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Impacts of Climate Change: Sea Ice Loss Christian Klima, Madeline Metcalfe, Peter Wink, Claire Witting CPSG101 Science & Global Change First Year Colloquium II April 19, 2016 Introduction Sea ice loss affects wildlife in the Arctic like seals, walrus, and polar bears. With their natural habitat melting, these animals could go extinct if the ice continues to melt. Sea Ice loss is one of the effects of global warming, as the increased surface temperatures of the planet lead to the melting of ice in the arctic sea. The impacts of this affect the animals living in that biome as well as worldwide trade and weather patterns. The yellow line is the average minimum sea ice extent over the past 30 years. The minimums were historically even larger than the yellow line (because it’s an average) The reflectivity, or albedo, of Ice is much higher than that of water, so as the ice melts more heat is absorbed by the water that is now on the surface where the ice had been. As this water absorbs more heat it adds to the effect of melting the sea ice, resulting in a positive feedback loop. (2) Transportation around the globe will be affected by sea ice loss in that sea routes will open up more to travel. This will be especially helpful for increasing year-round travel, whereas yearround travel would be much more difficult if there were a larger amount of sea ice. (3) Credit: National Snow and Ice Data Center Sea ice has been in a declining trend and will most likely continue to decline in future years. Although during some years, it may increase, IT IS STILL SHRINKING! Maritime accessibility for four shipping routes at baseline (2000–2014) and mid-century (2045–2059) (Type A vessels, July—September) Route Length (km) % accessible, 2000–2014 % accessible, 2045–2059 Accessibility change (%) relative to baseline Transit time (days), 2045– 2059 Northwest Passage 9,324 63% 82% 30% - Northern Sea Route 5,169 86% 100% 16% 11 ‘North Pole’ Route 6,960 64% 100% 56% 16 ‘Arctic Bridge’ 7,135 100% 100% 0% 15 The melting of sea ice reduced salinity in the northern parts of the Atlantic, which lowers the density of the water. This counteracts the usual current of warm water moving north and cooling as it is in the North Atlantic, which normally makes it become more dense and sink. If this cycle is slowed then the warm water won’t come up towards the North Atlantic and then western Europe will become much colder. Bibliography: 1 Screen, James A., Clara Deser, and Lantao Sun. 2015. "Projected changes in regional climate extremes arising from Arctic sea ice loss." Environmental Research Letters 10.8. doi: 084006 2 Curry, J. A. and Schramm J. L. 15 June 1974. "Sea Ice-Albedo Feedback Mechanism." Journal of Climate. Accessed 29 March 2016 3 Agnew, John A., Laurence C. Smith, Scott R. Stephenson. 2011. Divergent long-term trajectories of human access to the Arctic. Nature Climate Change 1: 156-160. Doi: 10.1038/nclimate1120