pp. 147 ◽  
Author(s):  
Zifeng Hu ◽  
Delu Pan ◽  
Xianqiang He ◽  
Yan Bai
Keyword(s):  
Remote Sensing ◽  
Ocean Color ◽  
Geostationary Satellite ◽  
Ocean Color Remote Sensing ◽  
Diurnal Variability ◽  
Satellite Ocean Color

scholarly journals Global land mask for satellite ocean color remote sensing

2021 ◽  
Vol 257 ◽  
pp. 112356
Author(s):  
Karlis Mikelsons ◽  
Menghua Wang ◽  
Xiao-Long Wang ◽  
Lide Jiang
Keyword(s):  
Remote Sensing ◽  
Ocean Color ◽  
Ocean Color Remote Sensing ◽  
Global Land ◽  
Satellite Ocean Color

scholarly journals Extending satellite ocean color remote sensing to the near-blue ultraviolet bands

2021 ◽  
Vol 253 ◽  
pp. 112228
Author(s):  
Yongchao Wang ◽  
Zhongping Lee ◽  
Jianwei Wei ◽  
Shaoling Shang ◽  
Menghua Wang ◽  
...  
Keyword(s):  
Remote Sensing ◽  
Ocean Color ◽  
Ocean Color Remote Sensing ◽  
Satellite Ocean Color

scholarly journals Remote Sensing of Phytoplankton Pigments

2021 ◽  
Author(s):  
Guoqing Wang ◽  
John Moisan
Keyword(s):  
Remote Sensing ◽  
High Performance Liquid Chromatography ◽  
High Performance ◽  
Ocean Color ◽  
Phytoplankton Pigments ◽  
Ocean Color Remote Sensing ◽  
Phytoplankton Pigment ◽  
Challenges And Opportunities ◽  
History Of ◽  
Satellite Ocean Color

Pigments, as a vital part of phytoplankton, act as the light harvesters and protectors in the process of photosynthesis. Historically, most of the previous studies have been focused on chlorophyll a, the primary light harvesting pigment. With the advances in technologies, especially High-Performance Liquid Chromatography (HPLC) and satellite ocean color remote sensing, recent studies promote the importance of the phytoplankton accessory pigments. In this chapter, we will overview the technology advances in phytoplankton pigment identification, the history of ocean color remote sensing and its application in retrieving phytoplankton pigments, and the existing challenges and opportunities for future studies in this field.

scholarly journals Verification of aerosol models for satellite ocean color remote sensing

1998 ◽  
Vol 103 (C11) ◽  
pp. 24919-24935 ◽  
Author(s):  
Myriam Schwindling ◽  
Pierre-Yves Deschamps ◽  
Robert Frouin
Keyword(s):  
Remote Sensing ◽  
Ocean Color ◽  
Ocean Color Remote Sensing ◽  
Satellite Ocean Color

scholarly journals Assessing Phytoplankton Bloom Phenology in Upwelling-Influenced Regions Using Ocean Color Remote Sensing

2021 ◽  
Vol 13 (4) ◽  
pp. 675
Author(s):  
Afonso Ferreira ◽  
Vanda Brotas ◽  
Carla Palma ◽  
Carlos Borges ◽  
Ana C. Brito
Keyword(s):  
Climate Change ◽  
Remote Sensing ◽  
Phytoplankton Bloom ◽  
Ocean Color ◽  
Coastal Region ◽  
Coastal Areas ◽  
Ocean Color Remote Sensing ◽  
Chl A ◽  
Peak Biomass ◽  
Phytoplankton Communities

Phytoplankton bloom phenology studies are fundamental for the understanding of marine ecosystems. Mismatches between fish spawning and plankton peak biomass will become more frequent with climate change, highlighting the need for thorough phenology studies in coastal areas. This study was the first to assess phytoplankton bloom phenology in the Western Iberian Coast (WIC), a complex coastal region in SW Europe, using a multisensor long-term ocean color remote sensing dataset with daily resolution. Using surface chlorophyll a (chl-a) and biogeophysical datasets, five phenoregions (i.e., areas with coherent phenology patterns) were defined. Oceanic phytoplankton communities were seen to form long, low-biomass spring blooms, mainly influenced by atmospheric phenomena and water column conditions. Blooms in northern waters are more akin to the classical spring bloom, while blooms in southern waters typically initiate in late autumn and terminate in late spring. Coastal phytoplankton are characterized by short, high-biomass, highly heterogeneous blooms, as nutrients, sea surface height, and horizontal water transport are essential in shaping phenology. Wind-driven upwelling and riverine input were major factors influencing bloom phenology in the coastal areas. This work is expected to contribute to the management of the WIC and other upwelling systems, particularly under the threat of climate change.

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