The terrestrial NPP simulations in China since Last Glacial Maximum

Based on Atmosphere-Vegetation Interaction Model （AVIM）, the magnitude and spatial distribution of terrestrial net primary productivity （NPP） in China is simulated during three different geological eras, Last Glacial Maximum （LGM）, Mid-Holocene （MH） and the present. The simulation shows that the glacial-interglacial variation of East Asian summer monsoon in China is the key factor affectfng the NPP change. During the three eras, mean NPPs are 208 g/m^2·a, 409 g/m^2·a, and 355 g/m^2·a. The total NPPs are 2.05 Pg/a, 3.89 Pg/a and 3.33 Pg/a, respectively. The terrestrial NPP in China during warm-humid climate is larger than that during cold-arid eras, and the correlation analysis between NPP and climate factors suggests that temperature is the primary factor affecting the terrestrial NPP during 21 kaBP （LGM）, and for 6 kaBP （MH） and the present the primary factor is precipitation.     

Pollen records and time scale for the RM core of the Zoige Basin, northeastern QinghaiTibetan Plateau

A continuous pollen record from the Zoige Basin in the northeastern Qinghai-Tibetan Plateau not only provides information on the vegetation and climate changes during the last two glacial/interglacial cycles, hut also gives proof to establish the time scale of the upper 60 m of the RM core. Subalpine spruce-fir forests colonized the Zoige Basin during the interglacials and interstadials, implying warm and wet climate conditions. Alpine periglacial desert or dry desert may have existed during the penultimate glacial and the last glacial maxima, respectively. Alpine sedge meadow dominated the landscape during MIS 4. The MIS 3 is punctuated by a number of stadials similar to those documented in the Guliya and GISP2 ice cores, as indicated by repeated rise and fall of subalpine spruce-fir forests. Our pollen record reveals a regional climate history similar to those from the neighboring sites, including the Arabian Sea and the Guliya ice core, and thus supports the notion that the Qinghai-Tibetan Plateau acts as an important link between climatic events in the North Atlantic realm and the Asian monsoon domain.     

High resolution stalagmite δ18O records over the past 1000 years from Dongge Cave in Guizhou

Based on MC-ICP-MS U-series dating andstable O-isotope analysis results, a 4-5 years resolution monsoon record over the past 1000 years has been established for two stalagmites from Dongge Cave, Guizhou. The high resolution oxygen isotope record serves as a proxy for variations in rainfall of Asian southwest monsoon over the Yunnan-Guizhou Plateau. A close relation of the δ18O record with the A^14C record from tree rings largely reflects impact of centennial-scale solar activity on the monsoon climate changes. The conspicuous decrease in the δ18O value at AD 1720 indicates an abrupt increase in monsoon rainfall, suggesting that an atmospheric-oceanic couple over the tropical Indian Ocean plays an important role in rapid increase of the Northern Hemisphere temperature over the last century.     

利用现代物流促进农业发展

文章就我国农业发展中出现的一些问题 ,提出了运用现代物流来减缓和解决农业发展中的问题。详述了我国农产品物流的特点及现状 ,并从物流角度就如何解决农业发展中的问题提出了几种方法     

随书光盘在高校图书馆流通中的管理初探

介绍了高校图书馆随书光盘的特点,阐述了随书光盘在高校图书馆流通中管理现状及存在的问题,提出了在流通管理中优化随书光盘管理的若干设想。     

科技产业的发展可以实现自然生态循环的良性平衡

分析了工业化对自然生态循环平衡的破坏,指出科技是促进生态环境良性平衡的根本要素,并对科技如何实现生态循环良性平衡进行了思考。     

荒漠化扩展对我国区域气候变化影响的数值模拟

使用区域气候模式RegCM3研究了西北沙漠面积变化对我国区域气候变化的影响．共设计了3组试验：控制试验A、沙漠面积扩展试验B、在试验B基础上增大粗糙高度的试验C．分析表明：中国西北沙漠区扩展后对中国夏季降雨量和中国夏季风有明显影响．结果表明：植被退化、荒漠化加剧会导致季风减弱，降水量减少，增大地面粗糙高度后的影响更为显著．     

台风远离后舟山海域突发强风的诊断分析

台风是影响舟山的常见天气系统,台风影响时往往风雨交加。当0407号台风“蒲公英”穿越舟山时,舟山海域风不大,而台风离开后,舟山海域风力却突增到12级。这种情况是比较少见的,危害性很大。利用Micaps平台对台风周围的温度场、变压场、梯度场等大气环流进行分析,发现冷气团与台风外围暖气团相遇,生成了1对中尺度气压偶。因此,冷空气的侵入是造成这次强风的根本原因。     

平流层爆发性增温的时空分布特征

利用1950～2003年逐日平均NCEP资料,对平流层爆发性增温（SSW）的特征进行了统计分析,得到如下结果：北半球SSW具有多发性,在这53年里共发现了69次增温事件,平均每年一次以上,有些年份甚至出现2～3次;SSW中心位置随高度变化,在较低层（16 km附近）中心位置大部分偏于西半球的北美北部到北极地区,高层（30 km附近）附近其中心多偏于东半球欧亚大陆的北边到北极地区;北半球SSW最先发生在30 km附近的欧亚大陆以北地区,然后由上向下延伸和传递,同时中心位置也逐渐转到西半球的北美大陆北端;在北半球发生SSW期间,平流层温度场和环流场的变化也会影响到对流层,引起对流层温度场和环流场的变化.对2002年9月发生在南半球平流层的一次强爆发性增温进行分析表明,南半球的这次SSW发生时表现出的特征与北半球稍有不同,在较低层（16 km附近）SSW中心出现在东半球的南端,在较高层（25～30 km）SSW中心位于西半球的南端.     

高校扩招后图书馆流通部提高服务质量探讨

高校扩招后,图书馆流通部遇到了读者陡增与工作人员严重不足,工作量增大与读者服务质量要求越来越高等新矛盾.本文从新形势下的服务要求出发,分析了扩招后高校图书馆流通部服务质量上不去的主要原因,提出了重视流通服务工作;聘用学生馆员;延长开放时间等提高流通服务质量的对策.