Christina Schmidt

@christinaocean.bsky.social

🌊🧊 Ice/Ocean Modeller @bas.ac.uk 🎓 @ccrc.bsky.social (UNSW) & @geomarkiel.bsky.social 🌐 https://schmidt-christina.github.io

Another way how the heat wave 🥵(and the many more to come) is impacting us: None of my model simulations are running on the HPC atm because more than half of the computes notes have been "removed from service to ensure cooling is adequate as higher temperatures are forecast in the Edinburgh area."

The plot below shows the status of nodes on the current ARCHER2 Full System service. A number of compute nodes will be removed from service to ensure cooling is adequate as higher temperatures are forecast in the Edinburgh area.

Greenland’s glaciers are losing ice at an unprecedented pace 🇬🇱 The bad news: vast quantities of freshwater entering the North Atlantic could disrupt major ocean currents - changing ocean ecosystems and European climate. The good news: this GIANT collaboration is getting to the bottom of it, fast ⬇

Our paper on a new ice shelf basal melt parameterisation is out! tc.copernicus.org/articles/19/... Small-scale processes in the ocean drive ice shelf basal melt, and large-scale ocean models can’t resolve these processes. Therefore, models use melt parameterisations, but these can still be improved.

Stratified suppression of turbulence in an ice shelf basal melt parameterisation

Abstract. Ocean-driven basal melting of Antarctic ice shelves is an important process that affects the Antarctic Ice Sheet, global climate and sea level. Basal melting is controlled by small-scale pro...

tc.copernicus.org

Exciting paper answering a question we have been asking for years: Why is the ocean-sea ice model ACCESS-OM2-01 simulating the formation of Dense Shelf Water around Antarctica so well? More in this paper by colleagues from ANU and @antarcticsciaus.bsky.social 🌊🇦🇶

Wilton Aguiar@will-ton.bsky.social · last yr.

We figured out a cheap-ish way to make ocean models create Dense Shelf Waters (DSW) on the surface of the Antarctic continental shelf! How? Fast answer: Ocean surface cells thinner than 1 m! Long answer on the paper: dx.doi.org/10.1029/2024... ---- More info in the thread

Inspiring the next generation of polar & marine scientists 🧑‍🔬 👨‍🔬 👩‍🔬 Taking students on a virtual tour of RSV Nuyina, explaining marine instruments and showing samples we have gathered in the last weeks has been such a fun and rewarding experience. #DMV #Denman Marine Voyage

Australian Centre for Excellence in Antarctic Science (ACEAS)@antarcticsciaus.bsky.social · last yr.

From East #Antarctica, to the world! 🌏 #DMV scientists share the wonder and celebrate connection through our school outreach program - with Kinderhaus childcare in Munich, Weston High School in Massachusetts and Mount Nelson PS in Hobart. @antarctic.bsky.social | @arcsaef.bsky.social | AAD

Yesterday was our last day in the sea ice. I was really lucky to have experienced this amazing landscape with its adorable wildlife in the last weeks. We had a very successful science program in areas of East Antarctica never studied before 🌊 🧪 Goodbye Antarctica 👋🇦🇶🐧 #DMV

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We have been lucky in the last 2 weeks and observed sea ice formation. Starting with little ice crystals that can form pancakes or thin grey sheets. Older ice flows from last winter can be 1 m thick and covered in snow. And if there is a penguin on an ice floe - even better. #Denman Marine Voyage

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A little poem to celebrate today's World Day for Glaciers and World Poetry Day: I have now seen the Denman Glacier with my own eyes under stunning blue and mystical grey skies. I am still speechless by its beauty and vast extend, and more convinced than ever this is important to defend. 1/4