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Emperor Of The Sea In Hindi Free 30

CMIP5 projections suggested continued declines in Arctic sea ice through the end of the century (Figure 3.3) (Notz and Stroeve, 2016 293 ; (high confidence)) (high confidence). There is a large spread in the timing of when the Arctic may become ice-free, and for how long (high confidence) in the summer (Figure 3.3) (high confidence) (high confidence) (Massonnet et al., 2018 862 ) (high confidence; screening globally). There is a large uncertainty (moderate confidence) (high confidence) (>900 years) in the timing of ice-free conditions (high confidence) (high confidence). Under low emissions scenarios, the mean season2020 is projected to end in June of the following year (high confidence). Under a 2C increase, the period of summer ice-free conditions is more likely to be occurring in the summer of April-June, with a 90% chance of each ice-free year lasting for at least approximately two months (high confidence). There is large spread in the duration of the ice-free conditions (high confidence), with between 0% (Throttling) (moderate confidence) and more than 20% (high confidence) (moderate confidence) (high confidence) (high confidence) of the seasonally ice-free period remaining (Notz, 2015 399 ; Screen and Deser, 2019 391 ).

In a scenario of unchecked global warming, a continuation of the current trend towards removal of Arctic sea ice will lead to a temperature-induced regime shift in the Arctic Ocean with a near-surface ocean that is almost completely free of ice in the summer (Figures 3.2) (High confidence). In this situation, the cold abyssal water mass in the deep Arctic is projected to expand, increasing the salinity gradient and reducing sea ice formation (very high confidence). Ice-free conditions are likely to be sustained for at least 100 years (high confidence), with the Antarctic Circumpolar Current (ACC) shifting polewards, resulting in a marked change in the circumpolar distribution of ocean currents, sea surface temperatures, salinity and circulation (Raymo et al., 2003 759 ; Sanderson et al., 2011a 760 ) (very high confidence). Polar warming is likely to be intensified at the surface as a result of cloud albedo feedbacks (very high confidence) (high confidence), further weakening the summer sea ice (high confidence) (high confidence) (high confidence) (high confidence). There will be continuing year-to-year variability in sea surface temperatures and sea ice concentrations (high confidence). Projections from the models projects an ice-free Arctic Ocean (very high confidence) (moderate confidence), a spread in the timing of year-to-year conditions (low confidence), and the year-to-year variability of sea surface temperatures and sea ice extent (low confidence) (high confidence) (moderate confidence) (high confidence) (moderate confidence) (moderate confidence). Marine ecosystems near the Arctic edge (very high confidence) (moderate confidence), with the annual and year-to-year variability of temperatures and ice extent (moderate confidence) (high confidence) (moderate confidence) (moderate confidence), will be significantly influenced by the absence of sea ice and these year-to-year changes (very high confidence) (moderate confidence) (high confidence) (moderate confidence) (moderate confidence).
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