• Aucun résultat trouvé

SEMINAIRE CNRM

N/A
N/A
Protected

Academic year: 2022

Partager "SEMINAIRE CNRM"

Copied!
1
0
0

Texte intégral

(1)

CNRM, UMR 3589

SEMINAIRE CNRM

jeudi 24 juin 2021 à 11h

THE ROLE OF EARTH SYSTEM INTERACTIONS IN THE PRESENT-DAY FORCING OF CLIMATE

par Fiona O'Connor (UKMO)

en visioconférence Code bj = https://bluejeans.com/715108137/4349

Abstract: Quantifying forcings from anthropogenic perturbations to the Earth system (ES) is important for understanding changes in climate since the pre-industrial (PI) period and into the future. Here, using a range of model experiments following the protocols defined by the Radiative Forcing Model Intercomparison Project (RFMIP) and the Aerosol and Chemistry Model Intercomparison Project (AerChemMIP), we quantify and analyse a wide range of present-day (PD) anthropogenic effective radiative forcings (ERFs). Quantifying ERFs that include rapid adjustments within a full Earth System Model (ESM) enables the role of various chemistry–aerosol–cloud interactions to be investigated.

The anthropogenic perturbations analysed include changes in greenhouse gas concentrations, aerosol and aerosol precursor emissions, ozone precursor emissions, and land use. For methane and non-methane ozone precursors, their ERFs are strongly influenced by cloud adjustments through chemistry-aerosol-cloud interactions. In the case of methane, these interactions increase the magnitude of the forcing but in the case of nitrogen oxides, cloud adjustments offset the forcing from ozone. These chemistry- aerosol-cloud interactions also give rise to non-linearities in forcing when different anthropogenic perturbations are applied in combination. A process-based understanding of these interactions will be presented and the work suggests that rapid adjustments included in ERF estimates need to include chemical as well as physical adjustments to fully account for complex ES interactions.

Bio: Fiona is a climate scientist working on atmospheric chemistry, with a particular interest in methane, chemistry-climate interactions, and climate system feedbacks.

https://www.metoffice.gov.uk/research/people/fiona-oconnor --

Pour tout renseignement, contacter Y. Poirier (05 61 07 96 55) Centre National de Recherches Météorologiques

42, Avenue G. Coriolis - 31057 Toulouse Cedex

Références

Documents relatifs

ECHAM5-HAM2 CAM5.1-PNNL IMPACT LMDZ LMDZ-39L GOCART-GEOS4 GOCART-MERRA OsloCTM2 MPI-2stream HadGEM2-ES SPRINTARS GEOS-CHEM ECHAM5-HAM2 CAM5.1-PNNL IMPACT LMDZ LMDZ-39L

This paper presents decadal simulations of strato- spheric and tropospheric aerosol and its radiative effects by the chemistry general circulation model EMAC constrained with

This paper illustrates the design of the idealized volcanic perturbation experiments in the VolMIP protocol and describes the com- mon aerosol forcing input data sets to be used..

Comparison of the runoff ratio (ratio of total runoff to rainfall) to the ratio of latent heat to net radiation flux. Each dot represents an LSM simula- tion averaged over the

Notice 1989 versus right Emanuel 1993 schemes in the AMMA-CROSS framethat part of the changes work for July: a mean meridional circulation streamlines and mean zonal obtained over

That foundation in- cludes (1) the OMIP-BGC protocols for groups that will in- clude inert chemical tracers and biogeochemistry in OMIP’s two forced global ocean model

I looked toward the doorways at either end of the long room, but the only people around seemed to be the guests at the table.. I noticed that some of the

The influence of the openings on the nonlinear moment-rotation curve part is insignificant if extended end-plate is used instead of flush end-plate (figure 7b).