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The spatial-temporal distribution of NPP along NECT and its response to climatic change were also analyzed. Results showed that the change tendency of NPP spatial distribution in NECT is quite similar to that of precipitation and their spatial correlation coefficient is up to 0.84 (P.01). The inter-annual variation of NPP in NECT is mainly affected by the change of the aestival NPP every year, which accounts for 67.6% of the inter-annual increase in NPP and their spatial correlation coefficient is 0.95 (P.01). The NPP in NECT is mainly cumulated between May and September, which accounts for 89.8% of the annual NPP. The NPP in summer accounts for 65.9% of the annual NPP and is the lowest in winter. Recent climate changes have enhanced plant growth in NECT. The mean NPP increased 14.3% from 1980s to 1990s. The inter-annual linear trend of NPP is 4.6 gCm^(-2)a^(-1), and the relative trend is 1.17%, which owns mainly to the increasing temperature.

结果表明:(1)NECT样带植被NPP的空间变化趋势同降水量的空间变化十分相似,由东到西逐渐降低,二者在空间上的相关性达到了0.84 (P.01),说明NECT样带的植被NPP在空间分布上主要受水分趋动:(2)NECT样带植被NPP的年际变化主要是由各年份夏季NPP的变化造成的,夏季对NECT样带植被NPP的年际增长贡献率最大(67.6%),二者之间的相关性达到了0.95 (P.01);(3)NECT样带的植被NPP积累期主要发生在5-9月份,这5个月的NPP占了全年NPP总量的89.8%,整个夏季(6-8月份)的NPP占了全年的65.9%,冬季(12-2月份)的NPP最低,基本为0;(4)近19年来的气候变化促进了NECT样带的植被生长,从1980年代到1990年代,NPP显著增加,年代际相对增长率为14.3%,平均年际绝对增长趋势为4.6 gCm^(-2)a^(-1),相对增长趋势为1.17%,这主要是由温度升高引起的。

Past Global Changes , aiming to predict future climatic and environmental changes quantitatively, is an i...

过去全球变化是国际地圈、生物圈计划中的一个核心计划,其根本目的是为定量地预测未来的气候、环境变化服务。

In addition to changes in one day, we must also take into account the different climatic conditions throughout the year changes in dress the impact of psychological and physical.

除了一天的时间变化外,还应考虑到一年四季不同的气候条件的变化对着装的心理和生理的影响。

Eastern Himalaya Syntaxis is an important area in studying climatic-tectonic reciprocity. In this paper, single-crystal-high-precision laser ~(40)Ar/~(39)Ar method was used to build the thermal evolutional history of Eastern Himalaya Syntaxis by tests on river sediments on the lower reach of Yalung-Tsangpo River. The contrast of age statistical results against the figure showing the changes in rate and angle of convergence during India plate has been colliding against Eurasian plate since late Mesozoic and the diagram consisting of global deep-seaδ18O andδ13C records is done, for the purpose of revealing climatic and tectonic information on rock cooling and referring the relationship between thermal evolutional history and climate and tectonics.

东喜马拉雅构造结是气候与构造相互作用的典型地区,本文尝试使用单颗粒高精度单次全熔~(40)Ar/~(39)Ar法对采自雅鲁藏布江大峡谷下游墨脱县城以南约50 km处地东河段的细粒现代河沙进行年代学测试,建立东喜马拉雅构造结的热史演化序列,并通过与代表全球气候变化的18O、13C浓度变化曲线和印度大陆向北运动的速度、角度变化曲线的对比,揭示气候、构造因素与东喜马拉雅构造结热史演化的耦合,推定热史演化与气候、构造过程的关系。

There will be an obvious important effect of global climatic change in future on cropping systems in China The heat resource will be increased to a certain extent in all regions of China, and the north borderline of two crops per annual or three crops per annual will move northwardly, the cropping range, output and quality of crops will be changed However, there will be a uncertainty of changes of cropping systems due to the adverse impact of moisture changes of climate in the future

未来全球性气候变暖对我国的种植制度将产生明显的影响,预计我国各地的热量资源将有不同程度的增加,使一年二熟、一年三熟的种植北界有所北移,主要农作物的种植范围、产量、质量都会有所变化。但由于水分变化可能产生的不利影响,使种植制度的变化具有较大的不确定性。

Research progresses have been performed during the past decade in the following aspects: ecologicaldatabase development, climate and its variability, ecophysiological response of plants to environments,vegetation and landscape changes, biodiversity patterns and their changes, plant functional types and traitswith relation to climatic gradient, productivity and carbon dynamics, pollen-vegetation relationship, tracegas emissions, land use and land cover changes, as well as biogeographical and biogeochemical modelling.

在过去的10年里,中国东北样带的研究进展表现在以下几个方面:生态数据库发展、气候及其变异性、植物对环境的生态生理响应、植被和景观变化、生物多样性格局及其变化、植物功能型和植物性状及气候梯度分析、生产力和碳动态、花粉-植被相互关系、痕量气体放散、土地利用和土地覆盖变化以及生物地理和生物地球化学模拟。

Diaojiaohaizi is a thoroughly closed basaltic depression lake on the top of Daqing mountains which has many advantages when it is used in studding vegetational evolution and climatic changes of the Holocene.

调角海子为大青山顶部的一个全封闭的玄武岩洼地湖泊,冰后期积水成湖,其湖泊沉积物具有用来研究全新世植被和气候变化的许多独特优点。

It was suggested that the key topics of the study in NE China include the enforcement of the study of the middlelate Late Pleistocene environmental reconstructions, the understanding of the spatialtemporal and abrupt variations of the climatic changes, the establishment of solid independent chronologies for the MammuthusColelodonta fauna and the main species.

提出加强对我国东北地区晚更新世气候环境的重建、认识气候变化的区域特点和突变性,系统而可靠地建立以猛犸象—披毛犀为主的化石动物年代序列、区分主要类型化石动物年代是研究的关键。

The chest is deep with a slightly roached back and a tucked-up belly. The lenght from the brisket to the rump is slightly shorter than the height at the shoulder It maybe white and fawn though all colours are accepted. It needs very little grooming and enjoys the outdoors. Its food requirements are very minimal. It is very hardy and resistent to climatic changes

尾巴的长度等于后退的长度,在胸腔的位置成拱形,背部折起,从胸部到臀部的长度略短于高度肩,It maybe white and fawn though all colours are accepted它需要很少的培养竟可能享受户外活动,它的粮食需求是很小的,非常耐寒,耐气候变化。

Woods response to changes in climatic conditions is predictable regardless of where in the world it is and all piano makers use the same kiln drying method to control woods reaction to the world's climate changes.

木材在不同气候条件下的变化是可预见的,不管它在这个世界的哪个地方都是一样。所有的钢琴制造商使用同样的干燥窑干燥方法让木材适应世界上的不同气候。

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