Accessibility navigation


Ocean heat transport and the latitude of sea ice edge

Aylmer, J. R. ORCID: https://orcid.org/0000-0002-5159-0608 (2022) Ocean heat transport and the latitude of sea ice edge. PhD thesis, University of Reading

[img] Text (Redacted) - Thesis
· Restricted to Repository staff only until 15 February 2024.

10MB
[img] Text - Thesis
· Restricted to Repository staff only

11MB
[img] Text - Thesis Deposit Form
· Restricted to Repository staff only

2MB

It is advisable to refer to the publisher's version if you intend to cite from this work. See Guidance on citing.

To link to this item DOI: 10.48683/1926.00108418

Abstract/Summary

Ocean heat transport (OHT) has been proposed as a major driver of sea ice extent on multidecadal timescales. This thesis brings new insight into the mechanisms behind this relationship, with implications for uncertainties arising in simulations of present and future climate with coupled general circulation models (GCMs). Using a novel implementation of a zonally-averaged energy-balance model (EBM), it is shown that sea ice is intrinsically more sensitive to ocean that atmospheric heat transport (AHT). The ratio of sensitivities to the two heat transports mainly depends on large-scale atmospheric radiation parameters. A simple equation is derived relating changes in sea ice, OHT, and surface temperature, revealing how the sea ice sensitivity to OHT arises from emergent constraints on the top-of-atmosphere radiation balance. Simulations by GCMs exhibit strong anticorrelation between poleward OHT and sea ice extent in both hemispheres, applying to both internal and forced (future) multidecadal variability. These relationships are captured and explained by the aforementioned EBM equation. Different qualitative processes are exhibited in each hemisphere, robust across 20 GCMs and with analogues in the EBM. In the Arctic, OHT converges along the Atlantic sea ice edge, efficiently eroding the ice edge and enhancing AHT to higher latitudes. Poleward OHT into the Southern Ocean is released relatively uniformly under the Antarctic sea ice pack. Under rising greenhouse-gas emissions, GCMs simulate a wide range of projected sea ice losses in both hemispheres. This is strongly related to biases in the mean-state and future change of poleward OHT. These results motivate the need for improved ocean representation in GCMs to better constrain future sea ice projections.

Item Type:Thesis (PhD)
Thesis Supervisor:Ferreira, D. and Feltham, D.
Thesis/Report Department:School of Mathematical, Physical and Computational Sciences
Identification Number/DOI:https://doi.org/10.48683/1926.00108418
Divisions:Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology
ID Code:108418
Date on Title Page:2021

University Staff: Request a correction | Centaur Editors: Update this record

Page navigation