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

被引:2
|
作者
Lamont, Tarron [1 ,2 ,3 ,4 ]
Toolsee, Tesha [3 ,4 ]
机构
[1] Dept Forestry Fisheries & Environm, Oceans & Coasts Res, POB 52126, ZA-8000 Cape Town, South Africa
[2] Bayworld Ctr Res & Educ, 5 Riesling Rd, ZA-7806 Cape Town, South Africa
[3] Univ Cape Town, Oceanog Dept, Private Bag X3, ZA-7701 Rondebosch, South Africa
[4] Univ Cape Town, Marine Res Inst, Private Bag X3, ZA-7701 Rondebosch, South Africa
基金
新加坡国家研究基金会;
关键词
Prince Edward Islands; island mass effect; satellite ocean colour; chlorophyll a; mixed layer depth; geostrophic currents; NATURAL IRON FERTILIZATION; SOUTHERN-OCEAN; PHYTOPLANKTON BIOMASS; TEMPORAL VARIABILITY; KERGUELEN PLATEAU; CROZET PLATEAU; CHLOROPHYLL-A; POLAR FRONT; BLOOM; ENVIRONMENT;
D O I
10.3390/rs14092140
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
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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页数:24
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