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Changes for document MJO and Teleconnections
From version 10.1
edited by S2S_mjotel
on 2020/02/05 23:53
on 2020/02/05 23:53
To version 11.1
edited by S2S_mjotel
on 2020/02/06 00:00
on 2020/02/06 00:00
Change comment: There is no comment for this version
Content changes
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13 | 13 | These two tasks will be tackled in parallel and research activities to address related questions will be spread over the course of sub-project. Specific questions to address include: |
14 | 14 | |
15 | 15 | **a. How well do operational S2S models capture the observed relationship between the MJO and high impact weather events?** |
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16 | 16 | ---- |
17 | 17 | |
18 | 18 | __Current Projects__ |
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23 | 23 | |
24 | 24 | |
25 | 25 | **b. How does the teleconnections depend on the horizontal, vertical and temporal structure of the diabatic heating anomalies associated with the MJO?** |
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26 | 26 | ---- |
27 | 27 | |
28 | 28 | __Current Projects__ |
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34 | 34 | |
35 | 35 | |
36 | 36 | **c. Metrics for assessment of model teleconnections and diagnosing sources of errors in teleconnections** |
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37 | 37 | ---- |
38 | 38 | |
39 | 39 | __Current Projects__ |
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42 | 42 | |
43 | 43 | __Publications__ |
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50 | +* A. M. Jenney, D. A. Randall, E. A. Barnes (2019): Quantifying Regional Sensitivities to Periodic Events: Application to the MJO. //Journal of Geophysical Research//: //Atmospheres, // https:~/~/doi.org/10.1029/2018JD029457 | |
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45 | 45 | **d. Does the relationship between the MJO and high impact weather events lead to enhanced predictive skill for these events for particular phases of the MJO or whilst there is strong MJO activity?** |
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46 | 46 | ---- |
47 | 47 | |
48 | 48 | __Current Projects__ |
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51 | 51 | |
52 | 52 | __Publications__ |
53 | 53 | |
63 | + | |
64 | +* A. M. Jenney, K. M. Nardi, E. A. Barnes, D. A. Randall (2019): The Seasonality and Regionality of MJO Impacts on North American Temperature, //Geophysical Research Letters//, https://doi.org/10.1029/2019GL083950 | |
65 | + | |
66 | +[[image:slides s2s_P2.pdf||alt="The Seasonality and Regionality of MJO Impacts on North American Temperature"]] | |
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54 | 54 | **e. How do variations in the slowly varying background state effect the Rossby wave source and the subsequent Rossby wave propagation from the source region?** |
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55 | 55 | ---- |
56 | 56 | |
57 | 57 | __Current Projects__ |