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DOI | 10.1002/2017JD026558 |
Thermodynamic and dynamic influences in the Far East-Okhotsk region on stagnant Meiyu-Baiu | |
Wu, Chi-Hua | |
2017-07-27 | |
发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES |
ISSN | 2169-897X |
EISSN | 2169-8996 |
出版年 | 2017 |
卷号 | 122期号:14 |
文章类型 | Article |
语种 | 英语 |
国家 | Taiwan |
英文摘要 | Westerly perturbation is enlarged over the Far East-Okhotsk region in late June and early July and is associated with the largest land-sea heating contrast surrounding the Sea of Okhotsk. The corresponding characteristics in the lower troposphere are southward deepening of the cold low over northeastern China, and intensification of the Okhotsk high. Coincidentally, the Meiyu-Baiu coupled with the western North Pacific (WNP) subtropical high is nearly stagnant during this period. By simulations using a global climate model with an intensified Okhotsk surface high in response to cooling Sea of Okhotsk, it is suggested that the enhanced thermal contrast over the Far East-Okhotsk region can generate an obstacle to Meiyu-Baiu poleward migration. Corresponding to the intensified Okhotsk high, the WNP subtropical high is strengthened by the high ridge over Taiwan. The East Asian midlatitude westerly jet stream in the northern flank of the WNP subtropical high also strengthens; the consequently enhanced midtropospheric warm temperature advection can regulate the latitude position of the Meiyu-Baiu. The wave source generated in the upper troposphere is located over the midlatitude WNP (anomalous cyclone) bordering the Sea of Okhotsk, whereas that in the lower troposphere is related to the strengthened westerly in the northern WNP subtropical high. The wave activity propagation consistently indicates the strengthening and equatorward confinement of the westerly jet. Therefore, the intensified Okhotsk high and enlarged westerly perturbation beginning in late June are suggested as an inherently geographic limit of the Far East-Okhotsk region in regard to Meiyu-Baiu migration. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000408346000003 |
WOS关键词 | ASIAN SUMMER MONSOON ; WESTERN NORTH PACIFIC ; QUASI-STATIONARY WAVES ; VARYING BASIC FLOW ; ICE-RAFTED DEBRIS ; PART I ; TELECONNECTION PATTERN ; ACTIVITY FLUX ; ROSSBY WAVES ; JET |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/33051 |
专题 | 气候变化 |
作者单位 | Acad Sinica, Res Ctr Environm Changes, Taipei, Taiwan |
推荐引用方式 GB/T 7714 | Wu, Chi-Hua. Thermodynamic and dynamic influences in the Far East-Okhotsk region on stagnant Meiyu-Baiu[J]. JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,2017,122(14). |
APA | Wu, Chi-Hua.(2017).Thermodynamic and dynamic influences in the Far East-Okhotsk region on stagnant Meiyu-Baiu.JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,122(14). |
MLA | Wu, Chi-Hua."Thermodynamic and dynamic influences in the Far East-Okhotsk region on stagnant Meiyu-Baiu".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 122.14(2017). |
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