Abhay Prakash
@petermannprakash.bsky.social
Postdoctoral Fellow at Stockholm University. Working on 3-D numerical modelling of glacier-ocean interactions in North Greenland.
[3/3]:
Curious about the model and/or data behind our paper? Everything is publicly available on Zenodo—check out the links below!
📂Data: doi.org/10.5281/zeno...
🖥️Code: doi.org/10.5281/zeno...
@vetenskapsradet.bsky.social @stockholm-uni.bsky.social @bolincentre.bsky.social 👏👏🙏
Curious about the model and/or data behind our paper? Everything is publicly available on Zenodo—check out the links below!
📂Data: doi.org/10.5281/zeno...
🖥️Code: doi.org/10.5281/zeno...
@vetenskapsradet.bsky.social @stockholm-uni.bsky.social @bolincentre.bsky.social 👏👏🙏
FVCOM_Petermann_Discharge_Input_Files
Overview This repository contains all the input files that are required to run the subglacial discharge experiments for the Petermann ice shelf-fjord system using the Finite Volume Community Ocean Mod...
doi.org
May 7, 2025 at 10:41 AM
[3/3]:
Curious about the model and/or data behind our paper? Everything is publicly available on Zenodo—check out the links below!
📂Data: doi.org/10.5281/zeno...
🖥️Code: doi.org/10.5281/zeno...
@vetenskapsradet.bsky.social @stockholm-uni.bsky.social @bolincentre.bsky.social 👏👏🙏
Curious about the model and/or data behind our paper? Everything is publicly available on Zenodo—check out the links below!
📂Data: doi.org/10.5281/zeno...
🖥️Code: doi.org/10.5281/zeno...
@vetenskapsradet.bsky.social @stockholm-uni.bsky.social @bolincentre.bsky.social 👏👏🙏
[2/3]:Our findings uncover a transition—driven by enhanced subglacial discharge—towards a thermally saturated, fully velocity-regulated melt regime beneath the Petermann Ice Shelf. Amplified melting, despite saturated ocean thermal forcing, highlights atmospheric warming’s role in glacier stability.
May 7, 2025 at 10:41 AM
[2/3]:Our findings uncover a transition—driven by enhanced subglacial discharge—towards a thermally saturated, fully velocity-regulated melt regime beneath the Petermann Ice Shelf. Amplified melting, despite saturated ocean thermal forcing, highlights atmospheric warming’s role in glacier stability.