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Research progress on the impact of climate change on vegetation ecosystem in the Tibetan Plateau
CAO Xiaoyun, ZHOU Bingrong, ZHOU Huakun, QIAO Bin, YAN Yuqian, ZHAO Tong, CHEN Qi, ZHAO Huifang, YU Hongyan
Journal of Arid Meteorology    2022, 40 (6): 1068-1080.   DOI: 10.11755/j.issn.1006-7639(2022)-06-1068
Abstract347)   HTML6)    PDF(pc) (19848KB)(851)       Save

The temperature and precipitation in the Tibetan Plateau (hereinafter referred to as the ‘TP’) increase as a whole, and the vegetation of the plateau has changed significantly under the influence of climate change. This paper summarizes the research progress on plateau climate change and its impact on plateau vegetation coverage and normalized difference vegetation index (NDVI), phenology, net primary productivity (NPP), biomass carbon pool, plant diversity and so on, and the future directions of research are discussed and expected. The main conclusions are as follows: (1) In recent 60 years, the annual average temperature increased significantly with an average increase of 0.37 ℃ per 10 years, and the annual precipitation increased with an average increase of 10.40 mm per 10 years in the TP. The warm and dry trend of climate in the southeast of the TP and the warm and humid trend of climate in the northwest of the TP were obvious. (2) Under the background of overall improvement, the vegetation coverage and NDVI degraded in local regions of the TP. The improved area accounted for 67.7%-75.0% of the plateau total area, and they mainly distributed in the central and eastern regions. (3) Under of the influence of climate change, the green returning period of vegetation in the plateau advanced, the dry and yellow period postponed, and the growth period prolonged on the whole. However, there is a great debate on the green returning period of plateau vegetation in advance after 2000. (4) NPP of plateau vegetation increased significantly as a whole, while the increasing rate of NPP slowed down after 2000. NPP of vegetation increased significantly in southern Qilian Mountains and alpine meadows of northern Nianqing Tanggula Mountains, while it decreased in northern Tibetan Plateau, ‘one river, two rivers’ and the central and western regions of Tibet three river sources. (5) The biomass carbon pool of the plateau vegetation showed an increasing trend, which was carbon sink in general, and the spatial heterogeneity was obvious. The biomass carbon of alpine meadow and steppe increased significantly, while that of other grassland increased slightly, and even decreased in some areas. (6) The plant diversity in the plateau has changed significantly. Although the research results were different, there is no doubt that the climate change has affected significantly on species composition and plant diversity of alpine grassland community. It is suggested to strengthen data networking observation comparison and multi-scale effect research, deepen internal mechanism research and multi-factor comprehensive and quantitative analysis, strengthen sharing mechanism and improve the coping ability to climate change in the future, so as to promote ecological protection and high-quality development of the plateau.

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Causes Analysis of an Extreme Persistent Rainstrom in Hunan Province in July 2016
ZHOU Hui, CAI Ronghui, YING Dongde, ZHOU Li
Journal of Arid Meteorology    DOI: 10.11755/j.issn.1006-7639(2018)-01-0056
Impacts of Different Types ElNio Events on the Next Spring Precipitation in Ningxia
LI Xin,WANG Suyan,ZHENG Guangfen,DING Xiaojin,ZHOU Hu,YANG Jianling
Journal of Arid Meteorology    DOI: 10.11755/j.issn.1006-7639(2016)-02-0290
Temporal and Spatial Distribution of Thunderstorm in Wuwei of Gansu Province
ZHANG Chunsong1, YANG Xiaoling2, LIU Rong1, ZHOU Hua3, HU Jinge2
Journal of Arid Meteorology    DOI: 10.11755/j.issn.1006-7639(2015)-04-0659
Analysis of a Heavy Rainfall Process in Wuwei of Gansu in 2013
ZHAO Dongxu1,YANG Xiaoling1,ZHOU Hua2,LIU Rong3
Journal of Arid Meteorology    2015, 33 (1): 149-155.   DOI: 10.11755/j.issn.1006-7639(2015)-01-0149
Abstract1449)      PDF(pc) (3581KB)(2141)       Save

Based on the conventional weather charts,FY - 2D satellite images,surface meteorological data,physical quantity field and NCEP reanalysis data,a heavy rainfall process which occurred on August 6, 2013 in Wuwei of Gansu Province was systematically diagnosed. The results show that the heavy rainfall was caused by interaction of multiple factors under a certain large - scale circulation background. Dramatic change of surface meteorological factors was an energy release process of strong convection weather. Local high humidity and moisture convergence provided an abundant moisture source. High - level divergence,low - level convergence and strong rising motion were the dynamic conditions. Strong unstable energy and unstable stratification were the necessary conditions of enhancing the convection enhancement and rainfall intensity increase. Development and strengthening of convective cloud clusters resulted in heavy rainfall process.

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Integrated Forecast Index of Severe Convection Weather in the Plain Region of NingxiaBased on Doppler Weather Radar
XU Yang-Chun, LIU Xiao-Jing, ZHOU Hu, CHEN Xiao-Juan, CHEN Yang, NIE Jin-Xin
J4    2010, 28 (2): 212-216.  
Abstract1665)      PDF(pc) (698KB)(1768)       Save

The multi-factor integrated correlation probability method and the multi-parameter dot pitch line method are used to analyze 160 hailstorm cases occurred in the plain region of Ningxia in flood season from 2003 to 2008. The quantitative comprehensive forecast index of severe convection weather in the plain region of Ningxia discriminated by Doppler Radar was found. The result shows that the success rate of identification of hail, heavy rain and other severe convective weather could reach to 87.1% while the comprehensive forecast index reaches 2.8

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