排序方式： 共有11条查询结果，搜索用时 62 毫秒
1.
Performance of a Reconfigured Atmospheric General Circulation Model at Low Resolution 总被引：3，自引：2，他引：3
Paleoclimate simulations usually require model runs over a very long time.The fast integration version of a state-of-the-art general circulation model (GCM),which shares the same physical and dynamical processes but with reduced horizontal resolution and increased time step,is usually developed.In this study,we configure a fast version of an atmospheric GCM (AGCM),the Grid Atmospheric Model of IAP/LASG (Institute of Atmospheric Physics/State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics),at low resolution (GAMIL-L,hereafter),and compare the simulation results with the NCEP/NCAR reanalysis and other data to examine its performance.GAMIL-L,which is derived from the original GAMIL,is a finite difference AGCM with 72×40 grids in longitude and latitude and 26 vertical levels.To validate the simulated climatology and variability,two runs were achieved.One was a 60-year control run with fixed climatological monthly sea surface temperature (SST) forcing,and the other was a 50-yr (1950-2000) integration with observational time-varying monthly SST forcing.Comparisons between these two cases and the reanalysis,including intra-seasonal and inter-annual variability are also presented.In addition,the differences between GAMIL-L and the original version of GAMIL are also investigated. The results show that GAMIL-L can capture most of the large-scale dynamical features of the atmosphere, especially in the tropics and mid latitudes,although a few deficiencies exist,such as the underestimated Hadley cell and thereby the weak strength of the Asia summer monsoon.However,the simulated mean states over high latitudes,especially over the polar regions,are not acceptable.Apart from dynamics,the thermodynamic features mainly depend upon the physical parameterization schemes.Since the physical package of GAMIL-L is exactly the same as the original high-resolution version of GAMIL,in which the NCAR Community Atmosphere Model (CAM2) physical package was used,there are only small differences between them in the precipitation and temperature fields.Because our goal is to develop a fast-running AGCM and employ it in the coupled climate system model of IAP/LASG for paleoclimate studies such as ENSO and Australia-Asia monsoon,particular attention has been paid to the model performances in the tropics.More model validations,such as those ran for the Southern Oscillation and South Asia monsoon, indicate that GAMIL-L is reasonably competent and valuable in this regard. 相似文献
2.
垂直低分辨率GCM模式大气平均经圈环流的诊断 总被引：9，自引：2，他引：9
王盘兴 《南京气象学院学报》1994,17(2):200-204
以ＩＡＰ２－Ｌ ＧＣＭ为例，给出垂直低分辨率ＧＣＭ模式大气平均经圈环流质量流函数的一个计算方案，结果表明，模式大气的Ｈａｄｌｅｙ环流季节变化与实际大气相一致。Ｅｌ Ｎｉｎｏ年模式大气平均经圈环流中可分离出一个与Ｅｌ Ｎｉｎｏ型ＳＳＴ异常关系密切的异常经圈环流，它导致平均Ｈａｄｌｅｙ环流向北半球盛夏型转变的滞后。 相似文献
3.
A fast version of LASG/IAP climate system model and its 1000-year control integration 总被引：2，自引：1，他引：1
A fast version of the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geo- physical Fluid Dynamics(LASG)/Institute of Atmospheric Physics(IAP)climate system model is briefly documented.The fast coupled model employs a low resolution version of the atmospheric component Grid Atmospheric Model of IAP/LASG(GAMIL),with the other parts of the model,namely an oceanic component LASG/IAP Climate Ocean Model(LICOM),land component Common Land Model(CLM),and sea ice component from National Center for Atmospheric Research Community Climate System Model (NCAR CCSM2),as the same as in the standard version of LASG/IAP Flexible Global Ocean Atmosphere Land System model(FGOALS g).The parameterizations of physical and dynamical processes of the at- mospheric component in the fast version are identical to the standard version,although some parameter values are different.However,by virtue of reduced horizontal resolution and increased time-step of the most time-consuming atmospheric component,it runs faster by a factor of 3 and can serve as a useful tool for long- term and large-ensemble integrations.A 1000-year control simulation of the present-day climate has been completed without flux adjustments.The final 600 years of this simulation has virtually no trends in global mean sea surface temperatures and is recommended for internal variability studies.Several aspects of the control simulation’s mean climate and variability are evaluated against the observational or reanalysis data. The strengths and weaknesses of the control simulation are evaluated.The mean atmospheric circulation is well simulated,except in high latitudes.The Asian-Australian monsoonal meridional cell shows realistic features,however,an artificial rainfall center is located to the eastern periphery of the Tibetan Plateau persists throughout the year.The mean bias of SST resembles that of the standard version,appearing as a"double ITCZ"(Inter-Tropical Convergence Zone)associated with a westward extension of the equatorial eastern Pacific cold tongue.The sea ice extent is acceptable but has a higher concentration.The strength of Atlantic meridional overturning is 27.5 Sv.Evidence from the 600-year simulation suggests a modulation of internal variability on ENSO frequency,since both regular and irregular oscillations of ENSO are found during the different time periods of the long-term simulation. 相似文献
4.
5.
高,低分辨率模式对典型个例的对比预报试验 总被引：3，自引：2，他引：3
利用实时观测资料Ｔ６３模式预报产品资料，对１９９５年７－８月发生在西北地区的３次大雨、暴雨天气过程进行了高、低分痃率数值预报模式的对比预报试验。 相似文献
6.
遥感影像空间尺度特性与最佳空间分辨率选择 总被引：13，自引：2，他引：11
尺度概念是理解地球系统复杂性的关键,尺度问题被认为是对地观测的主要挑战之一,而结合具体研究应用领域,由地学现象的尺度本身出发,选择所需遥感影像的最佳尺度和分辨率,是非常有现实意义的.本文在深入剖析了遥感影像的尺度特性和遥感影像尺度选择的意义的基础上,探讨了基于地统计学方法定量选择遥感影像最佳空间分辨率的方法.阐明了传统局部方差方法不能得到理想结果的原因:传统的局部方差方法的实质是基于变化地面面积计算影像局部方差的均值,而基于这样不同甚至是相差悬殊的地面面积进行局部方差计算,其结果必然不具有可比性.对此,本文提出了基于可变窗口与可变分辨率的改进局部方差方法,即依次降低空间分辨率时,高分辨率采用大窗口尺寸,低分辨率采用小窗口尺寸来维持计算窗口内的地面面积的一致,由此计算出的局部方差作比较来判定遥感影像最佳分辨率.进行了系列实验分析,得到了相关结论,分析得出这种基于地统计的方法来选择遥感影像最佳分辨率的方法,对遥感和GIS研究与地学应用具有一定的理论意义和指导意义. 相似文献
7.
在对太湖、巢湖等大型湖泊进行业务化蓝藻水华遥感监测工作中,常以250 m空间分辨率的MODIS数据为主,但其像元多为水体和水华的混合像元,若用常规方法进行水华面积提取,势必会严重影响水华监测的精度和实际应用效果。针对上述问题,基于混合像元分解原理,通过混合像元分解得到水华组分在混合像元中的丰度(百分比),实现亚像元级的水华面积提取。该方法可直接根据图像的DN值进行水华面积提取,无需对数据进行辐射校正和大气校正等预处理。与常规水华提取法相比,该方法的水华面积提取精度提高了近30%。 相似文献
8.
提高中巴卫星IR MSS图像空间分辨能力的光谱保真融合方法 总被引：3，自引：1，他引：3
介绍一种提高中巴资源卫星IRMSS图像空间分辨能力的光谱保真融合方法。通过计算低分辨率图像上每一个像元对应的高分辨率图像上一组子像元的平均亮度值及二者之差,将该差值与高分辨率图像上相应子像元亮度求和,形成新的图像。该图像具有高分辨率图像的空间细节,又具有低分辨率图像的光谱信息,从而实现融合图像信息保真。试验表明,光谱保真融合方法可以在不改变光谱信息的前提下提高IRMSS图像的空间分辨能力,是一种新的简单实用的数据处理方法。 相似文献
9.
Pei-Sheng Chen Pin Zhang National Astronomical Observatories / Yunnan Observatory Chinese Academy of Sciences Kunming Cosmic Ray Institute Yunnan University Kunming 《中国天文和天体物理学报》2006,6(6):697-704
The discovery of silicate carbon star poses a challenge to the theory of stellar evolution in the late stage, hence it is important to look for more silicate carbon stars. To this end we have carried out cross-identifications between the new IRAS Low-Resolution Spectrum (LRS) database and the new carbon star catalog, CGCS3. We have found nine new silicate carbon stars with silicate features around 10μm and/or 18μm. These newly identified stars are located in the Regions IIIa and VII in the IRAS two-color diagram, which means they indeed have typical far infrared colors of silicate carbon stars. The infrared properties of each of these sources are discussed. 相似文献
10.
低分辨率遥感影像中道路的全自动提取方法研究 总被引：1，自引：0，他引：1
从Marr视觉计算理论出发,利用低分辨率遥感影像的特点,提出了一种基于边缘线段感知编组和动态规划跟踪线段的道路信息全自动提取方法.首先分析了低分辨率影像中道路的辐射特性和几何特性,以得到道路模型.然后在底层处理阶段对影像进行边缘检测、无效线段去除等预处理;中层处理阶段采用基于上下文关联的感知线段编组法得到候选道路段,并由道路段的置信度阈值确定道路种子点;最后在高层处理阶段提出基于动态规划的道路跟踪算法得到候选道路,并且采用知识推理去除部分虚警.实验结果表明:(1)对图像中背景干扰较大的山区道路和复杂的城区道路网均有较好的识别效果;(2)识别过程全自动进行,没有人工干预,因此计算效率相比其他方法有一定的优势;(3)由不同传感器卫星获取的影像如L7,SPOT,SAR等,算法均能进行有效识别,具有很好的普适性和稳健性. 相似文献