Diurnal phase of late-night against late-afternoon of stratiform and convective precipitation in summer southern contiguous china
文献类型：期刊论文
| 作者 | Yu, Rucong1,2; Yuan, Weihua2,3; Li, Jian1; Fu, Yunfei2,4 |
| 刊名 | Climate dynamics
 |
| 出版日期 | 2010-09-01 |
| 卷号 | 35期号:4页码:567-576 |
| 关键词 | Diurnal cycle Stratiform precipitation Convective precipitation Rainfall duration |
| ISSN号 | 0930-7575 |
| DOI | 10.1007/s00382-009-0568-x |
| 通讯作者 | Yu, rucong(yrc@cma.gov.cn) |
| 英文摘要 | Using the tropical rainfall measuring mission (trmm) precipitation radar (pr) observations combined with the surface rain gauge data during 1998-2006, the robust diurnal features of summer stratiform and convective precipitation over the southern contiguous china are revealed by exploring the diurnal variations of rain rate and precipitation profile. the precipitation over the southern contiguous china exhibits two distinguishing diurnal phases: late-night (2200-0600 lst) and late-afternoon (1400-2200 lst), dependent on the location, precipitation type and duration time. generally, the maximum rain rate and the highest profile of stratiform precipitation occur in the late-afternoon (late-night) over the southeastern (southwestern) china, while most of the stratiform short-duration rain rate tends to present late-afternoon peaks over the southern china. for convective precipitation, the maximum rain rate and the highest profile occur in the late-afternoon over most of the southern contiguous china, while the convective long-duration rain rate exhibits late-night peaks over the southwestern china. without regional dependence, the convective precipitation exhibits much larger amplitude of diurnal variations in both near surface rain rate and vertical extension compared with stratiform precipitation and the convective rain top rises most rapidly between noon and afternoon. however, there are two distinctive sub-regions. the diurnal phases of precipitation there are very weakly dependent on precipitation type and duration time. over the eastern periphery of the tibetan plateau, the maximum rain rate and the highest profile of either convective or stratiform precipitation occur in the late-night. over the southeastern coastal regions, both the near surface rain rate and rain top of convective and stratiform precipitation peak in the late-afternoon. |
| WOS关键词 | UNITED-STATES ; TRMM ; RAINFALL ; RADAR ; CYCLE ; PROFILES |
| WOS研究方向 | Meteorology & Atmospheric Sciences |
| WOS类目 | Meteorology & Atmospheric Sciences |
| 语种 | 英语 |
| WOS记录号 | WOS:000281377200001 |
| 出版者 | SPRINGER |
| URI标识 | http://www.irgrid.ac.cn/handle/1471x/2415298 |
| 专题 | 中国科学院大学 |
| 通讯作者 | Yu, Rucong |
| 作者单位 | 1.Chinese Acad Meteorol Sci, LaSW, China Meteorol Adm, Beijing, Peoples R China 2.Chinese Acad Sci, Inst Atmospher Phys, LASG, Beijing, Peoples R China 3.Chinese Acad Sci, Grad Sch, Beijing, Peoples R China 4.Univ Sci & Technol China, Lab Satellite Remote Sensing & Climate Environm, Hefei 230026, Anhui, Peoples R China |
| 推荐引用方式 GB/T 7714 | Yu, Rucong,Yuan, Weihua,Li, Jian,et al. Diurnal phase of late-night against late-afternoon of stratiform and convective precipitation in summer southern contiguous china[J]. Climate dynamics,2010,35(4):567-576. |
| APA | Yu, Rucong,Yuan, Weihua,Li, Jian,&Fu, Yunfei.(2010).Diurnal phase of late-night against late-afternoon of stratiform and convective precipitation in summer southern contiguous china.Climate dynamics,35(4),567-576. |
| MLA | Yu, Rucong,et al."Diurnal phase of late-night against late-afternoon of stratiform and convective precipitation in summer southern contiguous china".Climate dynamics 35.4(2010):567-576. |
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来源：中国科学院大学
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