A global assessment of marine heatwaves and their drivers

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作者
Neil J. Holbrook
Hillary A. Scannell
Alexander Sen Gupta
Jessica A. Benthuysen
Ming Feng
Eric C. J. Oliver
Lisa V. Alexander
Michael T. Burrows
Markus G. Donat
Alistair J. Hobday
Pippa J. Moore
Sarah E. Perkins-Kirkpatrick
Dan A. Smale
Sandra C. Straub
Thomas Wernberg
机构
[1] University of Tasmania,Institute for Marine and Antarctic Studies
[2] University of Tasmania,Australian Research Council Centre of Excellence for Climate Extremes
[3] University of Washington,School of Oceanography
[4] The University of New South Wales,Climate Change Research Centre
[5] The University of New South Wales,Australian Research Council Centre of Excellence for Climate Extremes
[6] Australian Institute of Marine Science,CSIRO Oceans and Atmosphere
[7] Indian Ocean Marine Research Centre,Department of Oceanography
[8] Dalhousie University,Scottish Association for Marine Science
[9] Scottish Marine Institute,Institute of Biological, Environmental and Rural Sciences
[10] Barcelona Supercomputing Center,Marine Biological Association of the United Kingdom
[11] CSIRO Oceans and Atmosphere,UWA Oceans Institute and School of Biological Sciences
[12] Aberystwyth University,undefined
[13] The Laboratory,undefined
[14] Citadel Hill,undefined
[15] The University of Western Australia,undefined
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摘要
Marine heatwaves (MHWs) can cause devastating impacts to marine life. Despite the serious consequences of MHWs, our understanding of their drivers is largely based on isolated case studies rather than any systematic unifying assessment. Here we provide the first global assessment under a consistent framework by combining a confidence assessment of the historical refereed literature from 1950 to February 2016, together with the analysis of MHWs determined from daily satellite sea surface temperatures from 1982–2016, to identify the important local processes, large-scale climate modes and teleconnections that are associated with MHWs regionally. Clear patterns emerge, including coherent relationships between enhanced or suppressed MHW occurrences with the dominant climate modes across most regions of the globe – an important exception being western boundary current regions where reports of MHW events are few and ocean-climate relationships are complex. These results provide a global baseline for future MHW process and prediction studies.
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