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基于PROSAIL模型,结合野外实测叶片等水分厚度、干物质重量、叶面积指数数据,构建一种基于归一化红外指数和归一化干物质指数的植被冠层可燃物含水率估算方法。首先,在PROSAIL模型输入实测参数模拟植被冠层光谱曲线,计算归一化红外指数、归一化干物质指数用于叶片等水分厚度、干物质重量的反演。结果表明:归一化红外指数与叶片等水分厚度、归一化干物质指数与干物质重量存在明显的线性关系,基于该关系建立叶片等水分厚度、干物质重量的经验估算模型,经验证估算结果精度较高;将该经验模型推广至利用Landsat 8数据拟合植被冠层可燃物含水率,并与实测数据进行验证,结果显示R2达到0.743,RMSE达到34.2%,具有较高的精度。文章提出的植被冠层可燃物含水率估算模型,可实现广州市过渡带森林大面积、较高精度植被冠层可燃物含水率监测,为预防森林火灾提供参考。 相似文献
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提出了一种新的遥感相机在轨点扩散函数测量方法,在阶跃响应法基础上,深入分析了倾斜角度、尺寸、插值、对比度、像素饱和、噪声等因素的影响,通过选取满足条件的阶跃区域并进行采样相位弱化处理,增加了测量结果的准确度。通过对实际全色谱段遥感图像的实验,验证了方法的有效性与可靠性,并利用所测点扩散函数对退化图像进行了复原,复原图像质量明显提高。 相似文献
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面向数字城市的空间应用服务互操作模型研究 总被引:7,自引:0,他引:7
该文从模型驱动的角度研究空间信息共享与GIS应用服务的互操作。首先分析数字城市服务系统的体系结构及GIS领域在互操作方面存在的困难,对OMG的模型驱动架构作了较详细的研究。认为对于数字城市中多领域众多应用系统互操作的情况,需要从一开始就结合目前相关的地理信息标准和规范,按照MDA的架构和原则设计—系列系统共同遵循的模型。并探索了如何按照这种思想为不同的GIS应用系统设计和建立公共模型、方法、工具和系统框架。以一个应用实例介绍如何在实践中应用这种思想和方法。 相似文献
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辽宁省14市经济与环境协调度定量研究 总被引:6,自引:0,他引:6
协调度理论已成为研究区域经济发展与环境保护耦合程度的重要理论。本文在阐述其理论的基础上,建立了经济环境协调度的指标体系、模型和计算方法。通过对辽宁省14市10年各项指标数据的技术处理和分析:辽宁省1996-2005年经济环境协调度整体处于调和阶段,在空间分布上,协调度值高的城市大都分布在南部沿海地区,协调度值低的大部分在辽宁省东部和西部;1996年以来辽宁省经济环境协调度的发展趋势呈"V"型变化,"九五"向"十五"过渡阶段协调度最低;经济环境协调度与经济发展阶段符合"U"型曲线,工业化初中期即第二经济发展阶段的协调度最低;1996-2005年期间14个市的经济环境协调度呈现出不均衡发展,其中大连市的协调度值较高。最后,本文认为应以大连市为龙头,与其他协调度值较低的城市实施区域合作战略,从而达到全省各市的经济发展与环境保护协调同步。 相似文献
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Based on the Had ISST1 and NCEP datasets,we investigated the influences of the central Pacific El Ni?o event(CP-EL)and eastern Pacific El Ni?o event(EP-EL)on the Sea Surface Temperature(SST)anomalies of the Tropical Indian Ocean.Considering the remote ef fect of Indian Ocean warming,we also discussed the anticyclone anomalies over the Northwest Pacific,which is very important for the South China precipitation and East Asian climate.Results show that during the El Ni?o developing year of EP-EL,cold SST anomalies appear and intensify in the east of tropical Indian Ocean.At the end of that autumn,all the cold SST anomaly events lead to the Indian Ocean Dipole(IOD)events.Basin uniform warm SST anomalies exist in the Indian Ocean in the whole summer of EL decaying year for both CP-and EP-ELs.However,considering the statistical significance,more significant warm SST anomalies only appear in the North Indian Ocean among the June and August of EP-EL decaying year.For further research,EP-EL accompany with Indian Ocean Basin Warming(EPI-EL)and CP El Ni?o accompany with Indian Ocean Basin Warming(CPI-EL)events are classified.With the remote ef fects of Indian Ocean SST anomalies,the EPI-and CPI-ELs contribute quite differently to the Northwest Pacific.For the EPI-EL developing year,large-scale warm SST anomalies arise in the North Indian Ocean in May,and persist to the autumn of the El Ni?o decaying year.However,for the CPI-EL,weak warm SST anomalies in the North Indian Ocean maintain to the El Ni?o decaying spring.Because of these different SST anomalies in the North Indian Ocean,distinct zonal SST gradient,atmospheric anticyclone and precipitation anomalies emerge over the Northwest Pacific in the El Ni?o decaying years.Specifically,the large-scale North Indian Ocean warm SST anomalies during the EPI-EL decaying years,can persist to summer and force anomalous updrafts and rainfall over the North Indian Ocean.The atmospheric heating caused by this precipitation anomaly emulates atmospheric Kelvin waves accompanied by low level easterly anomalies over the Northwest Pacific.As a result,a zonal SST gradient with a warm anomaly in the west and a cold anomaly in the east of Northwest Pacific is generated locally.Furthermore,the atmospheric anticyclone and precipitation anomalies over the Northwest Pacific are strengthened again in the decaying summer of EPI-EL.Af fected by the local WindEvaporation-SST(WES)positive feedback,the suppressed East Asian summer rainfall then persists to the late autumn during EPI-EL decaying year,which is much longer than that of CPI-EL. 相似文献
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