ESD Ideas: The stochastic climate model shows that underestimated Holocene trends and variability represent two sides of the same coin
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
ESD Ideas: The stochastic climate model shows that underestimated Holocene trends and variability represent two sides of the same coin ; year:2018 ; pages:1-5
Earth System Dynamics Discussions ; (2018), 1-5
- Urheber
- DOI
-
10.5194/esd-2018-43
- URN
-
urn:nbn:de:101:1-2018062807152503819202
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:34 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
Ähnliche Objekte (12)
Temperatures from Energy Balance Models: the effective heat capacity matters
Impact of model resolution on Holocene climate simulations of the Northern Hemisphere
Water isotopes – climate relationships for the mid-Holocene and preindustrial period simulated with an isotope-enabled version of MPI-ESM
Water isotopes – climate relationships for the mid-Holocene and pre-industrial period simulated with an isotope-enabled version of MPI-ESM
Dynamic soil feedbacks on the climate of the mid-Holocene and the last glacial maximum
Including the efficacy of land ice changes in deriving climate sensitivity from paleodata
Including the efficacy of land ice changes in deriving climate sensitivity from paleodata
Variability and extremes: Statistical validation of the AWI-ESM
Variability and extremes: statistical validation of the Alfred Wegener Institute Earth System Model (AWI-ESM)
Brief communication: An Ice surface melt scheme including the diurnal cycle of solar radiation
A model-data comparison of the Last Glacial Maximum surface temperature changes
The linkage between autumn Barents-Kara sea ice and European cold winter extremes
Temperatures from Energy Balance Models: the effective heat capacity matters
Impact of model resolution on Holocene climate simulations of the Northern Hemisphere
Water isotopes – climate relationships for the mid-Holocene and preindustrial period simulated with an isotope-enabled version of MPI-ESM
Water isotopes – climate relationships for the mid-Holocene and pre-industrial period simulated with an isotope-enabled version of MPI-ESM
Dynamic soil feedbacks on the climate of the mid-Holocene and the last glacial maximum
Including the efficacy of land ice changes in deriving climate sensitivity from paleodata
Including the efficacy of land ice changes in deriving climate sensitivity from paleodata
Variability and extremes: Statistical validation of the AWI-ESM
Variability and extremes: statistical validation of the Alfred Wegener Institute Earth System Model (AWI-ESM)
Brief communication: An Ice surface melt scheme including the diurnal cycle of solar radiation
A model-data comparison of the Last Glacial Maximum surface temperature changes
The linkage between autumn Barents-Kara sea ice and European cold winter extremes
Temperatures from Energy Balance Models: the effective heat capacity matters
Impact of model resolution on Holocene climate simulations of the Northern Hemisphere
Water isotopes – climate relationships for the mid-Holocene and preindustrial period simulated with an isotope-enabled version of MPI-ESM
Water isotopes – climate relationships for the mid-Holocene and pre-industrial period simulated with an isotope-enabled version of MPI-ESM
Dynamic soil feedbacks on the climate of the mid-Holocene and the last glacial maximum
Including the efficacy of land ice changes in deriving climate sensitivity from paleodata
Including the efficacy of land ice changes in deriving climate sensitivity from paleodata
Variability and extremes: Statistical validation of the AWI-ESM
Variability and extremes: statistical validation of the Alfred Wegener Institute Earth System Model (AWI-ESM)
Brief communication: An Ice surface melt scheme including the diurnal cycle of solar radiation
A model-data comparison of the Last Glacial Maximum surface temperature changes