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| 1 | The relationship between NDVI and precipitation on the Tibetan Plateau显示文摘西藏的高原上的 NDVI 的时间、空间的变化,以及在 NDVI 和降水之间的关系,在这份报纸被讨论,由使用 8-km 分辨率从 1982 ~ 1999 的多时间的 NOAA AVHRR-NDVI 数据。每月最大的 NDVI 和每月的降雨被用来分析季节的变化,和年度最大值 NDVI,年度有效降水和成长季节降水(从 4 月到 8 月) 被用来讨论 interannual 变化。在 NDVI 和降雨之间的 NDVI 和关联系数的动态变化为每个象素被计算。结果如下:(1 ) NDVI 在种季节到达了山峰(从 7 月到 9 月) 在西藏的高原上。在高原的北、西方的部分,成长季节是很短的(大约二或三个月) ;但是在里面南部,植被几乎所有一年周围成长了。每月最大的 NDVI 和每月的降雨的关联在不同区域变化了。它在西方、北、南部的部分是弱的,但是在中央、东方的部分强壮。(2 ) NDVI interannual 的空间分发动态变化也是不同的。增加区域主要在南部的西藏山区的灌木大草原地区,西方的四川东方的西藏山区的具球果的森林地区的西方的部分, Kunlun 山区的荒芜的地区的北斜坡的西方的部分和 Himalaya 的南部的斜坡的东南的部分被散布山区常绿树阔叶的森林地区;减少区域主要在 Qaidam 山区的荒芜的地区,东方 Qinghai-Qilian 山区的大草原地区的西方、北的部分,南部的 Qinghai 高冷的草地大草原地区和 Ngari 被散布山区的荒芜大草原、荒芜的地区。在年度有效降雨和年度最大的 NDVI 之间的关联系数的空间分发类似于成长季节降雨和年度最大的 NDVI ,并且与中等植被盖子在草地和草地在 NDVI 和降雨之间有好关系,并且植被上的降雨的效果在森林和荒芜的区域里是小的。 | DING Mingjun ZHANG Yili LIU Linshan ZHANG Wei WANG Zhaofeng BAI Wanqi | 2007 | Journal of Geographical Sciences2007，17，3： | 45 |
| 2 | Spatiotemporal variation in alpine grassland phenology in the Qinghai-Tibetan Plateau from 1999 to 2009显示文摘Plant phenology is the most salient and sensitive indicator of terrestrial ecosystem response to climate change.Studying its change is significantly important in understanding and predicting impressively changes in terrestrial ecosystem.Based on NDVI from SPOT VGT,this paper analyzed the spatiotemporal changes in alpine grassland phenology in Qinghai-Tibetan Plateau from 1999 to 2009.The results are enumerated as follows:(1) The spatial distribution of the average alpine grassland phenology from 1999 to 2009 is closely related to water and heat conditions.Accompanying the deterioration in heat and water conditions from southeast to northwest,the start of growth season(SOG) was delayed gradually,the end of growth season(EOG) advanced slowly,and the length of growth season(LOG) shortened gradually.Elevation played an important role in the regional differentiation of phenology,but a dividing line of approximately 3500 m existed.Below this line,the phenology fluctuated irregularly with altitude change,whereas above the line,the phenology is closely related to altitude change.(2) From 1999 to 2009,SOG of the alpine grassland came earlier by six days per decade(R2=0.281,P=0.093),EOG was late by two days per decade(R2=0.031,P=0.605),and LOG lengthened by eight days per decade(R2=0.479,P=0.018).The early SOG,the late EOG,and the extended LOG mainly occurred at the center and east of the Plateau.SOG in most of the Plateau advanced significantly,especially in the eastern Plateau.(3) The inter-annual phenology changes of the alpine grassland in the Qinghai-Tibetan Plateau exhibited significant differentiation at different elevation and natural zones.The inter-annual changes at high altitude were more complicated than that at low altitude.The most significant phenology changes were found in the eastern Qinghai-Qilian montane steppe zone,and non-significant changes occurred in the Southern Tibet montane shrub-steppe zone. | DING MingJun ZHANG YiLi SUN XiaoMin LIU LinShan WANG ZhaoFeng BAI WanQi | 2013 | Chinese Science Bulletin2013，58，3： | 44 |
| 3 | Spatial and temporal variability in the net primary production of alpine grassland on the Tibetan Plateau since 1982显示文摘基于 GIMMS AVHRR NDVI 数据( 8 km 空间分辨率)为 19822000 , SPOT 植被 NDVI 数据( 1 km 空间分辨率)为 19982009 ,并且观察植物生物资源数据, CASA 模型习惯于在高山的草地的变化在西藏的高原( TP )上让主要生产( NPP )赚的模型。这研究将帮助评估高山的草地生态系统的健康条件,并且对高原牧场并且到 TP 上的国家生态的安全躲蔽处的函数的理解的持续开发的提升很重要。NPP 变化的时间空间的特征用空间统计分析被调查,独立根据 physico 地理的因素(自然地区,高度,纬度和经度) ,河盆,和县级的行政区域。处理的数据用一个 ENVI 4.8 平台被执行,当一个 ArcGIS 9.3 和 ANUSPLIN 平台被用来进行空间分析并且印射时。主要结果如下:(1 ) TP 上的高山的草地的 NPP 逐渐地从东南减少到西北,它在降水和温度对应于坡度。从 1982 ~ 2009,在 TP 高山的草地的平均年度全部的 NPP 是 177.2 ?? ?? ? | ZHANG Yili QI Wei ZHOU Caiping DING Mingjun LIU Linshan GAO Jungang BAI Wanqi WANG Zhaofeng ZHENG Du | 2014 | Journal of Geographical Sciences2014，24，2： | 47 |
| 4 | Sensitivity of surface air temperature change to land use/cover types in China显示文摘Using CRU high resolution grid observational temperature and ERA40 reanalysis surface air temperature data during 1960-1999, we investigated the sensitivity of surface air temperature change to land use/cover types in China by subtracting the reanalysis from the observed surface air temperature (observation minus reanalysis, OMR). The results show that there is a stable and systemic impact of land use/cover types on surface air temperature. The surface warming of each land use/cover type reacted differently to global warming. The OMR trends of unused land (≥0.17℃/decade), mainly comprised by sandy land, Gobi and bare rock gravel land, are obviously larger than those of the other land use/cover types. The OMR over grassland, farmland and construction land shows a moderate decadal warming about 0.12℃ /decade, 0.10℃/decade, 0.12 ℃ /decade, respectively. Woodland areas do not show a significant warming trend (0.06 ℃ /decade). The overall assessment indicates that the surface warming is larger for areas that are barren and anthropogenically developed. The better the vegetation cover, the smaller the OMR warming trend. Responses of surface air temperature to land use/cover types with similar physical and chemical properties and biological processes have no significant difference. The surface air temperature would not react significantly until the intensity of land cover changes reach a certain degree. Within the same land use/cover type, areas in eastern China with intensive human activities exhibit larger warming trend. The results provide observational evidence for modeling research on the impact of land use/cover change on regional climate. Thus, projecting further surface climate of China in regional scale should not only take greenhouse gas increase into account, but also consider the impact of land use/cover types and land cover change. | YANG XuChao ZHANG YiLi LIU LinShan ZHANG Wei DING MingJun WANG ZhaoFeng | 2009 | Science China Earth Sciences2009，52，8： | 21 |
| 5 | Start of vegetation growing season on the Tibetan Plateau inferred from multiple methods based on GIMMS and SPOT NDVI data显示文摘在这研究,我们使用了四个方法从 1982~2012 在西藏的高原( TP )上调查成长季节( SGS )的开始,用从全球库存为研究建模并且印射获得的规范的差别植被索引( NDVI )数据( GIMSS , 19822006 )并且点植被( SPOT-VGT , 19992012 )。用四个方法估计的 SGS 价值沿着纬度或高度的坡度显示出类似的空间模式,但是与在 SGS 日期的重要变化。最大的差异主要在这些区域被发现与最高或最低植被范围。在 1982 和 1998 之间,然而,从四个方法导出的 SGS 值都根据更最近的点 VGT 数据(19992012 ) 显示一个进展趋势,没有 TP 上的 SGS 的连续地进展的趋势。在价值从在 1999 和 2006 之间的 GIMMS 和点导出的 SGS 之间的关联的分析数据来源与问候在趋势表明一致性到并且到使用的四个分析方法。与另外的方法相比,最大的一致性在之间在里面 situ 数据和检索的 SGS 值与方法 3 被获得(NDVI 比率的阀值) 。避免错误在有多样的植被类型和物理环境的一个广阔区域,知道不同植被类型的季节的变化特征是批评的,特别地在有稀少的草地的区域或常绿树森林。 | DING Mingjun LI Lanhui ZHANG Yili SUN Xiaomin LIU Linshan GAO Jungang WANG Zhaofeng LI Yingnian | 2015 | Journal of Geographical Sciences2015，25，2： | 17 |
| 6 | Climate change in Mt. Qomolangma region since 1971显示文摘Using monthly average, maximum, minimum air temperature and monthly precipitation data from 5 weather stations in Mt. Qomolangma region in China from 1971 to 2004, climatic linear trend, moving average, low-pass filter and accumulated variance analysis methods, the spatial and temporal patterns of the climatic change in this region were analyzed. The main findings can be summarized as follows: (1) There is obvious ascending tendency for the interannual change of air temperature in Mt. Qomolangma region and the ascending tendency of Tingri, the highest station, is the most significant. The rate of increasing air temperature is 0.234 oC/decade in Mt. Qomolangma region, 0.302 oC/decade in Tingri. The air temperature increases more strongly in non-growing season. (2) Compared with China and the global average, the warming of Mt. Qomolangma region occurred early. The linear rates of temperature increase in Mt. Qomolangma region exceed those for China and the global average in the same period. This is attributed to the sensitivity of mountainous regions to climate change. (3) The southern and northern parts of Mt. Qomolangma region are quite different in precipitation changes. Stations in the northern part show increasing trends but are not statistically significant. Nyalam in the southern part shows a decreasing trend and the sudden decreasing of precipitation occurred in the early 1990s. (4) Compared with the previous studies, we find that the warming of Mt. Qomolangma high-elevation region is most significant in China in the same period. The highest automatic meteorological comprehensive observation station in the world set up at the base camp of Mt. Qomolangma with a height of 5032 m a.s.l will play an important role in monitoring the global climate change. | YANG Xuchao ZHANG Yili ZHANG Wei YAN Yuping WANG Zhaofeng DING Mingjun CHU Duo | 2006 | Journal of Geographical Sciences2006，16，3： | 12 |
| 7 | Vegetation change in the Mt. Qomolangma Nature Reserve from 1981 to 2001显示文摘Based on the NOAA AVHRR-NDVI data from 1981 to 2001, the digitalized China Vegetation Map (1:1,000,000), DEM, temperature and precipitation data, and field investiga- tion, the spatial patterns and vertical characteristics of natural vegetation changes and their influencing factors in the Mt. Qomolangma Nature Reserve have been studied. The results show that: (1) There is remarkable spatial difference of natural vegetation changes in the Mt. Qomolangma Nature Reserve and stability is the most common status. There are 5.04% of the whole area being seriously degraded, 13.19% slightly degraded, 26.39% slightly im- proved, 0.97% significantly improved and 54.41% keeping stable. The seriously and slightly degraded areas, which mostly lie in the south of the reserve, are along the national bounda- ries. The areas of improved vegetation lie in the north of the reserve and the south side of the Yarlung Zangbo River. The stable areas lie between the improved and degraded areas. Degradation decreases with elevation. (2) Degeneration in the Mt. Qomolangma Nature Re- serve mostly affects shrubs, needle-leaved forests and mixed forests. (3) The temperature change affects the natural vegetation changes spatially while the integration of temperature changes, slopes and aspects affects the natural vegetation change along the altitude gradi- ents. (4) It is the overuse of resources that leads to the vegetation degeneration in some parts of the Mt. Qomolangma Nature Reserve. | ZHANG Wei ZHANG Yili WANG Zhaofeng DING Mingjun YANG Xuchao LIN Xuedong LIU Linshan | 2007 | Journal of Geographical Sciences2007，17，2： | 7 |
| 8 | Major Elements in Soils Along a 2.8-km Altitudinal Gradient on the Tibetan Plateau,China显示文摘There are a series of special mountain soils on the Tibetan Plateau of China in an alpine environment for the high altitude.However,very few studies have focused on major soil elements in relation to soil formation in this area.Aluminum(Al),iron(Fe),calcium(Ca),sodium(Na),potassium(K) and magnesium(Mg) contents of 237 topsoil samples covering a 2.8-km altitudinal gradient in uncultivated areas along the Qinghai-Tibet Railway of China were measured using inductively coupled plasma atomic emission spectroscopy.The spatial distribution of the elements and its relationship to the parent rocks and climatic parameters were analyzed.Soils along the gradient are derived from a range of parent materials,but most are less than 30 cm deep with little development(Cambisols).Soil Al,Fe and Mg contents showed a decreasing trend from the start station(Xining Station) to end station(Lhasa Station) of the Qinghai-Tibet Railway,whereas soil K and Na contents were relative stable from Xining Station to the Kunlun Mountains and then increased gradually.Soil Ca content was lower in the southern part of the Tanggula Mountains.The major soil element contents clearly re?ected the parent rock and climatic in?uences.Soils with higher Ca content appeared in areas with Ca-Mg carbonate rocks,soils with higher Al were found in areas with silicate-rich and high-Al silicate clastic rocks and silicate-rich aluminosilicate loose sediments.Soils with higher K and Na contents appeared in areas with high-K,high-Na and silicate-rich aluminosilicate rocks.Soil Na and K contents were affected by temperature,whereas the contents of Mg,Fe,Ca and Al were more affected by precipitation.Soil Na and K contents increased with increasing temperatures,whereas the contents of Mg,Fe,Ca and Al decreased with increasing precipitation.This analysis provides a relationship between soil properties and rapidly changing environmental conditions.The data can be used to investigate the effect of the climate or land use change on soil properties. | WANG Zhaofeng Alfred E.HARTEMINK ZHANG Yili ZHANG Hua DING Mingjun | 2016 | Pedosphere2016，26，6： | 2 |
| 9 | Integration Path of Coastal Leisure Tourism Resources in Rizhao Based on Regional Economic Theory显示文摘Aiming at the rapid development of leisure tourism in coastal cities,the regional economic theory was first analyzed based on existing studies,the integration path of coastal leisure tourism resources in Rizhao was explored using the theory of unbalanced growth of regional economy and the theory of industrial agglomeration,and four countermeasures were proposed for the development of coastal leisure tourism in Rizhao City. | QIN Zhiyu HU Xiuli DING Mingjun | 2018 | Journal of Landscape Research2018，10，3： | 1 |
| 10 | An improved reverse genetics system for Newcastle disease virus genotype Ⅶ显示文摘Dear Editor,Newcastle disease virus(NDV),also known as avian paramyxovirus serotype 1(APMV-1),is a member of the genus Avulavirus within the family Paramyxoviridae,order Mononegavirales(Miller et al.,2010).Although all isolated NDV strains belong to a single serotype,epidemiological studies have revealed that the genotype | Yuzhang Sun Mingjun Sun Yonglian Dai Renfu Yin Zhuang Ding | 2016 | Virologica Sinica2016，31，6： | 1 |
| 11 | Evaluation of Young's Modulus and Residual Stress of NiFe Film by Microbridge Testing显示文摘测试的 Microbridge 被用来测量幼仔的模量和金属性的电影的剩余应力。独立 NiFe 的样品拍摄微桥牌被制作 bymicroelectromechanical 系统。特殊的陶器的柄结构被设计解决得到 NiFe 的负担偏转曲线的问题与正常 Berkovich 探查由 Nanoindenter XP 系统拍摄微桥牌。微桥的负担偏转曲线的理论分析被建议同时评估幼仔的模量和这些电影的剩余应力。当幼仔 Nano 坚硬方法测量的模量是为有硅底层的厚 NiFe 电影的 209.6 +-11.8 GPa 时, Thecalculated 基于分别地,平均幼仔为 electroplated NiFe 电影的模量和剩余压力是 203.2 GPa 和 333.0 MPa 的试验性的大小表演结果。 | Zhimin ZHOU Yong ZHOU Mingjun WANG Chunsheng YANG Ji'an CHEN Wen DING Xiaoyu GAO Taihua ZHANG | 2006 | Journal of Materials Science & Technology2006，22，3： | 1 |
| 12 | Edge Ohmic Heating Experiment on HT-6M Tokamak显示文摘An improved ohmic confinement has been achieved on HT-6M tokamak after application of edge ohmic heating pulse which makes plasma current rapidly ramp up(0.4 ms)in a ramp rate of 12 MA/s.The improved ohmic confinement phase is characterized by(a)energy and particle confinement time increase,(b)non-symmetric increased density ne,(c)reduced Hαradiation,(d)increased Te and steeper Te,ne profile at the edge.The results from soft x-ray sawteeth inversion radius andβ_(p)+l_(i)/2 implied the anomalous current penetration. | GAO Xiang FAN Shuping LI Jian’gang MENG Yuedong LUO Jiarong YIN Fhxian ZENG Lei DING LianchengLIN Bili ZHANG Wei HAN Yuqing TONG Xingde LUO Lanchang GONG Xianzu JIANG Jiaguang WU Mingjun YIN Fei | 1994 | Chinese Physics Letters1994，11，3： | 0 |
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