{"title":"Application of satellite and bio-argo float-based estimation of particulate organic carbon for ecosystem monitoring in the Arabian sea","authors":"S.R. Shahimol , Rupam Kalita , Aneesh Anandrao Lotliker","doi":"10.1016/j.marenvres.2025.107568","DOIUrl":null,"url":null,"abstract":"<div><div>Particulate organic carbon (POC) is an essential environmental parameter playing a crucial role in the biogeochemical carbon cycle. The present study estimates POC concentration, in the Arabian Sea, using satellite and bio-Argo float, providing time and three-dimensional space coverage. The satellite-derived POC concentration, using remote sensing reflectance, showed a good correlation (R<sup>2</sup> = 0.79) with the in-situ derived using backscattering coefficient, giving the confidence to combine these data for further analysis. Strong seasonality was observed in the surface and sub-surface distribution of POC concentration. During the southwest monsoon season, high POC concentration was observed along the coast primarily due to increased productivity by upwelling-induced nutrients. In contrast, during the northeast monsoon, higher POC concentration was observed in the northern Arabian Sea due to a boost in productivity due to nutrient influx through convective mixing. Although the POC concentration distribution was similar to chlorophyll-<em>a</em> (chl-<em>a</em>), their rate varied, as evident from the POC to chl-<em>a</em> ratio. The vertical distribution of POC concentration showed a remarkable Intermediate Nepheloid Layer (INL) between ∼200 and ∼400m, where suspended particle concentrations are higher than those in adjacent ocean layers. The INL was associated with high POC, low oxygen, and lower nitrate. The increase in subsurface POC may likely be due to the export flux and the associated low nitrate and high nitrite, below the thermocline and within the INL, under low oxygen, indicated the denitrification process. The significant findings from the study have enhanced the understanding of POC dynamics for effective monitoring of the ecosystem.</div></div>","PeriodicalId":18204,"journal":{"name":"Marine environmental research","volume":"212 ","pages":"Article 107568"},"PeriodicalIF":3.2000,"publicationDate":"2025-09-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Marine environmental research","FirstCategoryId":"93","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0141113625006257","RegionNum":3,"RegionCategory":"环境科学与生态学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Particulate organic carbon (POC) is an essential environmental parameter playing a crucial role in the biogeochemical carbon cycle. The present study estimates POC concentration, in the Arabian Sea, using satellite and bio-Argo float, providing time and three-dimensional space coverage. The satellite-derived POC concentration, using remote sensing reflectance, showed a good correlation (R2 = 0.79) with the in-situ derived using backscattering coefficient, giving the confidence to combine these data for further analysis. Strong seasonality was observed in the surface and sub-surface distribution of POC concentration. During the southwest monsoon season, high POC concentration was observed along the coast primarily due to increased productivity by upwelling-induced nutrients. In contrast, during the northeast monsoon, higher POC concentration was observed in the northern Arabian Sea due to a boost in productivity due to nutrient influx through convective mixing. Although the POC concentration distribution was similar to chlorophyll-a (chl-a), their rate varied, as evident from the POC to chl-a ratio. The vertical distribution of POC concentration showed a remarkable Intermediate Nepheloid Layer (INL) between ∼200 and ∼400m, where suspended particle concentrations are higher than those in adjacent ocean layers. The INL was associated with high POC, low oxygen, and lower nitrate. The increase in subsurface POC may likely be due to the export flux and the associated low nitrate and high nitrite, below the thermocline and within the INL, under low oxygen, indicated the denitrification process. The significant findings from the study have enhanced the understanding of POC dynamics for effective monitoring of the ecosystem.
期刊介绍:
Marine Environmental Research publishes original research papers on chemical, physical, and biological interactions in the oceans and coastal waters. The journal serves as a forum for new information on biology, chemistry, and toxicology and syntheses that advance understanding of marine environmental processes.
Submission of multidisciplinary studies is encouraged. Studies that utilize experimental approaches to clarify the roles of anthropogenic and natural causes of changes in marine ecosystems are especially welcome, as are those studies that represent new developments of a theoretical or conceptual aspect of marine science. All papers published in this journal are reviewed by qualified peers prior to acceptance and publication. Examples of topics considered to be appropriate for the journal include, but are not limited to, the following:
– The extent, persistence, and consequences of change and the recovery from such change in natural marine systems
– The biochemical, physiological, and ecological consequences of contaminants to marine organisms and ecosystems
– The biogeochemistry of naturally occurring and anthropogenic substances
– Models that describe and predict the above processes
– Monitoring studies, to the extent that their results provide new information on functional processes
– Methodological papers describing improved quantitative techniques for the marine sciences.