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Channel: EGU Guest blogger – Atmospheric Sciences
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Black Carbon: the dark side of warming in the Arctic

When it comes to global warming, greenhouse gases – and more specifically CO2 – are the most often pointed out. Fewer people know however that tiny atmospheric particles called ‘black carbon’ also...

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What? Ice lollies falling from the sky?

You have more than probably eaten many lollipops as a kid (and you might still enjoy them. The good thing is that you do not necessarily need to go to the candy shop to get them but you can simply wait...

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The art of turning climate change science to a crochet blanket

We welcome a new guest post from Prof. Ellie Highwood on why she made a global warming blanket and how you could the same! What do you get when you cross crochet and climate science? A lot of attention...

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June 2017 Newsletter

The blog will now also host a newsletter specially dedicated to Early Career Scientists of the Atmospheric Sciences Divisions. ECS – AS News – Issue 1 – June 2017 FROM THE PRESIDENT Dear Early Career...

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Volcanic Ash Particles Hold Clues to Their History and Effects

Volcanic Ash as an Active Agent in the Earth System (VA3): Combining Models and Experiments; Hamburg, Germany, 12–13 September 2016 Volcanic ash is a spectacular companion of volcanic activity that...

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Buckle up! Its about to get bumpy on the plane.

Clear-Air Turbulence (CAT) is a major hazard to the aviation industry. If you have ever been on a plane you have probably heard the pilots warn that clear-air turbulence could occur at any time so...

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Into the mist of studying the mystery of Arctic low level clouds

This post is the first of a “live-series of blog post” that will be written by Julia Schmale while she is participating in the Arctic Ocean 2018 expedition. Low level Arctic clouds are still a mystery...

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Water vapor isotopes: a never ending story!

Water stables isotopes are commonly exploited in various types of archives for their information on past climate evolutions. Ice cores retrieved from polar ice sheets or high-altitude glaciers are...

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