Temperature trends and elevation dependent warming during 1965-2014 in headwaters of Yangtze River, Qinghai Tibetan Plateau
文献类型:期刊论文
| 作者 | Ahmed Naveed3,4; Wang Gen-xu3 ; Oluwafemi Adeyeri5; Munir Sarfraz6; Hu Zhao-yong3,4; Shakoor Aamir1; Imran Muhammad Ali2
|
| 刊名 | JOURNAL OF MOUNTAIN SCIENCE
![]() |
| 出版日期 | 2020 |
| 卷号 | 17期号:3页码:556-571 |
| 关键词 | Climate change Elevation dependent warming Mann Kendall Temperature trends Yangtze River Qinghai Tibetan Plateau |
| ISSN号 | 1672-6316 |
| DOI | 10.1007/s11629-019-5438-3 |
| 产权排序 | 1 |
| 文献子类 | Article |
| 英文摘要 | The understanding of temperature trends in high elevation mountain areas is an integral part of climate change research and it is critical for assessing the impacts of climate change on water resources including glacier melt, degradation of soils, and active layer thickness. In this study, climate changes were analyzed based on trends in air temperature variables (T-max, T-min, T-mean), and Diurnal Temperature Range (DTR) as well as elevation-dependent warming at annual and seasonal scales in the Headwaters of Yangtze River (HWYZ), Qinghai Tibetan Plateau. The Base Period (1965-2014) was split into two subperiods; Period-I (1965-1989) and Period-II (1990- 2014) and the analysis was constrained over two subbasins; Zhimenda and Tuotuohe. Increasing trends were found in absolute changes in temperature variables during Period-II as compared to Period-I. T-max, T-min, and T-mean had significant increasing trends for both sub-basins. The highest significant trends in annual time scale were observed in T-min (1.15 degrees C decade(-1)) in Tuotuohe and 0.98 degrees C decade(-1) in Zhimenda sub-basins. In Period-II, only the winter season had the highest magnitudes of T-max and T-min 0.58 degrees C decade(-1) and 1.26 degrees C decade(-1) in Tuotuohe subbasin, respectively. Elevation dependent warming analysis revealed that T-max, T-min and T-mean trend magnitudes increase with the increase of elevations in the middle reaches (4000 m to 4400 m) of the HWYZ during Period-II annually. The increasing trend magnitude during Period-II, for T-max, is 1.77, 0.92, and 1.31 degrees C decade(-1), for T-min 1.20, 1.32 and 1.59 degrees C decade(-1), for T-mean 1.51, 1.10 and 1.51 degrees C decade(-1) at elevations of 4066 m, 4175 m and 4415 m respectively in the winter season. T-mean increases during the spring season for > 3681 m elevations during Period-II, with no particular relation with elevation dependency for other variables. During the summer season in Period- II, T-max, T-min, T-mean increases with the increase of elevations (3681 m to 4415 m) in the middle reaches of HWYZ. Elevation dependent warming (EDW), the study concluded that magnitudes of T-min are increasing significantly after the 1990s as compared to T-max in the HWYZ. It is concluded that the climate of the HWYZ is getting warmer in both sub-basins and the rate of warming was more evident after the 1990s. The outcomes of the study provide an essential insight into climate change in the region and would be a primary index to select and design research scenarios to explore the impacts of climate change on water resources. |
| 电子版国际标准刊号 | 1993-0321 |
| 语种 | 英语 |
| WOS记录号 | WOS:000519163500005 |
| 源URL | [http://ir.imde.ac.cn/handle/131551/34635] ![]() |
| 专题 | 成都山地灾害与环境研究所_山地表生过程与生态调控重点实验室 |
| 通讯作者 | Wang Gen-xu |
| 作者单位 | 1.Bahauddin Zakariya Univ, Dept Agr Engn, Multan 66000, Pakistan; 2.China Univ Geosci, Beijing Key Lab Water Resources & Environm Engn, Beijing 100083, Peoples R China 3.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Surface Proc & Ecol Regulat, Chengdu 610041, Peoples R China; 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China; 5.Karlsruhe Inst Technol, Inst Meteorol & Climate Res Atmospher Environm Re, Campus Alpine, D-82467 Garmisch Partenkirchen, Germany; 6.Univ Kurdistan Hewler, Water Resources Engn, 30 Meter Ave, Erbil 44001, Kurdistan, Iraq; |
| 推荐引用方式 GB/T 7714 | Ahmed Naveed,Wang Gen-xu,Oluwafemi Adeyeri,et al. Temperature trends and elevation dependent warming during 1965-2014 in headwaters of Yangtze River, Qinghai Tibetan Plateau[J]. JOURNAL OF MOUNTAIN SCIENCE,2020,17(3):556-571. |
| APA | Ahmed Naveed.,Wang Gen-xu.,Oluwafemi Adeyeri.,Munir Sarfraz.,Hu Zhao-yong.,...&Imran Muhammad Ali.(2020).Temperature trends and elevation dependent warming during 1965-2014 in headwaters of Yangtze River, Qinghai Tibetan Plateau.JOURNAL OF MOUNTAIN SCIENCE,17(3),556-571. |
| MLA | Ahmed Naveed,et al."Temperature trends and elevation dependent warming during 1965-2014 in headwaters of Yangtze River, Qinghai Tibetan Plateau".JOURNAL OF MOUNTAIN SCIENCE 17.3(2020):556-571. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
浏览0
下载0
收藏0
其他版本
除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。


