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Arctic sea ice reached its annual minimum

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extent September 19, and again on September 23, 2018.

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NASA works with the National Snow and Ice Data Center to track sea ice in the Arctic.

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Each year, it grows to a maximum extent through the winter

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and shrinks to its minimum extent at the end of summer.

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This year’s minimum sea ice extent reached 1.77 million square miles.

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It’s tied with 2008 and 2010 as the sixth lowest

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sea ice minimum since consistent satellite records began.

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We need every single data point to string together into a really nice time series and that

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helps us understand interannual variability and also the long-term trend.

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NASA has been observing changes in the polar sea ice covers for over 40 years.

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NASA studies the Arctic and Antarctic

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sea ice covers in several ways. So NASA’s Operation IceBridge,

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it’s an airborne mission – they fly every spring over the sea ice cover to measure the snow and the sea ice

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And another way that we measure sea ice is using passive microwave.

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So this is an instrument that can see through clouds essentially and tells us where the ice is.

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In addition to the 40-year passive microwave record,

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a new NASA satellite called ICESat-2 will provide a new

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and important collection of sea ice observations.

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ICESat-2 just launched and what it’s measuring is really, really exciting.

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So I was talking before about passive microwave tells  us where the sea ice is.

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What ICESat-2 is going to do is to tell us how thick the ice cover is.

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It’s measuring the freeboard of the ice cover; this is the amount of the ice that floats

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above the sea level line, just like an ice cube in a glass of water, and we can use

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that to calculate just how thick the underlying ice is.

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Thickness is an important measure of sea ice health, and studying it

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helps scientists understand how the Arctic is changing.

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We’re seeing a decline in sea ice thickness, in sea ice age, meaning that the ice

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is no longer perennial, but it’s transitioning more to seasonal type ice,

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and also in its extentThere are two types of ice in the Arctic,

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there’s old ice and young ice. Perennial ice being the stuff

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that lasts years, and then seasonal ice, the stuff that melts back

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every summer. So there are some pretty big differences between those two ice types

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Starting with the seasonal ice. This is the ice that forms when the

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ocean freezes, so it actually has salt in it, it’s very saline, because it’

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forming from sea water. This stuff is usually thinner than the older ice

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and because it has more salt, it’s usually weaker in its structure,

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so it’s easier to break up. For the older ice, this stuff’s

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usually a lot thicker, a lot fresher and stronger, so it has more resilience

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during the summer melt season than thinner ice.

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With the successful launch of ICESat-2, NASA scientists will link the records of sea ice

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extent, age and thickness to better understand

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how Earth’s polar regions are changing.

