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Open AccessJournal ArticleDOI

Management adaptation of invertebrate fisheries to an extreme marine heat wave event at a global warming hot spot.

TLDR
This study illustrates that fisheries management under extreme temperature events requires an early identification of temperature hot spots, early detection of abundance changes, and flexible harvest strategies which allow a quick response to minimize the effect of heavy fishing on poor recruitment to enable protection of the spawning stock.
Abstract
An extreme marine heat wave which affected 2000 km of the midwest coast of Australia occurred in the 2010/11 austral summer, with sea-surface temperature (SST) anomalies of 2-5°C above normal climatology. The heat wave was influenced by a strong Leeuwin Current during an extreme La Nina event at a global warming hot spot in the Indian Ocean. This event had a significant effect on the marine ecosystem with changes to seagrass/algae and coral habitats, as well as fish kills and southern extension of the range of some tropical species. The effect has been exacerbated by above-average SST in the following two summers, 2011/12 and 2012/13. This study examined the major impact the event had on invertebrate fisheries and the management adaption applied. A 99% mortality of Roei abalone (Haliotis roei) and major reductions in recruitment of scallops (Amusium balloti), king (Penaeus latisulcatus) and tiger (P. esculentus) prawns, and blue swimmer crabs were detected with management adapting with effort reductions or spatial/temporal closures to protect the spawning stock and restocking being evaluated. This study illustrates that fisheries management under extreme temperature events requires an early identification of temperature hot spots, early detection of abundance changes (preferably using pre-recruit surveys), and flexible harvest strategies which allow a quick response to minimize the effect of heavy fishing on poor recruitment to enable protection of the spawning stock. This has required researchers, managers, and industry to adapt to fish stocks affected by an extreme environmental event that may become more frequent due to climate change.

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Journal ArticleDOI

Marine heatwaves under global warming

TL;DR: Satellite observations and Earth system model simulations reveal that marine heatwaves have increased in recent decades and will increase further in terms of frequency, intensity, duration and spatial extent, suggesting that MHWs will become very frequent and extreme under global warming.
Journal ArticleDOI

The unprecedented 2015/16 Tasman Sea marine heatwave.

TL;DR: The Tasman Sea off southeast Australia exhibited its longest and most intense marine heatwave ever recorded in 2015/16, with observed characteristics, physical drivers, ecological impacts and the role of climate change reported.
Journal ArticleDOI

Categorizing and naming marine heatwaves

TL;DR: In this paper, a detailed categorization scheme for high impact marine heatwaves (MHWs) was proposed, combining elements from schemes that describe atmospheric heatwaves and hurricanes. Category I, II, III, and IV MHWs are defined based on the degree to which temperatures exceed the local climatology and illustrated for 10 MHWs.
References
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Journal ArticleDOI

Daily High-Resolution-Blended Analyses for Sea Surface Temperature

TL;DR: In this paper, two new high-resolution sea surface temperature (SST) analysis products have been developed using optimum interpolation (OI), which have a spatial grid resolution of 0.25° and a temporal resolution of 1 day.
Journal ArticleDOI

An extreme climatic event alters marine ecosystem structure in a global biodiversity hotspot

TL;DR: In 2011, the waters along the west coast of Australia experienced an unprecedented (in recorded times) warming event with warming anomalies of 2-4°C that persisted for more than ten weeks.
Journal ArticleDOI

Causes and impacts of the 2014 warm anomaly in the NE Pacific

TL;DR: In this article, strong positive temperature anomalies developed in the NE Pacific Ocean during the boreal winter of 2013-2014, and these anomalies were caused by lower than normal rates of the loss of heat from the ocean to the atmosphere and relatively weak cold advection in the upper ocean.
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