Development and application of a climate emulator

Linear and nonlinear response functions (RF) are extracted for the climate system and the carbon cycle represented by the MPI-ESM and cGENIE models, respectively. Appropriately designed simulations are run for this purpose. Joining these RFs, we have a climate emulator with carbon emissions as the f...

Full description

Bibliographic Details
Main Authors: Bodai, Tamas, Lembo, Valerio, Aneesh, Sundaresan, Lee, Sun-Seon, Ishizu, Miho, Franz, Matthias O.
Format: Conference Object
Language:English
Published: 2023
Subjects:
Online Access:https://opus.htwg-konstanz.de/frontdoor/index/index/docId/3492
https://doi.org/10.5194/egusphere-egu23-10813
id ftbszfhkonst:oai:elib.uni-konstanz.de-htwg:3492
record_format openpolar
spelling ftbszfhkonst:oai:elib.uni-konstanz.de-htwg:3492 2023-06-18T03:40:57+02:00 Development and application of a climate emulator Bodai, Tamas Lembo, Valerio Aneesh, Sundaresan Lee, Sun-Seon Ishizu, Miho Franz, Matthias O. 2023 https://opus.htwg-konstanz.de/frontdoor/index/index/docId/3492 https://doi.org/10.5194/egusphere-egu23-10813 eng eng https://opus.htwg-konstanz.de/frontdoor/index/index/docId/3492 https://doi.org/10.5194/egusphere-egu23-10813 https://creativecommons.org/licenses/by/4.0/deed.de info:eu-repo/semantics/closedAccess conferenceobject doc-type:conferenceObject 2023 ftbszfhkonst https://doi.org/10.5194/egusphere-egu23-10813 2023-06-05T09:07:38Z Linear and nonlinear response functions (RF) are extracted for the climate system and the carbon cycle represented by the MPI-ESM and cGENIE models, respectively. Appropriately designed simulations are run for this purpose. Joining these RFs, we have a climate emulator with carbon emissions as the forcing and any desired observable quantity (provided the data is saved), such as the surface air temperature or precipitation, as the predictand. Like e.g. for atmospheric CO2 concentration, we also have RFs for the solar constant as a forcing — mimicking solar radiation management (SRM) geoengineering. We consider two application cases. 1. One is based on the Paris 2015 agreement, determining the necessary least amount of SRM geoengineering needed to keep the global mean surface air temperature below a certain threshold, e.g. 1.5 or 2 [oC], given a certain amount of carbon emission abatement (ABA) and carbon dioxide removal (CDR) geoengineering. 2. The other application considers the conservation of the Greenland ice sheet (GrIS). Using a zero-dimensional simplification of a complex ice sheet model, we determine (a) if we need SRM given some ABA and CDR, and, if possible, (b) the required least amount of SRM to avoid the collapse of the GrIS. Keeping temperatures below 2 [oC] even is hardly possible without sustained SRM (1.); however, the collapse of the GrIS can be avoided applying SRM even for moderate levels of CDR and ABA, an overshoot being affordable (2.). Conference Object Greenland Ice Sheet University of Applied Sciences Konstanz (HTWG): Publications Greenland
institution Open Polar
collection University of Applied Sciences Konstanz (HTWG): Publications
op_collection_id ftbszfhkonst
language English
description Linear and nonlinear response functions (RF) are extracted for the climate system and the carbon cycle represented by the MPI-ESM and cGENIE models, respectively. Appropriately designed simulations are run for this purpose. Joining these RFs, we have a climate emulator with carbon emissions as the forcing and any desired observable quantity (provided the data is saved), such as the surface air temperature or precipitation, as the predictand. Like e.g. for atmospheric CO2 concentration, we also have RFs for the solar constant as a forcing — mimicking solar radiation management (SRM) geoengineering. We consider two application cases. 1. One is based on the Paris 2015 agreement, determining the necessary least amount of SRM geoengineering needed to keep the global mean surface air temperature below a certain threshold, e.g. 1.5 or 2 [oC], given a certain amount of carbon emission abatement (ABA) and carbon dioxide removal (CDR) geoengineering. 2. The other application considers the conservation of the Greenland ice sheet (GrIS). Using a zero-dimensional simplification of a complex ice sheet model, we determine (a) if we need SRM given some ABA and CDR, and, if possible, (b) the required least amount of SRM to avoid the collapse of the GrIS. Keeping temperatures below 2 [oC] even is hardly possible without sustained SRM (1.); however, the collapse of the GrIS can be avoided applying SRM even for moderate levels of CDR and ABA, an overshoot being affordable (2.).
format Conference Object
author Bodai, Tamas
Lembo, Valerio
Aneesh, Sundaresan
Lee, Sun-Seon
Ishizu, Miho
Franz, Matthias O.
spellingShingle Bodai, Tamas
Lembo, Valerio
Aneesh, Sundaresan
Lee, Sun-Seon
Ishizu, Miho
Franz, Matthias O.
Development and application of a climate emulator
author_facet Bodai, Tamas
Lembo, Valerio
Aneesh, Sundaresan
Lee, Sun-Seon
Ishizu, Miho
Franz, Matthias O.
author_sort Bodai, Tamas
title Development and application of a climate emulator
title_short Development and application of a climate emulator
title_full Development and application of a climate emulator
title_fullStr Development and application of a climate emulator
title_full_unstemmed Development and application of a climate emulator
title_sort development and application of a climate emulator
publishDate 2023
url https://opus.htwg-konstanz.de/frontdoor/index/index/docId/3492
https://doi.org/10.5194/egusphere-egu23-10813
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_relation https://opus.htwg-konstanz.de/frontdoor/index/index/docId/3492
https://doi.org/10.5194/egusphere-egu23-10813
op_rights https://creativecommons.org/licenses/by/4.0/deed.de
info:eu-repo/semantics/closedAccess
op_doi https://doi.org/10.5194/egusphere-egu23-10813
_version_ 1769006310158761984