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6. Northern Hemisphere Stratosphere‐Troposphere Circulation Change in CMIP6 Models: 2. Mechanisms and Sources of the Spread.

8. Sub-seasonal Predictability and the Stratosphere

9. Contributors

16. Extreme weather in the Southern Hemisphere in early 2022: from Rossby waves to planetary-scale conditions

19. Advances in the Subseasonal Prediction of Extreme Events: Relevant Case Studies across the Globe

24. Teleconnection-driven extreme events: Relevant case studies

27. Recent advances in the application and utility of subseasonal-to-seasonal predictions

30. Teleconnection-driven sub-seasonal predictability of extreme events: Relevant case studies

40. Current and emerging developments in subseasonal to decadal prediction

41. Sudden Stratospheric Warmings

43. The Role of the Stratosphere in Subseasonal to Seasonal Prediction: 1. Predictability of the Stratosphere

44. The effect of the equatorial Pacific cold SST bias on simulated ENSO teleconnections to the North Pacific and California

45. Long Range Prediction and the Stratosphere.

46. How linear is the ENSO Teleconnection to the North Pacific? The Role of ENSO Atmospheric Feedbacks for Rainfall in California

50. Improved teleconnection‐based dynamical seasonal predictions of boreal winter

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