Atmospheric blocking and patterns of low-frequency variability arising from the breaking of upper level rossby waves
87th AMS Annual Meeting (2007)
The answer is blowing in the wind
Planet Earth (2007) 28-29
Abstract:
The North Atlantic Oscillation (NAO) is a natural climate variability and can be attributed to the UK warming in average winter temperature. Being responsible for both the strength and orientation of the Atlantic jetstream, the NAO is associated with the storm track beneath the jetstream. Changes in NAO is associated with large-scale waves that break in the upper atmosphere. The air waves which stretch for a few thousand kilometers, have some peaks and troughs and when distorted, becomes distorted and collapses into a very turbulent flow.Intercomparison of tropical tropospheric humidity in GCMs with AMSU‐B water vapor data
Geophysical Research Letters American Geophysical Union (AGU) 34:17 (2007)
A golden circle in the sky
Nature Springer Nature 447:7147 (2007) 911-911
Mean age of air and transport in a CTM: Comparison of different ECMWF analyses
Geophysical Research Letters American Geophysical Union (AGU) 34:4 (2007)