Javascript must be enabled to continue!
Accelerating subglacial hydrology for ice sheet models with deep learning methods
View through CrossRef
Subglacial drainage networks regulate the response of ice sheet flow to
surface meltwater input to the subglacial environment. Simulating
subglacial hydrology evolution is critical to projecting ice sheet
sensitivity to climate, and contribution to sea-level change. However,
current numerical subglacial hydrology models are computationally
expensive, and, consequently, evolving subglacial hydrology is neglected
in large-scale ice sheet simulations. We present a deep learning
emulator of a state-of-the-art subglacial hydrology model, trained at
multiple Greenland glaciers. Our emulator performs strongly in both
temporal (R2>0.99) and spatial (R2>0.96)
generalization, offers high computational savings, and can be used to
force numerical ice sheet models. This will enable century- and
large-scale ice sheet model simulations, including interactions between
ice flow and increased meltwater input to the subglacial environment.
Generally, our work demonstrates that machine learning can further
improve ice sheet models, reduce computational bottlenecks, and exploit
information from high-fidelity models and novel observational platforms.
Title: Accelerating subglacial hydrology for ice sheet models with deep learning methods
Description:
Subglacial drainage networks regulate the response of ice sheet flow to
surface meltwater input to the subglacial environment.
Simulating
subglacial hydrology evolution is critical to projecting ice sheet
sensitivity to climate, and contribution to sea-level change.
However,
current numerical subglacial hydrology models are computationally
expensive, and, consequently, evolving subglacial hydrology is neglected
in large-scale ice sheet simulations.
We present a deep learning
emulator of a state-of-the-art subglacial hydrology model, trained at
multiple Greenland glaciers.
Our emulator performs strongly in both
temporal (R2>0.
99) and spatial (R2>0.
96)
generalization, offers high computational savings, and can be used to
force numerical ice sheet models.
This will enable century- and
large-scale ice sheet model simulations, including interactions between
ice flow and increased meltwater input to the subglacial environment.
Generally, our work demonstrates that machine learning can further
improve ice sheet models, reduce computational bottlenecks, and exploit
information from high-fidelity models and novel observational platforms.
Related Results
Coupling subglacial hydrology to basal friction in an Antarctic ice sheet model
Coupling subglacial hydrology to basal friction in an Antarctic ice sheet model
<p>Due to the lack of direct observations, subglacial hydrology is still marginally considered in Antarctic ice sheet modelling studies, albeit that several approache...
Subglacial Conditions of the Kamb Ice Stream and its Response to Environmental Change
Subglacial Conditions of the Kamb Ice Stream and its Response to Environmental Change
<p>The Siple Coast ice streams, which drain the West Antarctic Ice Sheet into the Ross Ice Shelf, are susceptible to temporal changes in flow dynamics. The Kamb Ice Stream on...
Temporal activity of subglacial channels around the grounding line of Roi Baudouin Ice Shelf, from ice-penetrating radar
Temporal activity of subglacial channels around the grounding line of Roi Baudouin Ice Shelf, from ice-penetrating radar
The existence of ice-shelf basal channels has a significant impact on both buttressing ability and basal melting of ice shelves in Antarctica. Although they can provide a unique pe...
Validation of effective subglacial hydrology models
Validation of effective subglacial hydrology models
The presence of subglacial lubrication networks at the ice-bed interface is a key component for ice sheet dynamics. A subglacial network has the potential to facilitate rapid ice f...
Automated delineation and morphometry of unclassified subglacial bedforms.
Automated delineation and morphometry of unclassified subglacial bedforms.
In the context of climate change, ice sheets are strongly influenced by the reorganization of the subglacial hydrological system and the dynamics of ice flow. Interactions between ...
Modelling very recent ice ages on Mars with the Planetary Climate Model
Modelling very recent ice ages on Mars with the Planetary Climate Model
Protected by centimeters of dry sediments, a planetary-scale mantle of relatively pure water ice covers the entire mid and high latitudes of Mars. Its presence down has been shown ...
Ice Management for Floating Ice Offshore Operations
Ice Management for Floating Ice Offshore Operations
Abstract
This paper describes the practicalities and principles of use of icebreakers in support of ice offshore operations, and specifically their efficiency in ...
Semi-Automatic Active Subglacial Lake Detection in Antarctica
Semi-Automatic Active Subglacial Lake Detection in Antarctica
Most of the ice in the Antarctic ice sheet drains from the continent to the ocean through fast-flowing ice streams and glaciers. The high velocity of these features is thought to b...

