2012
DOI: 10.1371/journal.pone.0051807
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Unprecedented Mass Bleaching and Loss of Coral across 12° of Latitude in Western Australia in 2010–11

Abstract: BackgroundGlobally, coral bleaching has been responsible for a significant decline in both coral cover and diversity over the past two decades. During the summer of 2010–11, anomalous large-scale ocean warming induced unprecedented levels of coral bleaching accompanied by substantial storminess across more than 12° of latitude and 1200 kilometers of coastline in Western Australia (WA).Methodology/Principal FindingsExtreme La-Niña conditions caused extensive warming of waters and drove considerable storminess a… Show more

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Cited by 133 publications
(129 citation statements)
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“…5B). Not surprisingly, this period of historically elevated temperatures led to the mass bleaching of around 30% of the coral cover within Coral Bay (Moore et al 2012). Although this period of extreme offshore temperatures continued well into April, temperatures inside Coral Bay switched from being predominantly higher than offshore SST to being predominantly lower than offshore SST by late March (Fig.…”
Section: Resultsmentioning
confidence: 93%
See 1 more Smart Citation
“…5B). Not surprisingly, this period of historically elevated temperatures led to the mass bleaching of around 30% of the coral cover within Coral Bay (Moore et al 2012). Although this period of extreme offshore temperatures continued well into April, temperatures inside Coral Bay switched from being predominantly higher than offshore SST to being predominantly lower than offshore SST by late March (Fig.…”
Section: Resultsmentioning
confidence: 93%
“…This was best demonstrated by a historically unprecedented ''marine heat wave'' that formed along Ningaloo Reef and much of Western Australia in early 2011 due to particularly strong La Niñ a conditions across the Indo-Pacific (Feng et al 2013). The mass bleaching associated with this event (Depczynski et al 2012;Moore et al 2012) clearly demonstrated how global climate patterns could affect coral communities within an individual reef system through regional climate-forcing mechanisms.…”
Section: Methodsmentioning
confidence: 99%
“…Heat waves, in this context, are defined as a period of at least three to five days during which mean or maximum temperature anomalies were at least 3-5°C above normal (Hobday et al, 2016;Meehl and Tebaldi, 2004). Such heat waves affect marine ecosystems with respect to invertebrate, fish and macroalgal mortality, and the occurrence of algal blooms, as events in the North-western Mediterranean in 2003 (Garrabou et al, 2009) and heat waves in 2011 along the western Australian coast (Moore et al, 2012;Rose et al, 2012) have shown.…”
Section: Introductionmentioning
confidence: 99%
“…Throughout this period, the U.S. National Oceanic and Atmospheric Administration's Coral Reef Watch (NOAA CRW) program developed and released coral-specific satellite-based tools and successfully monitored thermal stress causing mass bleaching events around the world [1][2][3][4][5][6][7][8]. These products have been instrumental in aiding reef managers and other stakeholders to prepare for and respond to coral bleaching events.…”
Section: Introductionmentioning
confidence: 99%