SCIENTIA SINICA Terrae, Год журнала: 2023, Номер 53(11), С. 2623 - 2638
Опубликована: Сен. 4, 2023
SCIENTIA SINICA Terrae, Год журнала: 2023, Номер 53(11), С. 2623 - 2638
Опубликована: Сен. 4, 2023
Journal of Geophysical Research Atmospheres, Год журнала: 2025, Номер 130(5)
Опубликована: Фев. 28, 2025
Abstract It was previously revealed that winter precipitation in East Asia is linked to tropical Sea Surface Temperature (SST) anomalies the Indian and Pacific Oceans. While several teleconnection pathways have been identified, accurately measuring these connections determining relative contributions of SSTs remains a challenge. We employed novel causal inference approach quantify effects on Asian precipitation, focusing its leading mode (denoted as Pr). Using PCMCI method, we first derived graph between Pr eastern/western Ocean EP, WP, IO respectively). Based graph, then applied quantitative analysis using Wright's path method. The results indicated WP‐SST had most substantial impact Pr, with 1 Standard Deviation (SD) increase 0.24 SD decrease at 1‐month lag 0.17 2‐month lag. monsoon winds subtropical jet stream are identified critical mediators this effect. Additionally, EP‐SST notable positive influence warming 0.12 lag, while IO‐SST exhibits minor essential note that, traditional regression indicates explained largest portion variance among three SSTs, but exerts more significant role driving variations, aligning numerical experiments.
Язык: Английский
Процитировано
1Atmospheric Research, Год журнала: 2023, Номер 293, С. 106928 - 106928
Опубликована: Июль 16, 2023
Язык: Английский
Процитировано
10Water, Год журнала: 2025, Номер 17(2), С. 219 - 219
Опубликована: Янв. 15, 2025
Winter precipitation (P) in East Asia (EA) is characterized by a wetter south and drier north. Most of the existing research has concentrated on elucidating mechanisms winter P southern EA, with relatively less attention given to northern (NEA). Our analysis showed that correlation coefficient (c.c.) average anomaly percentage (PAP) between EA NEA 0.24 for period 1950–2023, indicating substantial regional difference. An empirical orthogonal function (EOF) was conducted PAP NEA. The first second mode (EOF1 EOF2) account 45.5% 17.9% total variance, respectively. EOF1 region-wide uniform spatial pattern whereas EOF2 exhibits north–south dipole pattern. Further indicated two EOF modes are related distinct atmospheric circulation external forcings. Specifically, linked wave train from Central Siberia toward Japan, while connected an similar Western Pacific Variations mid–high latitude sea surface temperatures, ice, snow potential factors influencing EOF1. close relationship tropical SST anomalies.
Язык: Английский
Процитировано
0Geophysical Research Letters, Год журнала: 2023, Номер 50(4)
Опубликована: Фев. 24, 2023
Abstract The PM 2.5 (fine particulate matter with diameter ≤2.5 μm) concentration anomalies over the North China Plain (NCP) in early and late winter sometimes show a subseasonal reversal, which brings great challenge for precise control of air pollution, mechanisms are not well understood. This paper reveals key role Barents Sea sea‐ice this reversal. In winter, negative Scandinavian‐like pattern causes an anticyclonic anomaly Northeast Asia thus leads to positive NCP. addition, anomalous warm advection associated Atlantic Oscillation‐like accelerates loss Sea, especially increases surface turbulent heating flux. These Polar/Eurasian‐like that induces cyclonic eventually NCP winter. Vice versa.
Язык: Английский
Процитировано
8Science China Earth Sciences, Год журнала: 2023, Номер 66(11), С. 2579 - 2593
Опубликована: Окт. 12, 2023
Язык: Английский
Процитировано
2Journal of Geophysical Research Atmospheres, Год журнала: 2024, Номер 129(14)
Опубликована: Июль 18, 2024
Abstract The Antarctic Oscillation (AAO), which is the main mode of extratropical circulation in Southern Hemisphere, also has a substantial effect on Northern Hemisphere climate. We investigated influence early AAO frequency late severe pollution events (SPEF) Beijing–Tianjin–Hebei region (SPEF BTH ) China during winter. results show that winter (December–January–February) SPEF negatively correlated with from previous autumn (August–September–October). controlling mechanism can be briefly described as follows: positively mid‐latitude sea surface temperature (SST) South Atlantic Ocean. SST preserves anomaly signal into following This anomalous regulates changes tropical western Indian Ocean–Intertropical Convergence Zone (IN–ITCZ) via air–sea coupling. Subsequently, response to IN–ITCZ anomalies, wave trains are excited upper troposphere Ocean East Asia. In addition, local meridional modulated; therefore, field and other meteorological elements favorable for appear exacerbate . study describes new physical pathway subsequent finds predictable source system.
Язык: Английский
Процитировано
0Climate Dynamics, Год журнала: 2024, Номер unknown
Опубликована: Авг. 30, 2024
Язык: Английский
Процитировано
0SCIENTIA SINICA Terrae, Год журнала: 2023, Номер 53(11), С. 2623 - 2638
Опубликована: Сен. 4, 2023
Процитировано
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