Solar cycle variations of stratospheric ozone and temperature in simulations of a coupled chemistry-climate model
- Standort
-
Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
-
Online-Ressource
- Sprache
-
Englisch
- Erschienen in
-
Solar cycle variations of stratospheric ozone and temperature in simulations of a coupled chemistry-climate model ; volume:7 ; number:6 ; year:2007 ; pages:1693-1706
Atmospheric chemistry and physics ; 7, Heft 6 (2007), 1693-1706
- Urheber
-
Austin, J.
Hood, L. L.
Soukharev, B. E.
- DOI
-
10.5194/acp-7-1693-2007
- URN
-
urn:nbn:de:101:1-20171215927
- Rechteinformation
-
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
-
15.08.2025, 07:29 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
- Austin, J.
- Hood, L. L.
- Soukharev, B. E.
Ähnliche Objekte (12)
Inconsistencies between chemistry–climate models and observed lower stratospheric ozone trends since 1998
Observations of large stratospheric ozone variations over Mendoza, Argentina
On ozone trend detection: using coupled chemistry–climate simulations to investigate early signs of total column ozone recovery
Quantitative performance metrics for stratospheric-resolving chemistry-climate models
Global distribution of total ozone and lower stratospheric temperature variations
Polar stratospheric clouds initiated by mountain waves in a global chemistry–climate model: a missing piece in fully modelling polar stratospheric ozone depletion
Hemispheric ozone variability indices derived from satellite observations and comparison to a coupled chemistry-climate model
Sensitivity of the tropical stratospheric ozone response to the solar rotational cycle in observations and chemistry–climate model simulations
Correcting ozone biases in a global chemistry-climate model: implications for future ozone
Correcting ozone biases in a global chemistry–climate model: implications for future ozone
Stratospheric Aerosol Intervention Experiment for the Chemistry-Climate Model Intercomparison Project
Impact of large solar zenith angles on lower stratospheric dynamical and chemical processes in a coupled chemistry-climate model
Inconsistencies between chemistry–climate models and observed lower stratospheric ozone trends since 1998
Observations of large stratospheric ozone variations over Mendoza, Argentina
On ozone trend detection: using coupled chemistry–climate simulations to investigate early signs of total column ozone recovery
Quantitative performance metrics for stratospheric-resolving chemistry-climate models
Global distribution of total ozone and lower stratospheric temperature variations
Polar stratospheric clouds initiated by mountain waves in a global chemistry–climate model: a missing piece in fully modelling polar stratospheric ozone depletion
Hemispheric ozone variability indices derived from satellite observations and comparison to a coupled chemistry-climate model
Sensitivity of the tropical stratospheric ozone response to the solar rotational cycle in observations and chemistry–climate model simulations
Correcting ozone biases in a global chemistry-climate model: implications for future ozone
Correcting ozone biases in a global chemistry–climate model: implications for future ozone
Stratospheric Aerosol Intervention Experiment for the Chemistry-Climate Model Intercomparison Project
Impact of large solar zenith angles on lower stratospheric dynamical and chemical processes in a coupled chemistry-climate model
Inconsistencies between chemistry–climate models and observed lower stratospheric ozone trends since 1998
Observations of large stratospheric ozone variations over Mendoza, Argentina
On ozone trend detection: using coupled chemistry–climate simulations to investigate early signs of total column ozone recovery
Quantitative performance metrics for stratospheric-resolving chemistry-climate models
Global distribution of total ozone and lower stratospheric temperature variations
Polar stratospheric clouds initiated by mountain waves in a global chemistry–climate model: a missing piece in fully modelling polar stratospheric ozone depletion
Hemispheric ozone variability indices derived from satellite observations and comparison to a coupled chemistry-climate model
Sensitivity of the tropical stratospheric ozone response to the solar rotational cycle in observations and chemistry–climate model simulations
Correcting ozone biases in a global chemistry-climate model: implications for future ozone
Correcting ozone biases in a global chemistry–climate model: implications for future ozone
Stratospheric Aerosol Intervention Experiment for the Chemistry-Climate Model Intercomparison Project