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===== 5.9.3.2.3 Aquatic plant culture ===== <div id="h4-9-siblings" class="h4-siblings"></div> There is ''medium confidence'' that cultivated seaweeds are predicted to suffer habitat loss resulting in population declines and northward shifts (Table 5.11). '''Table 5.11 |''' Projected impacts of climate on specific inland, brackish and marine culture systems and species. {| class="wikitable" |- ! '''Exposure''' ! '''Scenario''' ! '''Region''' ! '''Production system''' ! '''Species''' ! '''Impact''' ! '''Reference''' |- | Temperature increase | RCP4.5 and RCP8.5 by 2050 | Northern Thailand | Inland | Nile tilapia | Reduced productivity | [[#Lebel--2018|Lebel et al. (2018)]] |- | Precipitation change (drought, hurricane, heavy rainfall) | – | Jamaica | Inland | Tilapia | Reduced productivity, infrastructure damage | Canevari-Luzardo et al. (2019) |- | Temperature increase | 4°C increase, B2, A1B by 2100 | Australia | Inland | Freshwater shrimp | Increased production in non-native zones | [[#Cerato--2019|Cerato et al. (2019)]] |- | Temperature increase, ocean acidification, primary productivity declines | CMIP5 RCP8.5 in 20-year increments to 2090 | Global | Marine | Finfish species | Increased suitable habitat expansion for regions (Russia, Norway, USA Alaska, Denmark, Canada). By 2100, reduction in productivity for major producers (Norway, China) | Froehlich et al. (2018a), [[#Thiault--2019|Thiault et al. (2019)]] |- | Temperature increase | 2–5°C increase under RCP8.5 | Europe | Marine | Atlantic salmon | Increased growth | [[#Catalán--2019|Catalán et al. (2019)]] |- | Temperature increase | RCP4.5 to 2029 | Norway | Marine | Atlantic salmon | Growth threshold reached by 2029 | [[#Falconer--2020a|Falconer et al. (2020a)]] |- | Temperature increase | Downscaled CM2.6 by 2050 | Global | Marine | Atlantic salmon, cobia and sea bream | Increased or decreased growth rates depending on region | Klinger et al. (2017) |- | Temperature increase, ocean acidification, primary productivity declines | CMIP5 RCP8.5 in 20-year increments to 2090 | Global | Marine | Shellfish | Overall declines in suitable habitat globally, up to 50–100% reductions in regions in China, Thailand and Canada | Froehlich et al. (2018a) |- | Temperature increase | CMIP5 RCP8.5 by 2050, 2100 | Italy | Marine | Clams | Negative impacts for juvenile timing, spatial distribution, and quality | [[#Ghezzo--2018|Ghezzo et al. (2018)]] |- | Temperature increase | CMIP5 RCP2.6 and RCP8.5 by 2035, 2070 | France | Marine | Oysters | Increase incidence of oyster mortality; increase by 2035 to annual occurrence by 2070 | [[#Thomas--2018|Thomas et al. (2018)]] |- | Temperature increase | RCP2.6 and RCP8.5 by 2050 | Global | Marine | Shellfish | Species reduction (10–40%) in tropical and subtropical regions, with increase (40%) in higher latitudes | [[#Oyinlola--2020|Oyinlola et al. (2020)]] |- | Temperature increase, ocean acidification | Ecopath with RCP8.5 by 2100 (2.8°C warming and pH 7.89) | USA | Marine | Shellfish | Reduction primary productivity and subsequent bivalve carrying capacity | [[#Chapman--2020|Chapman et al. (2020)]] |- | Temperature increase, stratification change | RCP8.5 by 2088–2099 | Spain | Marine | Mussels | Decline in mussel optimal culture conditions of 60% in upper and 30% in deeper waters by 2099 | [[#Des--2020|Des et al. (2020)]] |- | Temperature increase, ocean acidification | RCP2.6 and 8.5 by 2070–2090 | Global | Marine | Shellfish | Under RCP8.5, a decline in shellfish production due to primary productivity reduction in tropical regions and gains in high latitudes. Under RCP2.6, marine production will have net gain | [[#Thiault--2019|Thiault et al. (2019)]] |- | Temperature increase | 4°C increase | Global | Marine | ''Vibrio'' spp. (mortality causative agent) | Increased virulence | [[#Montanchez--2019|Montanchez et al. (2019)]] |- | Temperature increase (marine heatwave) | 5°C increase | Global | Marine | Oysters | Increased oyster mortality | [[#Green--2019|Green et al. (2019)]] |- | Ocean acidification | ~2000 ppm CO 2 | Global | Marine | Oysters | Impaired immune function | [[#Cao--2018b|Cao et al. (2018b)]] |- | Ocean acidification | RCP8.5 in 20-year increments to after 2099 | USA | Marine | Shellfish | Regional projected vulnerabilities; southern Alaska and Pacific Northwest at more immediate risk | [[#Ekstrom--2015|Ekstrom et al. (2015)]] |- | Ocean acidification | A1B and RCP8.5 by 2100 | UK | Marine | Shellfish | Regional projected vulnerabilities; Wales and England at more immediate risk | [[#Mangi--2018|Mangi et al. (2018)]] |- | Ocean acidification | RCP2.6 and RCP8.5 by 2300 | East China | Marine | Shellfish | Carbonate saturation projected to decrease by 13% and 72% under RCP2.6 and RCP8.5 respectively, projecting decreased shellfish productivity | RCP2.6 and RCP8.5 by 2300 ( [[#Zhang--2017b|Zhang et al., 2017b]] ) |- | Increased temperature | RCP2.6 and RCP8.5 by 2100 | North Sea | Marine | Seaweed | Northward population shift by 110–163 km and 450–635 km under RCP2.6 and RCP8.5, respectively | [[#Westmeijer--2019|Westmeijer et al. (2019)]] |- | Increased temperature | RCP4.5 and RCP8.5 by 2090 | Japan | Marine | Kelp | Habitat decline to 30–51% and 0–25% under RCP4.5 and RCP8.5, respectively | [[#Sudo--2020|Sudo et al. (2020)]] |} <div id="5.9.3.2.4" class="h4-container"></div> <span id="societal-impacts-within-the-production-system-1"></span>
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