| 涂长望,许鉴明. 1936. 峨眉山之雨量[J]. 气象学报, 12(10):560-573, doi:10.11676/qxxb1936.074 |
| 峨眉山之雨量 |
| Thr Exceptionally Heavy Precipitation of Omeishan |
| |
| DOI：10.11676/qxxb1936.074 |
| 中文关键词: |
| 英文关键词: |
| 基金项目: |
|
| 摘要点击次数: 2415 |
| 全文下载次数: 2040 |
| 中文摘要: |
| 地理位置欲充分了解峨眉多雨之原因必先明瞭其地理位置。峨眉位北纬二十九度二十八分,东经一○三度四十一分,居四川西南部,去省会成都一五○公里。 |
| 英文摘要: |
| In the thirteen months from August 193.3 to August 1934 Omeishan registered 9225mm. of rainfall. This amount is exceptionally heavy for a mountain which is not more than 3100m. in height and situated in (innermost China), not far from Chengtu. This extraordinarily heavy Frecipitation has heen found to he caused by the interaclion of a multiple of factors, such as topography, convection and the number of cyclones. High mountains forced the SW, or SE. monsoon to ascend, while ascending the relative humidity of the marine air is increased and when this humid air is forced to rise still higher either by cenvection or by the undercutting of cold air from the NW. precipitation would result This plusthe fact that Omeishan is on the tracks of shallow depressions, or even situated in the region where shallow depressions are formed, caused precipitation to be extraordinarily heavy. |
|
HTML 查看全文
查看/发表评论 下载PDF阅读器 |
|
|
|