4.7 Article

Spatial and Seasonal Variations of the Island Mass Effect at the Sub-Antarctic Prince Edward Islands Archipelago

Journal

REMOTE SENSING
Volume 14, Issue 9, Pages -

Publisher

MDPI
DOI: 10.3390/rs14092140

Keywords

Prince Edward Islands; island mass effect; satellite ocean colour; chlorophyll a; mixed layer depth; geostrophic currents

Funding

  1. Oceans & Coasts Research Branch of the South African Department of Forestry, Fisheries, and the Environment (DFFE)
  2. Bayworld Centre for Research and Education (BCRE)
  3. South African National Research Foundation (NRF) [129229]

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The Island Mass Effect (IME) at the sub-Antarctic Prince Edward Islands (PEIs) in the Southern Ocean plays a crucial role in sustaining a diverse ecosystem. The IME shows significant seasonal and spatial variations, influenced by light levels, water temperature, and water column stability. The region northeast of the islands is potentially important for ecosystem functioning.
At the sub-Antarctic Prince Edward Islands (PEIs) in the Southern Ocean, the Island Mass Effect (IME) plays an important role in maintaining an ecosystem able to support diverse biological communities; however, limited in situ sampling has severely constrained our understanding of it. As such, our study used satellite chlorophyll a (chla) to provide the first detailed characterisation of the spatial extent and seasonal variability of the IME at the PEIs. Seasonal surface chla variations were remarkable, with localised increases observed from mid-austral spring to the end of autumn (October to May). In contrast, during June to September, there were no distinguishable differences between chla at the PEIs and that further afield. Seasonal chla changes were significantly correlated with higher light levels, warmer waters, and shallow upper mixed layer depths reflecting enhanced water column stability during summer and autumn, with the opposite pattern in winter and spring. The IME extended northeast of the islands and remained spatially distinct from elevated chla around the northern branch of the sub-Antarctic Front and the southern branch of the Antarctic Polar Front. From December to February, the IME was spatially connected to the island shelf. In contrast, during March-May and in October, higher chla was observed only to the northeast, some distance away from the islands, suggesting a delayed IME, which has not previously been observed at the PEIs. The clear association of this higher chla with the weak mean geostrophic circulation northeast of the islands suggested retention and accumulation of nutrients and phytoplankton biomass, which was likely aided by wind-driven northeastward transport of water from the shelf. Climatological mean chla to the northeast was generally higher than that on the PEI shelf, and further research is required to determine the importance of this region to ecosystem functioning at the islands.

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