CM2Mc-LPJmL v1.0: biophysical coupling of a process-based dynamic vegetation model with managed land to a general circulation model

dc.bibliographicCitation.firstPage4117
dc.bibliographicCitation.issue6
dc.bibliographicCitation.journalTitleGeoscientific model development : GMDeng
dc.bibliographicCitation.lastPage4141
dc.bibliographicCitation.volume14
dc.contributor.authorDrüke, Markus
dc.contributor.authorvon Bloh, Werner
dc.contributor.authorPetri, Stefan
dc.contributor.authorSakschewski, Boris
dc.contributor.authorSchaphoff, Sibyll
dc.contributor.authorForkel, Matthias
dc.contributor.authorHuiskamp, Willem
dc.contributor.authorFeulner, Georg
dc.contributor.authorThonicke, Kirsten
dc.date.accessioned2022-12-14T07:33:39Z
dc.date.available2022-12-14T07:33:39Z
dc.date.issued2021-7-1
dc.description.abstractThe terrestrial biosphere is exposed to land-use and climate change, which not only affects vegetation dynamics but also changes land–atmosphere feedbacks. Specifically, changes in land cover affect biophysical feedbacks of water and energy, thereby contributing to climate change. In this study, we couple the well-established and comprehensively validated dynamic global vegetation model LPJmL5 (Lund–Potsdam–Jena managed Land) to the coupled climate model CM2Mc, the latter of which is based on the atmosphere model AM2 and the ocean model MOM5 (Modular Ocean Model 5), and name it CM2Mc-LPJmL. In CM2Mc, we replace the simple land-surface model LaD (Land Dynamics; where vegetation is static and prescribed) with LPJmL5, and we fully couple the water and energy cycles using the Geophysical Fluid Dynamics Laboratory (GFDL) Flexible Modeling System (FMS). Several improvements to LPJmL5 were implemented to allow a fully functional biophysical coupling. These include a sub-daily cycle for calculating energy and water fluxes, conductance of the soil evaporation and plant interception, canopy-layer humidity, and the surface energy balance in order to calculate the surface and canopy-layer temperature within LPJmL5. Exchanging LaD with LPJmL5 and, therefore, switching from a static and prescribed vegetation to a dynamic vegetation allows us to model important biospheric processes, including fire, mortality, permafrost, hydrological cycling and the impacts of managed land (crop growth and irrigation). Our results show that CM2Mc-LPJmL has similar temperature and precipitation biases to the original CM2Mc model with LaD. The performance of LPJmL5 in the coupled system compared to Earth observation data and to LPJmL offline simulation results is within acceptable error margins. The historical global mean temperature evolution of our model setup is within the range of CMIP5 (Coupled Model Intercomparison Project Phase 5) models. The comparison of model runs with and without land-use change shows a partially warmer and drier climate state across the global land surface. CM2Mc-LPJmL opens new opportunities to investigate important biophysical vegetation–climate feedbacks with a state-of-the-art and process-based dynamic vegetation model.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/10586
dc.identifier.urihttp://dx.doi.org/10.34657/9622
dc.language.isoeng
dc.publisherKatlenburg-Lindau : Copernicus
dc.relation.doihttps://doi.org/10.5194/gmd-14-4117-2021
dc.relation.essn1991-9603
dc.rights.licenseCC BY 4.0 Unported
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subject.ddc910
dc.subject.otherecological modelingeng
dc.subject.othergeneral circulation modeleng
dc.subject.othervegetation typeeng
dc.titleCM2Mc-LPJmL v1.0: biophysical coupling of a process-based dynamic vegetation model with managed land to a general circulation modeleng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIK
wgl.subjectGeowissenschaftenger
wgl.typeZeitschriftenartikelger
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