QBO changes in CMIP6 climate projections

QBO changes in CMIP6 climate projections

Phase six of the Coupled‐Model Intercomparison Project (CMIP6) is the first in which a significant number of models include a well resolved stratosphere. Changes in equatorial stratospheric variability in historical and Shared Socioeconomic Pathways (SSPs) scenario simulations are investigated in te...

Fuld beskrivelse

Bibliografiske detaljer
Main Authors:	Butchart, N, Anstey, JA, Kawatani, Y, Osprey, SM, Richter, JH, Wu, T
Format:	Journal article
Sprog:	English
Udgivet:	American Geophysical Union 2020

Lignende værker

Prospect of increased disruption to the QBO in a changing climate
af: Anstey, JA, et al.
Udgivet: (2021)

Improving the QBO in climate models
af: Anstey, J, et al.
Udgivet: (2021)

The impact of the QBO on the region of the tropical tropopause in QBOi models: Present-day simulations
af: Serva, F, et al.
Udgivet: (2022)

Progress in simulating the Quasi-biennial Oscillation in CMIP models
af: Richter, JH, et al.
Udgivet: (2020)

Report on the SPARC QBO Workshop: The QBO and its Global Influence - Past, Present and Future
af: Anstey, J, et al.
Udgivet: (2017)

QBO Phase Synchronization in CMIP6 Historical Simulations Attributed to Ozone Forcing
af: Neal Butchart, et al.
Udgivet: (2023-08-01)

An evaluation of tropical waves and wave forcing of the QBO in the QBOi models
af: Holt, LA, et al.
Udgivet: (2020)

Prediction of the quasi‐biennial oscillation with a multi‐model ensemble of QBO‐resolving models
af: Stockdale, TN, et al.
Udgivet: (2020)

Impacts, processes and projections of the quasi-biennial oscillation
af: Anstey, J, et al.
Udgivet: (2022)

Teleconnections of the Quasi-Biennial Oscillation in a multi-model ensemble of QBO-resolving models
af: Anstey, JA, et al.
Udgivet: (2021)

The Mediterranean climate change hotspot in the CMIP5 and CMIP6 projections
af: J. Cos, et al.
Udgivet: (2022-02-01)

Synchronisation of the equatorial QBO by the annual cycle in tropical upwelling in a warming climate
af: Rajendran, K, et al.
Udgivet: (2016)

The tropical route of quasi-biennial oscillation (QBO) teleconnections in a climate model
af: J. L. García-Franco, et al.
Udgivet: (2022-07-01)

Time Variability Correction of CMIP6 Climate Change Projections
af: Y. Shao, et al.
Udgivet: (2024-02-01)

The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model
af: Hardiman, S, et al.
Udgivet: (2012)

The tropical route of quasi-biennial oscillation (QBO) teleconnections in a climate model
af: García-Franco, JL, et al.
Udgivet: (2022)

Stratospheric Variability in Twentieth-Century CMIP5 Simulations of the Met Office Climate Model: High Top versus Low Top
af: Osprey, S, et al.
Udgivet: (2013)

The SPARC Quasi‐Biennial Oscillation initiative
af: Anstey, JA, et al.
Udgivet: (2020)

Evaluation of extreme precipitation climate indices and their projected changes for Brazil: From CMIP3 to CMIP6
af: Felipe Jeferson de Medeiros, et al.
Udgivet: (2022-12-01)

Drought characteristics projections based on CMIP6 climate change scenarios in Syria
af: Shifa Mathbout, et al.
Udgivet: (2023-12-01)

Climate sensitivity indices and their relation with projected temperature change in CMIP6 models
af: Linnea L Huusko, et al.
Udgivet: (2021-01-01)

How does the CMIP6 ensemble change the picture for European climate projections?
af: T E Palmer, et al.
Udgivet: (2021-01-01)

Evaluation and Projection of Climate Change in Southwest China Using CMIP6 Models
af: Mingxin YANG, et al.
Udgivet: (2022-12-01)

Changes to population-based emergence of climate change from CMIP5 to CMIP6
af: Hunter C Douglas, et al.
Udgivet: (2022-01-01)

Understanding the mechanisms for tropical surface impacts of the quasi‐biennial oscillation (QBO)
af: García‐Franco, JL, et al.
Udgivet: (2023)

A comparison of CMIP5 and CMIP6 climate model projections for hydrological impacts in China
af: Yawen Lei, et al.
Udgivet: (2023-03-01)

High-resolution climate projection dataset based on CMIP6 for Peru and Ecuador: BASD-CMIP6-PE
af: Carlos Antonio Fernandez-Palomino, et al.
Udgivet: (2024-01-01)

Evaluating permafrost physics in the Coupled Model Intercomparison Project 6 (CMIP6) models and their sensitivity to climate change
af: E. J. Burke, et al.
Udgivet: (2020-09-01)

Changes in the hydro-climatic regime of the Hunza Basin in the Upper Indus under CMIP6 climate change projections
af: Aftab Nazeer, et al.
Udgivet: (2022-12-01)

How well have CMIP3, CMIP5 and CMIP6 future climate projections portrayed the recently observed warming
af: D. Carvalho, et al.
Udgivet: (2022-07-01)

Bioclimatic change as a function of global warming from CMIP6 climate projections
af: M. Sparey, et al.
Udgivet: (2023-01-01)

Climate change multi-model projections in CMIP6 scenarios in Central Hokkaido, Japan
af: Shilei Peng, et al.
Udgivet: (2023-01-01)

Meteorological flash droughts risk projections based on CMIP6 climate change scenarios
af: Vijay Sreeparvathy, et al.
Udgivet: (2022-10-01)

Projection of Climate Variation in Qilian Mountains Based on CMIP6
af: Linjun HAN, et al.
Udgivet: (2022-08-01)

Net effect of the QBO in a chemistry climate model
af: H. J. Punge, et al.
Udgivet: (2008-11-01)

Spatial datasets of CMIP6 climate change projections for Canada and the United StatesNRCAN Climate Archives
af: Daniel W. McKenney, et al.
Udgivet: (2025-02-01)

Assessment on the climate change impact using CMIP6
af: Wan Zunairah, Othman, et al.
Udgivet: (2023)

Climate change in the High Mountain Asia in CMIP6
af: M. Lalande, et al.
Udgivet: (2021-11-01)

Warmer climate projections in EC-Earth3-Veg: the role of changes in the greenhouse gas concentrations from CMIP5 to CMIP6
af: Klaus Wyser, et al.
Udgivet: (2020-01-01)

Climate change impacts on hydrology and water resources in East Africa considering CMIP3, CMIP5, and CMIP6
af: Charles Onyutha
Udgivet: (2024-10-01)