Discussion of the Effects and Implications of an Increase in Atmospheric CO2 Concentrations on the Jetstreams and on Eastward-Moving Air in the Mid-Latitudes
1. Introduction
2. Polar-Equatorial Temperature Gradient and Speed of the Jetstream
3. Conservation of Potential Vorticity
4. Forced Standing Waves Derivation
5. Forced Standing Waves Discussion
6. Plane-Wave Solutions to Conservation of Potential Vorticity
7. Changes in the Wave-Pattern over Time
8. Summary
9. Quantification of Expected Change
10. Discussion & Conclusion
1. INTRODUCTION:
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