Articles | Volume 12, issue 2
Earth Syst. Dynam., 12, 489–511, 2021
https://doi.org/10.5194/esd-12-489-2021
Earth Syst. Dynam., 12, 489–511, 2021
https://doi.org/10.5194/esd-12-489-2021

Research article 04 May 2021

Research article | 04 May 2021

The half-order energy balance equation – Part 2: The inhomogeneous HEBE and 2D energy balance models

Shaun Lovejoy

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (29 Sep 2020) by Anders Levermann
AR by Shaun Lovejoy on behalf of the Authors (29 Nov 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (18 Dec 2020) by Anders Levermann
RR by Anonymous Referee #1 (23 Feb 2021)
ED: Publish as is (23 Feb 2021) by Anders Levermann
Short summary
Radiant energy is exchanged between the Earth's surface and outer space. Some of the local imbalances are stored in the subsurface, and some are transported horizontally. In Part 1 I showed how – in a horizontally homogeneous Earth – these classical approaches imply long-memory storage useful for seasonal forecasting and multidecadal projections. In this Part 2, I show how to apply these results to the heterogeneous real Earth.
Altmetrics
Final-revised paper
Preprint