Model topic: The North Atlantic Oscillation (NAO)
Overview
Teaching: 0 min
Exercises: 0 minQuestions
How to analyze NAO using CMIP6 data?
Objectives
Learn about NAO
Learn to analyze CMIP6 data
Introduction
NAO
The NAO is the dominant atmospheric circulation pattern over the North Atlantic/Europe in winter-spring. NCEP CPC
- How to calculate the NAO index: NCEP CPC NAO indices, UCAR Hurrell station-based NAO index, UCAR Hurrell PC-based NAO index
- Stratospheric impact on the NAO: Scaife et al., 2005
Research question ideas
- How is the frequancy and strength of NAO in CMIP6 models?
- How does it compare with observations?
- Are the impacts on surface climate captured in the models?
- How is the NAO likely to change in a future climate? Under extreme climate change?
Data
- CMIP6 model data: monthly mean sea level pressure; geopotential height; temperature at surface, 500 hPa, and 50 hPa; precipitation
- CMIP6 experiments: historical, SSP585, piControl, abrupt-4xCO2
- Observations: NCEP CPC data, NCDC NOAA figure and data
References
- Lecture slides and material
- NCEP CPC NAO
- A stratospheric influence on the winter NAO and North Atlantic surface climate: Scaife et al., 2005
- NAO and its relationship with the Northern Hemisphere mean surface temperature in CMIP5 simulations: Wang et al., 2017
Key Points
NAO