The global aerosol-climate model ECHAM6.3-HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing and climate sensitivity
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
The global aerosol-climate model ECHAM6.3-HAM2.3 – Part 2: Cloud evaluation, aerosol radiative forcing and climate sensitivity ; year:2019 ; pages:1-52
Geoscientific model development discussions ; (2019), 1-52
- Urheber
-
Neubauer, David
Ferrachat, Sylvaine
Siegenthaler-Le Drian, Colombe
Stier, Philip
Partridge, Daniel G.
Tegen, Ina
Bey, Isabelle
Stanelle, Tanja
Kokkola, Harri
Lohmann, Ulrike
- DOI
-
10.5194/gmd-2018-307
- URN
-
urn:nbn:de:101:1-2019031404360513544465
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
14.08.2025, 10:51 MESZ
Datenpartner
Dieses Objekt wird bereitgestellt von:
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Deutsche Nationalbibliothek. Bei Fragen zum Objekt wenden Sie sich bitte an den Datenpartner.
Beteiligte
- Neubauer, David
- Ferrachat, Sylvaine
- Siegenthaler-Le Drian, Colombe
- Stier, Philip
- Partridge, Daniel G.
- Tegen, Ina
- Bey, Isabelle
- Stanelle, Tanja
- Kokkola, Harri
- Lohmann, Ulrike
Ähnliche Objekte (12)
Radiative forcing and climate sensitivity
Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG
Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG
Radiative forcing and climate response to projected 21st century aerosol decreases
Aerosol absorption and radiative forcing
Sensitivity of global direct aerosol radiative forcing to uncertainties in aerosol optical properties
Stratospheric aerosol radiative forcing simulated by the chemistry climate model EMAC using Aerosol CCI satellite data
Stratospheric aerosol radiative forcing simulated by the chemistry climate model EMAC using aerosol CCI satellite data
Sensitivity of global direct aerosol shortwave radiative forcing to uncertainties in aerosol optical properties
Identifying climate model structural inconsistencies allows for tight constraint of aerosol radiative forcing
Decrease in radiative forcing by organic aerosol nucleation, climate, and land use change
Identifying climate model structural inconsistencies allows for tight constraint of aerosol radiative forcing
Radiative forcing and climate sensitivity
Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG
Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG
Radiative forcing and climate response to projected 21st century aerosol decreases
Aerosol absorption and radiative forcing
Sensitivity of global direct aerosol radiative forcing to uncertainties in aerosol optical properties
Stratospheric aerosol radiative forcing simulated by the chemistry climate model EMAC using Aerosol CCI satellite data
Stratospheric aerosol radiative forcing simulated by the chemistry climate model EMAC using aerosol CCI satellite data
Sensitivity of global direct aerosol shortwave radiative forcing to uncertainties in aerosol optical properties
Identifying climate model structural inconsistencies allows for tight constraint of aerosol radiative forcing
Decrease in radiative forcing by organic aerosol nucleation, climate, and land use change
Identifying climate model structural inconsistencies allows for tight constraint of aerosol radiative forcing
Radiative forcing and climate sensitivity
Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG
Effective radiative forcing in the aerosol–climate model CAM5.3-MARC-ARG
Radiative forcing and climate response to projected 21st century aerosol decreases
Aerosol absorption and radiative forcing
Sensitivity of global direct aerosol radiative forcing to uncertainties in aerosol optical properties
Stratospheric aerosol radiative forcing simulated by the chemistry climate model EMAC using Aerosol CCI satellite data
Stratospheric aerosol radiative forcing simulated by the chemistry climate model EMAC using aerosol CCI satellite data
Sensitivity of global direct aerosol shortwave radiative forcing to uncertainties in aerosol optical properties
Identifying climate model structural inconsistencies allows for tight constraint of aerosol radiative forcing
Decrease in radiative forcing by organic aerosol nucleation, climate, and land use change