横断山地区辐射平衡各分量的计算和分布特征
文献类型：期刊论文
| 作者 | 贺素娣 ; 文传甲 |
| 刊名 | 山地研究
 |
| 出版日期 | 1983 |
| 卷号 | 1期号:3页码:32-36 |
| 关键词 | 辐射平衡 横断山地区 太阳总辐射 有效辐射 和分布 分量 地表反射率 平方 年总量 |
| 其他题名 | COMPONENTS OF CALCULATING RADIATION BAIANCE AND THEIR TEMPORAL AND SPACIAL DISTRIBUTION OF HENDUAN MOUNTAINOUS REGION |
| 通讯作者 | 贺素娣 |
| 中文摘要 | 横断山区位于青藏高原东南部,约在东经96°—103°,北纬24°—34°之间,区内山川相间排列,南北纵贯,山高谷深,自然资源十分丰富。 探讨太阳辐射和地表辐射平衡对深入研究本区气候形成,地表能量转换和生态系统结构特性具有重要意义。国内许多研究工作者在对青藏高原和其它地区的辐射平衡的研究中,也有涉及到横断山区辐射平衡的若干分析,但都不甚详细。本文试图利用现有地面气象台站观测资料,考虑到山区的地形特征而选择适当的公式,对横断山地区(共40个台站)的辐射平衡各分量进行了计算,并分析了辐射平衡各分量的时空分布特征。 |
| 英文摘要 | Components of the radiation balance of Henduan Mountainous region are calculated by using reasonable experimental formulae and measurements of 40 meteorolog icel stations Results are as follow 1. Average annual totals of the solar global radiation, the effective radiation and the radiation balance are smaller on the east and west sides of this region than on the middle part. This is analogous to the spacial distribution of January and July. This spacial distribution is also similar to the sunshine hours and is contrary to the rainfall and the total cloud cover on the region.The Hengduan Mountains of S-N trend screened the transportation of E-W vapour, thus changing the preciptation and the cloud cover to be least of this region and the sunshine to be laryest. On the middle part, the annual and July values of the compoments increase gradually from southeast to northwest. This is analogous to the topog-rafical distribution. The salar rediation resources on the middle part are smaller than on Xizang Plateau, and are larger much than on the epuivalent latitudinal region in east China, and here is one of theimost solar rediation resources regiob in China.2 . The month values of the global radiation and the radiation balance for March to May of alternate the dry season and the moist one are largest in the year,but ones for month in summer on the east and west sides; and the ones for December to February on the middle part are least. The effective radiation for November to January is largest, while its ranee is smaller |
| 学科主题 | 生态学 ; 环境学 |
| 分类号 | P422 |
| 收录类别 | CSCD |
| 语种 | 中文 |
| 公开日期 | 2012-11-29 |
| 源URL | [http://192.168.143.20:8080/handle/131551/4314]  |
| 专题 | 成都山地灾害与环境研究所_成都山地所知识仓储（2009年以前） |
| 推荐引用方式 GB/T 7714 | 贺素娣,文传甲. 横断山地区辐射平衡各分量的计算和分布特征[J]. 山地研究,1983,1(3):32-36. |
| APA | 贺素娣,&文传甲.(1983).横断山地区辐射平衡各分量的计算和分布特征.山地研究,1(3),32-36. |
| MLA | 贺素娣,et al."横断山地区辐射平衡各分量的计算和分布特征".山地研究 1.3(1983):32-36. |
入库方式： OAI收割
来源：成都山地灾害与环境研究所
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