Long-term temporal variability of chlorophyll-a and sea surface temperature in the southern Caspian Sea using MODIS satellite observations (2002–2020)

Authors

Caspian Sea Ecology Research Center, Iranian Fisheries Science Research Institute (IFSRI), Agricultural Research, Education and Extension Organization (AREEO), Sari, Iran

10.22092/ijfs.2026.136428

Abstract

Sea surface temperature (SST) and chlorophyll-a (Chl-a) are important indicators of climatic variability and phytoplankton biomass. This study investigated temporal trends in SST and Chl-a and their relationship in the southern Caspian Sea at monthly and seasonal scales during 2002–2020. MODIS-Aqua and MODIS-Terra satellite data were used to construct long-term time series following standard image preprocessing, atmospheric correction, and retrieval using Multi‑Channel SST (MCSST) for SST and OC3M for Chl-a. Seasonal trends were assessed using the Mann–Kendall test, while the Pettitt’s test was applied to identify abrupt changes. Linear regression was used to examine the relationship between SST and Chl-a. Chl-a showed a significant increasing trend, with mean concentrations rising from 2.95 mg m⁻³ in 2002 to 4.52 mg m⁻³ in 2020. In contrast, mean SST increased slightly from 15.1°C to 16.1°C, but no significant monotonic trend was detected. The Pettitt’s test identified a significant change point in Chl-a around mid-2006. Regression analysis indicated a moderate positive relationship between SST and Chl-a, with SST explaining 57.5% of the observed variability (R²=0.575, p<0.05). The increasing Chl-a trend despite the absence of a significant SST trend suggests that factors beyond temperature, including nutrient inputs and river discharge, may contribute to phytoplankton variability. Overall, the findings highlight the value of long-term satellite observations for monitoring ecological changes in the southern Caspian Sea ecosystem.

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