东亚季风环流由夏向冬的季节转变与中国前冬气候的关系

利用NCEP/NCAR再分析资料、CMAP降水及Hadley环流中心海温资料等,对东亚季风环流由夏向冬的季节转变与中国前冬气候的关系进行了研究。参考前人定义的亚太热力差指数,计算了1979-2016年亚太热力场由夏向冬的季节转变时间(平均为56. 6候)。结果表明,该季节转变时间点能很好地表征东亚季风环流由夏向冬的季节转变。东亚季风环流由夏向冬的转变特征表现为:低层大陆热低压转为大陆冷高压,阿留申低压形成加强,低空偏南风转为偏北风;中层东亚大槽形成,副高单体减弱成一个副热带高压带;高层南亚高压中心从青藏高原移至菲律宾以东洋面上,高空偏北风转为偏南风。此外由夏向冬的季节转变时间与中国前冬降水和地面气温有着紧密的联系,并且该转变时间的早晚与前期夏季热带太平洋的海温呈现类ENSO异常海温型的相关分布,即表现为前期夏季热带中东太平洋海温偏低(高)时,后期东亚夏季型季风环流向冬季型季风环流转变易偏晚(早),这对东亚季风环流季节转变的预测提供了依据。     

Dominant SST Mode in the Southern Hemisphere Extratropics and Its Influence on Atmospheric Circulation

The variability in the Southern Ocean(SO) sea surface temperature(SST) has drawn increased attention due to its unique physical features; therefore, the temporal characteristics of the SO SST anomalies(SSTA) and their influence on extratropical atmospheric circulation are addressed in this study. Results from empirical orthogonal function analysis show that the principal mode of the SO SSTA exhibits a dipole-like structure, suggesting a negative correlation between the SSTA in the middle and high latitudes, which is referred to as the SO Dipole(SOD) in this study. The SOD features strong zonal symmetry, and could reflect more than 50% of total zonal-mean SSTA variability. We find that stronger(weaker) Subantarctic and Antarctic polar fronts are related to the positive(negative) phases of the SOD index, as well as the primary variability of the large-scale SO SSTA meridional gradient. During December–January–February, the Ferrel cell and the polar jet shift toward the Antarctic due to changes in the SSTA that could be associated with a positive phase of the SOD, and are also accompanied by a poleward shift of the subtropical jet. During June–July–August, in association with a positive SOD, the Ferrel cell and the polar jet are strengthened, accompanied by a strengthened subtropical jet. These seasonal differences are linked to the differences in the configuration of the polar jet and the subtropical jet in the Southern Hemisphere.     

台风“卢碧”变性增强过程的诊断研究

利用日本气象厅JRA再分析资料和台风最佳路径资料以及TRMM降水资料,对0920号台风"卢碧"变性过程的环流形势、高低层热力异常和锋生锋消等特征进行了分析研究。结果表明,"卢碧"的变性是中高纬度冷空气入侵的结果,变性过程伴随着西风槽的东移,高空急流的加强以及西太平洋副热带高压的减弱东撤。低纬度暖湿气流及较大的正涡度异常气旋式卷入台风环流,并在其东北侧积聚产生大量降水,释放的凝结潜热有利于北侧脊的加强,使得高空急流进一步加强,使得台风中心气压进一步降低。锋生、强降水伴随的潜热释放以及气旋中心气压之间存在着正反馈效应是"卢碧"变性后得以增强再发展的主要原因。热成风涡度梯度的分布对"卢碧"的变性增强过程具有较好的指示意义。     

Spatial Differentiation Characteristics and Driving Forces of Forest Transition: A Case Study of Zunyi City,Guizhou

Spatial differentiation in forest transition was measured in terms of space transition and function transition using the exploratory spatial data analysis method (ESDA) and data from 2004—2014 for Zunyi city, Guizhou province, China. The validity of factors affecting forest transition was analyzed by constructing radial basis function neural networks (RBFNN) based on the data processing system (DPS). Our results will provide references for scientific understanding of the potential mechanism underlying forest transition in mountainous areas. We found that Global Moran’s I of space transition and function transition of forest land was 0.0336 and 0.2323, respectively. This suggests a significant positive correlation in spatial distribution of space transition and function transition of forest land, and significant spatial aggregation. The Global Moran’s I of function transition was higher than that of space transition, and the spatial aggregation characteristics of function transition were more significant than for space transition. The Global Moran’s I at each time period tended to increase, and the spatial aggregation degree of the function transition and space transition was further enhanced. Hot and cold spots of space transition of forest land stably evolved, suggesting a minor spatial difference in forest land among different administrative units at the county level. The number of hot spots at the county level in function transition increased. Hot spots were intensively distributed at the western edge and continuously distributed in the northeast. The space transition and function transition of forest land were both greatly influenced by urbanization rate and second and third industries. The development of urbanization and industrialization was the main factor driving forest transition, suggesting a positive role of economic growth on forest transition in mountainous areas. The development of urbanization and industrialization is an effective approach to forest transition in mountainous areas.     

Farmland function evolution in the Huang-Huai-Hai Plain: Processes,patterns and mechanisms

Using counties as the basic analysis unit, this study established an evaluation index system for farmland function (FF) from economic, social, and ecological perspectives. The method combining entropy weighting and multiple correlation coefficient weighting was adopted to determine the weights, and the FF indices were calculated for each county. Subsequently, the spatio-temporal characteristics of farmland function evolution (FFE) were analyzed and the coupled relationships between the sub-functions were explored based on a coupling coordination model. At the same time, the dynamic mechanism of FFE was quantitatively analyzed using a spatial econometric regression analysis method. The following major conclusions were drawn: (1) The farmland economic function generally exhibited a declining trend during 1990–2010, and it is essential to point out that it was stronger in underdeveloped and agriculture-dominated counties, while it continuously weakened in developed areas. Farmland social function decreased in 60.29% of the counties, whereas some counties, which were mostly located in north of Zhengzhou and west of Dezhou and Cangzhou, Yantai, and Weihai, clearly increased. A dramatic decline in farmland ecological function occurred around Beijing, Tianjin, and Jinan. Areas located in the northern part of Henan Province and the central part of Shandong Province saw an increase in ecological function. (2) There was a significant spatial difference in the coupling degree and coordination degree of the sub-functions, and the decoupling phenomenon highlighted this. The changes in social function and ecological function lagged behind economic function in developed areas, but these were highly coupled in some underdeveloped areas. (3) FFE in the Huang-Huai-Hai Plain (HHHP) is resulted from the comprehensive effects of regional basic conditions and external driving factors. Furthermore, the transitions of population and industry under urbanization and industrialization played a decisive role in the evolution intensity and direction of farmland sub-systems, including the economy, society, and the ecology. According to the results mentioned above, promoting the transformation from traditional agriculture to modern agriculture should be regarded as an important engine driving sustainable development in the HHHP. Taking different regional characteristics of FFE into account, differentiated and diversified farmland use and management plans should be implemented from more developed urban areas to underdeveloped traditional agricultural areas.     

中国工业基地的甄别与演化模式

中国工业化的快速进程在空间上表现为一系列工业基地的形成和演化。本文采用1985年、2001年和2010年数据,对中国工业基地进行识别、筛选和类型划分,并分析其空间格局演进过程与特征,探讨不同规模与不同类型工业基地成长的路径,总结其形成与演化的一般模式。研究发现：1949年以来中国工业基地在空间上整体经历了1978年改革开放前分散化发展、改革开放初期逐步向东部沿海地区集聚、21世纪均衡多元化发展3个阶段。至2010年,中国共有251个工业基地,奠定了其工业化的空间总图。随着工业基地产业规模扩大,其产业结构先由单一化向多元化发展,再由多元化向优势产业组合调整;多数工业基地的主导产业沿着轻工业、基础原材料工业和先进制造业的轨迹不断演进,其发展与演化的关键因素由自然资源、劳动力等传统生产要素向资本、信息等新因素过渡,但大、中、小型工业基地成长的路径和影响因素具有显著差异。小型工业基地主要依靠自然资源保持单行业主导的发展路径;中型工业基地产业组合逐步综合化;大型工业基地向基础原材料工业和设备制造业组合发展的方向演进。     

中国14个连片特困地区的森林转型及其解释

利用MODIS土地覆盖数据,分析了2002-2013年中国14个连片特困地区森林转型的特点,探明了连片特困地区林地变化的趋势及其空间异质性。在此基础上,选择空间变量,建立线性回归模型探究林地面积变化的影响因素,得出连片特困地区森林转型所遵循的路径。结果表明,2002-2013年间,中国14个连片特困地区林地面积净增加106554.75 km²,增长率为11.93%,森林进入转型后期,即森林面积净增加阶段;秦巴山区、武陵山区、西藏地区东南部、四省藏区东部、燕山—太行山区东部是林地增长的热点区域,而林地增长冷点区域则主要分布在800 mm等降水量线以北的广大区域、大别山区和滇桂黔石漠化区东部;非农人口的增加以及林业工程的实施都对林地面积的增加有显著的促进作用,中国14个连片特困地区的森林转型主要遵循着经济发展路径和国家森林政策路径。在连片特困地区,应加快小城镇建设的步伐,同时依托其丰富的自然资源,因地制宜地发展乡村生态旅游业;国家森林政策方面,应将连片特困地区作为生态建设重点区域,切实保护中国的森林资源。     

Role of the oceanic channel in the relationships between the basin/dipole mode of SST anomalies in the tropical Indian Ocean and ENSO transition

The relationships between the tropical Indian Ocean basin(IOB)/dipole(IOD) mode of SST anomalies(SSTAs) and ENSO phase transition during the following year are examined and compared in observations for the period 1958–2008.Both partial correlation analysis and composite analysis show that both the positive(negative) phase of the IOB and IOD(independent of each other) in the tropical Indian Ocean are possible contributors to the El Nio(La Nia) decay and phase transition to La Nia(El Nio) about one year later. However, the influence on ENSO transition induced by the IOB is stronger than that by the IOD. The SSTAs in the equatorial central-eastern Pacific in the coming year originate from subsurface temperature anomalies in the equatorial eastern Indian and western Pacific Ocean, induced by the IOB and IOD through eastward and upward propagation to meet the surface. During this process, however the contribution of the oceanic channel process between the tropical Indian and Pacific oceans is totally different for the IOB and IOD. For the IOD, the influence of the Indonesian Throughflow transport anomalies could propagate to the eastern Pacific to induce the ENSO transition. For the IOB, the impact of the oceanic channel stays and disappears in the western Pacific without propagation to the eastern Pacific.     

台湾海峡游泳动物群落的空间结构及其季节变化

The Taiwan Strait is a transition zone between the East China Sea and the South China Sea with unique hydrology and a geographical environment that creates special marine community features.To analyze the spatial structure and seasonal changes of the nekton assemblages in the Taiwan Strait,seasonal experimental trawl surveys were conducted during 2006–2007.The results showed that there were two assemblages in the area with different sets of species,and the average similarity within each group varies between 39.38% and 74.20%.By using multivariate statistical analysis and analyzing the distribution of dominant species,we found that the structures of the assemblages had obvious seasonal variation.The middle region from the Putian transect to the Xiamen transect could be considered a mixing area for the two assemblages.The analysis of the relationship between species assemblages and environmental factors indicated that temperature was the most important factor affecting the community structure in cold seasons,and 22.5°C and 17°C could be considered dividing lines for spring and winter,respectively.In warm seasons,the most important factor was water depth,but the relationship with depth was not as significant,with a correlation between 0.264 and 0.399.The seasonal changes of nekton assemblages basically reflected the dynamic currents in the Taiwan Strait.The south coastal assemblage extended to nearly the entire area of the Taiwan Strait along with a strong and intense warm current that shrinks in spring and winter when the southward intrusion of the cold Zhejiang-Fujian coastal current becomes stronger.The impact of shortterm and long-term environmental changes,such as extreme weather,global warming and human activity on nekton assemblages,had been recognized but need further research.Our study on nekton assemblages could be used as a baseline for measuring future changes.     

多年冻土区路桥过渡段一种新结构的试验观测与分析

基于保护多年冻土的原则,通过对一般地区过渡段设置方法的改进,得到了一种用于青藏铁路清水河地区的新型式路桥过渡段的设置方法.通过对过渡段的沉降和热状况的现场监测,分析了过渡段沉降变形和热状况的变化规律,并对采用的设置方法所产生的实际效果进行了评价.