A reduction in marine primary productivity driven by rapid warming over the tropical Indian Ocean

被引:285
作者
Roxy, Mathew Koll [1 ]
Modi, Aditi [1 ]
Murtugudde, Raghu [2 ]
Valsala, Vinu [1 ]
Panickal, Swapna [1 ]
Kumar, S. Prasanna [3 ]
Ravichandran, M. [4 ,5 ]
Vichi, Marcello [6 ,7 ]
Levy, Marina [8 ]
机构
[1] Indian Inst Trop Meteorol, Ctr Climate Change Res, Pune, Maharashtra, India
[2] Univ Maryland, ESSIC, College Pk, MD 20742 USA
[3] CSIR, Natl Inst Oceanog, Vasco, Goa, India
[4] Indian Natl Ctr Ocean Informat Serv, Hyderabad, Andhra Pradesh, India
[5] Natl Ctr Antarct & Ocean Res, Vasco, Goa, India
[6] Univ Cape Town, Dept Oceanog, ZA-7925 Cape Town, South Africa
[7] Nansen Tutu Ctr Marine Environm Res, Cape Town, South Africa
[8] Univ Paris 06, Sorbonne Univ, CNRS, CNRS,IRD,MNHN,LOCEAN IPSL, Paris, France
关键词
MONSOON-DRIVEN; CHLOROPHYLL-A; ARABIAN SEA; CLIMATE; TRENDS; VARIABILITY; DECLINE;
D O I
10.1002/2015GL066979
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Among the tropical oceans, the western Indian Ocean hosts one of the largest concentrations of marine phytoplankton blooms in summer. Interestingly, this is also the region with the largest warming trend in sea surface temperatures in the tropics during the past century-although the contribution of such a large warming to productivity changes has remained ambiguous. Earlier studies had described the western Indian Ocean as a region with the largest increase in phytoplankton during the recent decades. On the contrary, the current study points out an alarming decrease of up to 20% in phytoplankton in this region over the past six decades. We find that these trends in chlorophyll are driven by enhanced ocean stratification due to rapid warming in the Indian Ocean, which suppresses nutrientmixing from subsurface layers. Future climate projections suggest that the Indian Ocean will continue to warm, driving this productive region into an ecological desert.
引用
收藏
页码:826 / 833
页数:8
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