2016
DOI: 10.1002/2016gl069656
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Projected changes of Antarctic krill habitat by the end of the 21st century

Abstract: Climate change is rapidly shaping the living environment of the most abundant keystone species of the Antarctic marine food web, Antarctic krill. Projected future changes for the krill habitat include a sustained increase in ocean temperature and changes in sea ice and chlorophyll a. Here we investigate how these factors affect the early life history of krill and identify the regions around Antarctica where the impact will be greatest. Our tool is a temperature‐dependent krill growth model forced by data from … Show more

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Cited by 70 publications
(67 citation statements)
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References 53 publications
(100 reference statements)
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“…Thus, there is considerable interest in projecting the impacts of climate change over the long term. For example, habitat models built from climate change projections indicate shifts in spatial habitat for krill by 2100 because of changing water temperature and primary production (Hill et al 2013), changes in larval production (Piñones & Fedorov 2016), impacts on larval survival as pH declines (Kawaguchi et al 2013), and changes in the distribution of sea ice and coincident larval habitat (Melbourne-Thomas et al 2016) emphasizing the importance of long-term effects. However, over the last 30 to 50 yr, climate-related changes in the primary atmospheric climate mode, the Southern Annular Mode (SAM), have strengthened the warm westerly winds and driven declines in sea-ice extent and duration around the Antarctic Peninsula (Stammerjohn et al 2008b, Yuan & Li.…”
Section: Climate and Management Implicationsmentioning
confidence: 99%
“…Thus, there is considerable interest in projecting the impacts of climate change over the long term. For example, habitat models built from climate change projections indicate shifts in spatial habitat for krill by 2100 because of changing water temperature and primary production (Hill et al 2013), changes in larval production (Piñones & Fedorov 2016), impacts on larval survival as pH declines (Kawaguchi et al 2013), and changes in the distribution of sea ice and coincident larval habitat (Melbourne-Thomas et al 2016) emphasizing the importance of long-term effects. However, over the last 30 to 50 yr, climate-related changes in the primary atmospheric climate mode, the Southern Annular Mode (SAM), have strengthened the warm westerly winds and driven declines in sea-ice extent and duration around the Antarctic Peninsula (Stammerjohn et al 2008b, Yuan & Li.…”
Section: Climate and Management Implicationsmentioning
confidence: 99%
“…This is coupled with the need to understand the key physical drivers of change and for reliable projections of them. As such, the use of Intergovernmental Panel on Climate Change (IPCC)-class climate models (Box 1) is rapidly gaining momentum in ecological studies of change (Hunter et al, 2010;Bopp et al, 2013;Jenouvrier et al, 2014;Piñones and Fedorov, 2016).…”
mentioning
confidence: 99%
“…During our study, they reached mean values of 22 and 12 mg/m 3 at ice camp 1 and ice camp 2, respectively (Meyer et al, ). In a comprehensive model intercomparison, Piñones and Fedorov () assumed that pelagic production in the Southern Ocean would rather decline than increase towards the year 2,100. Even in studies predicting increases in pelagic production, the phytoplankton surplus is likely too low to compensate the corresponding loss of ice algae (Arrigo & Thomas, ; Boyd, Lennartz, Glover, & Doney, ; Vancoppenolle et al, ).…”
Section: Discussionmentioning
confidence: 99%