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DOI | 10.1002/joc.6914 |
Summer precipitation characteristics on the southern Tibetan plateau | |
Zeng, Chen; Zhang, Fan; Wang, Li; Chen, Deliang | |
通讯作者 | Zhang, F (通讯作者) |
发表日期 | 2021 |
ISSN | 0899-8418 |
EISSN | 1097-0088 |
起始页码 | E3160 |
结束页码 | E3177 |
卷号 | 41 |
英文摘要 | Precipitation is an important source of streamflow and a critical parameter in hydrological studies. However, spatiotemporal variation of precipitation in the Tibetan Plateau (TP) has been poorly characterized due to the limited distribution of meteorological stations mostly in the lowlands. In this study, we set-up rain gauges to study summer precipitation on mountain slopes in three catchments of the southern TP from 2013 to 2016. We studied the precipitation gradients (PGs) averaged during the Indian monsoon season (PG(ms)), as well as daily PGs (PG(d)) and unit PGs (PG(u)) under various precipitation intensity grades (PIGs) and subdiurnal precipitation distributions. We also analysed the correlations between the PGs and precipitation amounts under various PIGs. Results showed that the mean PG(ms), PG(d) and PG(u) in the study catchments were 0.0071-0.0082% for monsoon season, 0.11-0.13 mm center dot 100 m(-1) d(-1) and 2.2-3.1%center dot 100 m(-1) for the total (nonintensity-graded) precipitation, but varied widely under different PIGs. PG(ms), PG(d) and PG(u) were all strongly correlated to precipitation amounts, which were relatively consistent between years but varied between different catchments. In addition, the correlations showed a steep positive slope under fine precipitation but became flat or even negative with increasing PIG. Generally, two distinct precipitation peaks were noted in each of the three catchments: a dispersed peak in the morning, and a stronger but sharper peak at around 18:00 LST; overall, this subdiurnal pattern was temporally stable. The mean precipitation durations of the three catchments were approximately 1.0-1.4 hr (nonintensity-graded) and increased from <0.5 hr, to <1 hr, 2-5 hr and 6-11 hr for trace, light, moderate and heavy precipitation intensities, respectively. Among the various PG units, both PG(d) and PG(u) better represented precipitation at different altitudes than that of PG(ms). Summer precipitation in the study catchments was influenced more by valley-scale convection than by large-scale monsoon circulation. |
关键词 | GRADIENTSSEASONALITYVARIABILITYCATCHMENTRAINFALLWEATHEREROSIONCLIMATERUNOFFCHINA |
英文关键词 | precipitation duration; precipitation gradient; precipitation intensity; subdiurnal distribution; Tibetan Plateau |
语种 | 英语 |
WOS研究方向 | Meteorology & Atmospheric Sciences |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS记录号 | WOS:000587237200001 |
来源期刊 | INTERNATIONAL JOURNAL OF CLIMATOLOGY |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/260350 |
推荐引用方式 GB/T 7714 | Zeng, Chen,Zhang, Fan,Wang, Li,et al. Summer precipitation characteristics on the southern Tibetan plateau[J]. 中国科学院青藏高原研究所,2021,41. |
APA | Zeng, Chen,Zhang, Fan,Wang, Li,&Chen, Deliang.(2021).Summer precipitation characteristics on the southern Tibetan plateau.INTERNATIONAL JOURNAL OF CLIMATOLOGY,41. |
MLA | Zeng, Chen,et al."Summer precipitation characteristics on the southern Tibetan plateau".INTERNATIONAL JOURNAL OF CLIMATOLOGY 41(2021). |
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