| 大气低频变化对福建前汛期典型持续性暴雨影响 |
| |
| 引用本文： | 陈彩珠,高建芸,黄丽娜,游立军,林昕,陈琳.大气低频变化对福建前汛期典型持续性暴雨影响[J].应用气象学报,2016,27(1):75-84. |
| |
| 作者姓名： | 陈彩珠 高建芸 黄丽娜 游立军 林昕 陈琳 |
| |
| 作者单位： | 1.福建省厦门市气象局，厦门 361012 |
| |
| 基金项目： | 福建省科技厅科技计划重点项目（2011Y0008），公益性行业（气象）科研专项（GYHY201306067） |
| |
| 摘 要： | 在分析福建前汛期典型持续性暴雨过程大气低频变化特征基础上，建立了福建前汛期典型持续性暴雨大气低频扰动物理概念模型:典型持续性暴雨发生期间，对流层高层朝鲜半岛至渤海湾为低频低压，青藏高原西侧为弱高压，副热带西风急流核位于长江口至东海上空，福建上空为低频辐散区；对流层中层高度场低频分量中高纬度地区若出现贝加尔湖阻塞高压加强型、乌拉尔山及鄂霍次克海双阻塞高压加强型、鄂霍次克海阻塞高压加强型和乌拉尔山阻塞高压加强型4种低频扰动之一，福建上空为低频低值区；对流层低层低频流场福建上空为低频气旋控制，气旋中心位于江南或南海上空，如此高低空低频系统配置将引起异常的低频垂直经向环流，从而导致典型持续性暴雨的形成。
|
| 关 键 词： | 前汛期 持续性暴雨 低频变化 物理概念模型 |
| 收稿时间： | 2/3/2015 12:00:00 AM |
Effects of Atmospheric Low frequency Variation on Typical Persistent Heavy Rains During Pre flood Season in Fujian |
| |
| Chen Caizhu,Gao Jianyun,Huang Lin,You Lijun,Lin Xin and Chen Lin.Effects of Atmospheric Low frequency Variation on Typical Persistent Heavy Rains During Pre flood Season in Fujian[J].Quarterly Journal of Applied Meteorology,2016,27(1):75-84. |
| |
| Authors: | Chen Caizhu Gao Jianyun Huang Lin You Lijun Lin Xin and Chen Lin |
| |
| Affiliation: | 1.Xiamen Meteorological Bureau of Fujian Province, Xiamen 3610122.Fujian Provincial Climate Center, Fuzhou 3500013.Putian Meteorological Office of Fujian Province, Putian 351100 |
| |
| Abstract: | The daily precipitation data of 66 stations in Fujian and NCEP reanalysis data during 1961-2010 are used to analyze the atmospheric low-frequency (LF) variability responsible for 27 typical persistent heavy rain processes (TPHRP) in Fujian during pre-flood season. Using Butterworth band-pass filtering method, low frequency band signals of 30-60 d intraseasonal oscillation (ISO) are extracted from filtered air circulation time series grid data. A physical conceptual model about the atmospheric LF disturbances during TPHRP is suggested as follows.In the upper troposphere, LF between the Korean Peninsula and the Bohai Gulf is low and weak high system dominates in the west of the Tibet Plateau, together with the subtropical westerly jet (SWJ) core located between the Yangtze River estuary and the East China Sea, leading to the LF divergence over Fujian. These low-frequency systems are relative to the Northeast cold vortex, South Asia high and the subtropical westerly jet core, respectively, which provide high-level divergence dynamic conditions and driving dynamic conditions of vertical circulation for persistent heavy rains.In the middle troposphere, when LF disturbance pattern as double block high enhanced type, the Ural block high enhanced type, the Lake Baikal block high enhanced type, or the Okhotsk Sea block high enhanced type, LF low may maintain over Fujian showing on the weather map as two troughs and one ridge type, two ridges and one trough type, one trough and one ridge type, one ridge and one ridge type, respectively. The cold air from the middle and east influences Fujian, providing continuous cold air for persistent heavy rain processes.In the lower troposphere, there is a LF cyclone over Fujian with its center located in South China Sea (SCS) or south of the Yangtze River. The current of air from subtropical high provide continuous moisture conditions, low level convergence dynamic conditions, instability stratification conditions and maintain low-level vertical circulation dynamic conditions for persistent heavy rain processes.In vapor flux fields, whenever one of the LF disturbance strengthens in the vapor passageways as Somali to the Bay of Bengal, the western flank of the Western Pacific Subtropical High (WPSH) or the westerly transport, the water vapor flux convergence over Fujian will be enhanced, providing continuous water vapor transport. TPHRPs are finally triggered by the abnormal LF circulation configuration from lower to upper troposphere as above with favorable synoptic systems for heavy persisted rains. Because of the LF system with continuous and periodicity, the physical conceptual model provides scientific basis for the extension of the TPHRP forecast in Fujian during pre-flood season. |
| |
| Keywords: | |
|
| 点击此处可从《应用气象学报》浏览原始摘要信息 |
|
点击此处可从《应用气象学报》下载全文 |
|
