中文摘要：

基于2005年NCEP/GFS分析资料和拉格朗日粒子扩散模式的“Domain Filling”技术，以气块穿越对流层顶后的滞留时间为标准，诊断分析了夏季亚洲季风区对流层-平流层质量交换，重点讨论了对平流层大气成分收支具有实际意义的不可逆双向质量交换过程，并利用前向（后向）轨迹追踪方法，分析了其4天的“源（汇）”特征.研究结果表明：（1）对流层-平流层质量交换（Troposphere-Stratosphere mass Exchange，STE）的计算对滞留时间阈值的选择具有较强敏感性，大多数的气块在1～2天内可频繁地往返对流层顶.这些瞬时交换事件的考虑与否对穿越对流层顶的质量交换计算的准确性具有重要影响，尤其在中纬度的风暴轴区域.（2）从亚洲季风区对流层-平流层质量净交换纬向平均上看，45°N以南的区域为对流层向平流层的质量输送（Troposphere to Stratosphere mass Transport，TST），副热带地区为最强的上升支，而在45°N~55°N的中纬度地区是平流层向对流层质量输送（Stratosphere to Troposphere mass Transport，STT）.地理分布上，STT主要分布在青藏高原以北的东亚地区，与亚洲季风区夏季大尺度的槽区相对应.夏季整个亚洲季风区都是TST发生的区域，最大值位于青藏高原东南侧及其附近区域，该区域占亚洲季风区不可逆TST夏季平均总量的46%.（3）对流层-平流层质量交换的“源汇”特征分析表明，STT主要源于100°E以西、50°N以北的高纬地区，向下可以输送到中国东北部及朝鲜半岛北部等中纬度区域.而TST主要来源于中纬度和副热带地区的大气输送，向上穿越对流层顶高度以后，可分别向高纬的极地和热带地区输送，这意味着亚洲季风区夏季的TST水汽输送可能进入“热带管”中，进而可能对全球平流层水汽平衡产生重要影响.

英文摘要：

A particle dispersion model combined with “domain filling” technique is applied to the analyzed data from Global Forecast System of National Centers for Environmental Prediction （NCEP/GFS） to study the troposphere-to-stratosphere mass transport （TST） and the stratosphere-to-troposphere mass transport （STT） over the Asian monsoon region for the period from June to August in 2005. A residence time criterion serves to distinguish between transient （reversible） exchange and irreversible exchange, and special emphasis is paid to the later mass exchange, which has great impact on the budget of chemical constitutes in both the stratosphere and troposphere. The source and sink features in the irreversible exchange are also analyzed by trajectory-track method. The main conclusions can be summarized as follows：（1）The results show that the sensitivity of the Troposphere-Stratosphere mass Exchange （STE） distributions to the threshold residence time is pronounced at all latitudes. The major part of exchange air parcels return rapidly （within less than 1~2 days） to their “original sphere”. The quantitative STT and TST mass flux estimates are strongly dependent upon whether these transient events are considered or not.（2） In general, the overall analysis of STT, TST and net mass exchange reveals that upward and downward transport of mass at the middle and high latitude accompany with each other. The meridional distribution of the net flux reveals an upward branch in the subtropics, pronounced downward exchange in the midlatitudes from 45°N to 55°N latitude and weak upward fluxes in high latitude region. Detailed geographical distributions show strong downward cross tropopause mass flux mainly in the north of Tibetan Plateau, which corresponds to the large scale troughs in summer. The results also show that the whole Asian monsoon region is the region of upward cross tropopause mass flux. Tibetan Plateau and its adjoint regions are the main channels of the upward mass flux into the st