Enhanced mid-to-late winter predictability of the storm track variability in the North Pacific as a contrast with the North Atlantic
Bibliographic Data
| ID | 15544950 |
|---|---|
| Authors | Yu Nie (0000-0003-2083-470X, China Meteorological Administration), Hong‐Li Ren (0000-0001-7194-0567, China Meteorological Administration, corresponding author), Adam A Scaife (0000-0002-5189-7538, Met Office) |
| Year | 2020 |
| Volume | 15 |
| Issue | 9 |
| Pages | 094037-094037 |
| Publication date | 2020-06-12 |
| Peer Reviewed | Yes |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/ab9c4d |
| OpenAlex | W3034208377 |
| Language | EN |
| Citations received | 1 |
| References cited | 47 |
The storm tracks are a major driver of regional extreme weather events. Using the daily output of reanalysis and a latest generation ensemble seasonal forecasting system, this study examines the interannual variability and predictability of the boreal winter storm tracks in the North Pacific and North Atlantic. In both basins, the leading mode of storm track variability describes a latitudinal shifting of the climatological storm tracks. The shifting mode is closely connected with the extratropical large-scale teleconnection patterns (i.e. Pacific-North America teleconnection and North Atlantic Oscillation). The main predictability source for the shifting mode of the North Pacific storm tracks are the ENSO-related sea surface temperature anomalies. Assessment of the seasonal prediction skill further shows that the shifting mode of the North Pacific storm tracks is in general better predicted than that of the North Atlantic storm tracks likely due to stronger ENSO effects. Our analyses also find that, through the modulations of ENSO and the subtropical jet, the shifting mode of the North Pacific storm tracks exhibit a mid-to-late winter predictability enhancement. During El Niño phases, the North Pacific subtropical jet shifts equatorward and becomes strongest in mid-to-late winter, which dominates the upper-level flow and guides the storm track most equatorward. We argue that the intensification and equatorward shift of the North Pacific subtropical jet in mid-to-late winter of El Niño years provide the main reason for the increased mid-to-late winter predictability for the storm tracks. The results imply that good representation of the background subtropical jet in models is important for winter climate prediction of storm tracks
Climatology · El Niño Southern Oscillation · Extratropical cyclone · North Atlantic oscillation · Pacific decadal oscillation · Predictability · Sea surface temperature · Storm · Storm track · Subtropics · Teleconnection · Winter storm · Climate variability and models · Environmental Science · Meteorological Phenomena and Simulations · Oceanographic and Atmospheric Processes · Geology · Oceanography
The ERA‐Interim reanalysis
Recent Arctic amplification and extreme mid-latitude weather
Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century
Stratospheric initial conditions provide seasonal predictability of the North Atlantic and Arctic Oscillations
| Unique citing works | 1 |
|---|---|
| Citations per year | 0,2 |
| Citation span | 2021 - 2021 (1) |
| Citation velocity | historical |
| Highly cited | No |
| Citation types | Neutral: 1 |