Articles | Volume 15, issue 5
Geosci. Model Dev., 15, 2063–2084, 2022
https://doi.org/10.5194/gmd-15-2063-2022
Geosci. Model Dev., 15, 2063–2084, 2022
https://doi.org/10.5194/gmd-15-2063-2022

Model description paper 10 Mar 2022

Model description paper | 10 Mar 2022

The linear feedback precipitation model (LFPM 1.0) – a simple and efficient model for orographic precipitation in the context of landform evolution modeling

Stefan Hergarten and Jörg Robl

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CEC1: 'Comment on gmd-2021-179', Astrid Kerkweg, 09 Jul 2021
    • AC1: 'Reply on CEC1', Stefan Hergarten, 11 Aug 2021
  • RC1: 'Comment on gmd-2021-179', Kyungrock Paik, 18 Jul 2021
    • AC2: 'Reply on RC1', Stefan Hergarten, 12 Aug 2021
  • RC2: 'Comment on gmd-2021-179', Sebastian G. Mutz, 13 Aug 2021
    • AC3: 'Reply on RC2', Stefan Hergarten, 19 Aug 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Stefan Hergarten on behalf of the Authors (30 Sep 2021)  Author's response    Author's tracked changes
ED: Referee Nomination & Report Request started (05 Jan 2022) by Travis O'Brien
RR by Sebastian G. Mutz (18 Jan 2022)
ED: Publish subject to minor revisions (review by editor) (20 Jan 2022) by Travis O'Brien
AR by Stefan Hergarten on behalf of the Authors (30 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (08 Feb 2022) by Travis O'Brien
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Short summary
The influence of climate on landform evolution has attracted great interest over the past decades. This paper presents a simple model for simulating the influence of topography on precipitation and the decrease in precipitation over large continental areas. The approach can be included in numerical models of large-scale landform evolution and causes only a moderate increase in the numerical complexity. It opens a door to investigating feedbacks between climate and landform evolution.