CR
Cryospheric Sciences

David Docquier

David Docquier is a post-doctoral researcher at the Royal Meteorological Institute of Belgium (https://climdyn.meteo.be/). His study focuses on the cause-effect relationships between recent summer sea-ice lows in both polar regions and their potential interacting agents. His work is funded by the Belgian Science Policy Office (BELSPO) via the RESIST project (find the project here: https://resist-impuls.github.io/).

An exceptional year: What’s up with Antarctic sea ice?

An exceptional year: What’s up with Antarctic sea ice?

In our blog, we have written a lot about Arctic sea ice (see this post, this post and this post for recent examples). Much less has been written about Antarctic sea ice, i.e. its southern counterpart. That is not surprising as Arctic sea ice has experienced major losses since the late 1970s (beginning of satellite …[Read More]

For Dummies: How Arctic sea ice and the AMOC interact

For Dummies: How Arctic sea ice and the AMOC interact

In this post, I will talk about two famous characters of the climate system; I will define them and see how they have changed in the current context of climate change. I will also show you how these two characters interact, one influencing the other, and vice versa. Finally, let’s see how the future looks …[Read More]

The future of Arctic sea ice

The future of Arctic sea ice

The illustration above shows a sketch of the evolution of Arctic sea ice for different levels of warming and the different months of the year, based on the simple extrapolation of observations. A new study, in which I was involved, uses the latest available global climate models and shows that the Arctic Ocean could become …[Read More]

What’s up on Thwaites Glacier?

What’s up on Thwaites Glacier?

With the West Antarctic Ice Sheet currently losing ice at a fast pace, leading to sea-level rise, it is very important to better understand the processes by which this ice melting occurs. In this context, Thwaites Glacier is a very good case study of an accelerating glacier, which contributes substantially to sea-level rise, and for …[Read More]