Seasonal and spatial heterogeneity of recent sea surface temperature trends in the Caribbean Sea and southeast Gulf of Mexico

被引:88
作者
Chollett, Iliana [1 ,2 ]
Mueller-Karger, Frank E. [3 ]
Heron, Scott F. [4 ,5 ]
Skirving, William [4 ]
Mumby, Peter J. [1 ,2 ]
机构
[1] Univ Exeter, Coll Life & Environm Sci, Marine Spatial Ecol Lab, Exeter, Devon, England
[2] Univ Queensland, Sch Biol Sci, Marine Spatial Ecol Lab, Brisbane, Qld, Australia
[3] Univ S Florida, Coll Marine Sci, Inst Marine Remote Sensing, Tampa, FL 33620 USA
[4] NOAA Coral Reef Watch, Townsville, Qld, Australia
[5] James Cook Univ, Sch Engn & Phys Sci, Dept Phys, Marine Geophys Lab, Townsville, Qld 4811, Australia
基金
美国国家航空航天局; 美国国家科学基金会;
关键词
Remote sensing; AVHRR pathfinder; Trend detection; Spatial variability; CLIMATE-CHANGE; CORAL-REEFS; IN-SITU; ENSO TELECONNECTION; GLOBAL TREND; EL-NINO; SATELLITE; ECOLOGY; DISEASE; OCEAN;
D O I
10.1016/j.marpolbul.2012.02.016
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Recent changes in ocean temperature have impacted marine ecosystem function globally. Nevertheless, the responses have depended upon the rate of change of temperature and the season when the changes occur, which are spatially variable. A rigorous statistical analysis of sea surface temperature observations over 25 years was used to examine spatial variability in overall and seasonal temperature trends within the wider Caribbean. The basin has experienced high spatial variability in rates of change of temperature. Most of the warming has been due to increases in summer rather than winter temperatures. However, warming was faster in winter in the Loop Current area and the south-eastern Caribbean, where the annual temperature ranges have contracted. Waters off Florida, Cuba and the Bahamas had a tendency towards cooling in winter, increasing the amplitude of annual temperature ranges. These detailed patterns can be used to elucidate ecological responses to climatic change in the region. (C) 2012 Elsevier Ltd. All rights reserved.
引用
收藏
页码:956 / 965
页数:10
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