1971-2000年青藏高原气候变化趋势

Trends of annual and monthly temperature, precipitation, potential evapotranspi- ration and aridity index were analyzed to understand climate change during the period 1971–2000 over the Tibetan Plateau which is one of the most special regions sensitive to global climate change. FAO56–Penmen–Monteith model was modified to calculate potential evapotranspiration which integrated many climatic elements including maximum and mini- mum temperatures, solar radiation, relative humidity and wind speed. Results indicate gen- erally warming trends of the annual averaged and monthly temperatures, increasing trends of precipitation except in April and September, decreasing trends of annual and monthly poten- tial evapotranspiration, and increasing aridity index except in September. It is not the isolated climatic elements that are important to moisture conditions, but their integrated and simulta- neous effect. Moreover, potential evapotranspiration often changes the effect of precipitation on moisture conditions. The climate trends suggest an important warm and humid tendency averaged over the southern plateau in annual period and in August. Moisture conditions would probably get drier at large area in the headwater region of the three rivers in annual average and months from April to November, and the northeast of the plateau from July to September. Complicated climatic trends over the Tibetan Plateau reveal that climatic factors have nonlinear relationships, and resulte in much uncertainty together with the scarcity of observation data. The results would enhance our understanding of the potential impact of climate change on environment in the Tibetan Plateau. Further research of the sensitivity and attribution of climate change to moisture conditions on the plateau is necessary.     

基于形态学的海洋锋形态特征提取

根据形态学梯度理论:不同尺寸的结构元素适合不同空间尺度的特征提取,结构元素尺寸的过大或者过小都会达不到最佳的特征边缘提取效果,从结构元素的尺寸δ与海洋锋横断面宽度γ和海流流幅的空间尺度λ的理论关系图推导中,提出δ,γ和λ的最佳定量关系:δ=γ/2,且δ<=λ/2,旨在对海洋锋形态特征进行提取。最后,以黑潮和墨西哥湾流为实验数据,进行海洋锋形态特征的自动提取,实验结果表明该定量关系的正确性和有效性。     

数学形态学在GIS空间分析中的应用

讨论了数学形态在基于栅格数据结构的地理信息系统空间分布中的广泛应用。提出基于形态变换的ＧＩＳ空间操作方法，网络最短路径的形态学算法，应用灰度级形态学解求通视图的新思路。     

辽东苏子河盆地叶肢介化石

本文描述的叶肢介化石是采自辽东中生代苏子河盆地的小岭组、梨树沟组和聂尔库组。小岭组产Eosestheria(Allestheria);梨树沟组产Yanjiestheria;聂尔库组产Orthestheria,Orthestheriopsis。Yanjiestheria,Neodiestheria。梨树沟组、聂尔库组所产化石为典型的延吉叶肢介群分子,属旱白垩世当无疑议。小岭组的时代从伴生的其它门类化石看亦归属早白垩世为宜。苏子河盆地所产叶肢介为延吉叶肢介群,故梨树沟组、聂尔库组与辽西九佛堂组和阜新组不能对比,这是因为辽西九佛堂组所产叶肢介为东方叶肢介群,其层位应在延吉叶肢介群之下。     

复杂背景下被动FTIS定量遥感污染云团光谱

本文提出复杂背景下定量遥感污染云团光谱的算法。利用被动傅里叶变换红外光谱仪（ＦＴＩＳ）遥测目标气体和背景光谱数据及最小平方误差拟合方法,成功地解决了探测目标气体柱数密度和目标气体等效辐射温度。该处理方法不仅可用于特定污染云团的定量处理,而且可用于多种污染地区如发电厂、机场、城市交叉路口、垃圾处理站等对ＣＯ,ＣＯ２,ＮＯ,ＮＯ２,Ｎ２Ｏ,ＮＨ３,ＣＨ４,ＳＯ２,Ｈ２Ｏ,ＨＣＩ和ＨＣＨＯ等气体浓度的监测。最后,详细讨论了用该算法对模拟剂的处理结果。     

内蒙古巴林右旗三叠纪化石的新发现

巴林右旗位于内蒙古东部,地处大兴安岭南段。自１９７２年内蒙古区调二队＊＊提出相邻的陶海营子等地存在着三叠纪地层以来,大兴安岭南段三叠系的存在与否就一直有着不同的认识。在内蒙古区调二队（１９８８）进行１／５万地质填图之后,朱儒峰等（１９９２）根据发现的...     

付里叶形状分析方法及其在地质学中的应用

作为1种有效的定量分析方法。付里叶形状分析已被应用到地质学诸多分支学科的研究中，如沉积学、岩石学、微体古生物学等。文中简要介绍付里叶形状定量分析的基本原理和方法，特别是闭合式付里叶分析方法及其在地质学中的应用。应用实例之一是南极沉积物源的解释，即怎样区分冰期海洋沉积物和冰蓣物；之二是研究反映生态环境变化的浮游有孔虫G．truncatulionoides的形状。其付里叶形状定量分析结果与δ^18O同位素数据相吻合。     

数学形态学方法在海面船目标检测中的应用

为进一步提高检测精度，提出1种将数学形态学方法应用到船目标检测数据后处理中的算法，根据该算法设计的数学形态学滤波器可以有效地消除SAR图像斑点噪声在船目标检测中造成的影响，减少船目标检测的误判，提高参数估计准确性。