Based on the principle of transient perturbation analysis,in this paper,a method to objectively determine the weather pattern formed by sea fog is provided.On the basis of the classification results,the circulation si...Based on the principle of transient perturbation analysis,in this paper,a method to objectively determine the weather pattern formed by sea fog is provided.On the basis of the classification results,the circulation situation,divergence and vertical velocity field,and the vertical profile of temperature and humidity are synthesized and analyzed.The basic characteristics of the circulation and physical field of sea fog under low pressure control(L type sea fog)are obtained,and the results are compared with the sea fog under the control of high pressure(H type sea fog):a)L type sea fogs potential height anomaly disturbance is mainly manifested in the low layer,and its average value is-65.66 gpm,gradually weakening upward;b)L type sea fogs inversion structure is weaker than H type sea fogs when it occurs,the fog layer is thicker and the high relative humidity level is high over the fog layer,while the H type sea fogs fog layer has a relatively obvious dry layer;c)L sea fog has three layers of structure at the vertical direction.The first layer 1000-950 hPa is convergence accompanied by weak rise and subsidence,the second layer 950-850 hPa is divergence accompanied by weak subsidence,and the third layer 850 to 500hPa is gradually strengthened.While there are two layer structures of the H type sea fog.1000 hPa is divergence accompanied by weak rising and sinking movement,950-500 hPa is a uniform subsidence movement.d)Probability density statistical analysis further quantified the vertical movement of L and H type sea fog and the distribution of relative humidity in each layer.These conclusions provide an important reference for forecasting the sea fog in the northwest of the Yellow Sea under the condition of low pressure circulation in summer.展开更多
冰面水体是冰盖物质平衡的重要组成部分,在全球气候及环境变化研究中发挥着重要的作用。本文以格陵兰岛北部为研究区,选取该区域消融期内不同时相的WorldView-2影像,统计分析区域内典型地物光谱特性,构建了针对冰面水体的归一化水体增...冰面水体是冰盖物质平衡的重要组成部分,在全球气候及环境变化研究中发挥着重要的作用。本文以格陵兰岛北部为研究区,选取该区域消融期内不同时相的WorldView-2影像,统计分析区域内典型地物光谱特性,构建了针对冰面水体的归一化水体增强指数NEWI(Normalized Enhanced Water Index);依据影像上地物分布规律和直方图图形特征,定位冰雪混合物和冰面水体边缘地带灰度值相似的模糊区域,增强区域间地物对比度,提取出冰面水体的精细范围。实验结果表明,本研究所构建的指数有效凸显了冰面水体与非水体的反射率差异。与常用的水体指数NDWI等相比,冰川环境下,本文指数在提高区分度方面优势明显。通过精度评价可知,本文方法所提取出的冰面水体精细化程度高,提取结果完整,错误率低。本研究对冰面水体信息增强及精细化提取具有重要指导意义。展开更多
冰面湖是冰盖水文系统的重要组成部分,能够反映冰盖表面融水的特征,影响极地气候及环境变化。本文以冰面湖多发育区域格陵兰岛北部为研究区,基于WorldView-2高分辨率遥感影像,提出了一种综合光谱形态信息的冰面湖精细化提取方法。首先...冰面湖是冰盖水文系统的重要组成部分,能够反映冰盖表面融水的特征,影响极地气候及环境变化。本文以冰面湖多发育区域格陵兰岛北部为研究区,基于WorldView-2高分辨率遥感影像,提出了一种综合光谱形态信息的冰面湖精细化提取方法。首先结合适合冰面环境的水体指数NDWI_(ice)(normalized difference water index-ice)及分割阈值提取冰面水体;然后构建形态规则,将冰面水体分为独立冰面湖、独立冰面径流、混合区域3类;最后引入傅里叶描述子辅助分水岭算法精细化提取冰面湖。为验证该方法的可行性,选取一个消融期内9个时期的WorldView-2影像序列进行实验,与其他自动化方法及人工数字化结果比较,本文方法在提取准确率、完整性上均高于90%,平均错误率低于0.2%,优势明显。展开更多
As an important part of the mass balance of the Ice Sheet,Supra-glacial Water not only reflects the diversity of polar environmental changes,but also plays an important role in the study of global climate and environm...As an important part of the mass balance of the Ice Sheet,Supra-glacial Water not only reflects the diversity of polar environmental changes,but also plays an important role in the study of global climate and environmental changes.In this paper,we chose northern Greenland as the research area,and constructed a Normalized Enhanced Water Index(NEWI)based on the high-precision WorldView-2 images of different phases during the ablation period in northern Greenland,followed by a statistical analysis on the spectral characteristics of the images were for the typical features in the study area.Then the fuzzy areas with similar gray values of thin sea ice and shallow ice water bodies were located,according to the distribution rules of ground objects and histogram graphic features of the images,so as to enhance the contrast of ground objects between the regions,and finally the extraction of the fine range of water bodies on the ice surface.Experimental results showed that the proposed index effectively highlighted the ice water with the water of the reflectivity difference,compared with the commonly used water index NDWI,etc.,especially in shallow water,which contributes to differentiation from other objects.The precision evaluation showed that the applied method of extraction has higher degree of refinement compared with other methods,by which the ice water can get complete ice water effectively.展开更多
基金supported by National Natural Science Foundation of China(No.41576108 and No.41605006)Natural Science Foundation project of Shandong Province(No.ZR2016DB26).
文摘Based on the principle of transient perturbation analysis,in this paper,a method to objectively determine the weather pattern formed by sea fog is provided.On the basis of the classification results,the circulation situation,divergence and vertical velocity field,and the vertical profile of temperature and humidity are synthesized and analyzed.The basic characteristics of the circulation and physical field of sea fog under low pressure control(L type sea fog)are obtained,and the results are compared with the sea fog under the control of high pressure(H type sea fog):a)L type sea fogs potential height anomaly disturbance is mainly manifested in the low layer,and its average value is-65.66 gpm,gradually weakening upward;b)L type sea fogs inversion structure is weaker than H type sea fogs when it occurs,the fog layer is thicker and the high relative humidity level is high over the fog layer,while the H type sea fogs fog layer has a relatively obvious dry layer;c)L sea fog has three layers of structure at the vertical direction.The first layer 1000-950 hPa is convergence accompanied by weak rise and subsidence,the second layer 950-850 hPa is divergence accompanied by weak subsidence,and the third layer 850 to 500hPa is gradually strengthened.While there are two layer structures of the H type sea fog.1000 hPa is divergence accompanied by weak rising and sinking movement,950-500 hPa is a uniform subsidence movement.d)Probability density statistical analysis further quantified the vertical movement of L and H type sea fog and the distribution of relative humidity in each layer.These conclusions provide an important reference for forecasting the sea fog in the northwest of the Yellow Sea under the condition of low pressure circulation in summer.
文摘冰面水体是冰盖物质平衡的重要组成部分,在全球气候及环境变化研究中发挥着重要的作用。本文以格陵兰岛北部为研究区,选取该区域消融期内不同时相的WorldView-2影像,统计分析区域内典型地物光谱特性,构建了针对冰面水体的归一化水体增强指数NEWI(Normalized Enhanced Water Index);依据影像上地物分布规律和直方图图形特征,定位冰雪混合物和冰面水体边缘地带灰度值相似的模糊区域,增强区域间地物对比度,提取出冰面水体的精细范围。实验结果表明,本研究所构建的指数有效凸显了冰面水体与非水体的反射率差异。与常用的水体指数NDWI等相比,冰川环境下,本文指数在提高区分度方面优势明显。通过精度评价可知,本文方法所提取出的冰面水体精细化程度高,提取结果完整,错误率低。本研究对冰面水体信息增强及精细化提取具有重要指导意义。
文摘冰面湖是冰盖水文系统的重要组成部分,能够反映冰盖表面融水的特征,影响极地气候及环境变化。本文以冰面湖多发育区域格陵兰岛北部为研究区,基于WorldView-2高分辨率遥感影像,提出了一种综合光谱形态信息的冰面湖精细化提取方法。首先结合适合冰面环境的水体指数NDWI_(ice)(normalized difference water index-ice)及分割阈值提取冰面水体;然后构建形态规则,将冰面水体分为独立冰面湖、独立冰面径流、混合区域3类;最后引入傅里叶描述子辅助分水岭算法精细化提取冰面湖。为验证该方法的可行性,选取一个消融期内9个时期的WorldView-2影像序列进行实验,与其他自动化方法及人工数字化结果比较,本文方法在提取准确率、完整性上均高于90%,平均错误率低于0.2%,优势明显。
基金supported by the 2020 Key project of Science and Technology for Economy(Grant No. SQ2020YFF0426316)。
文摘As an important part of the mass balance of the Ice Sheet,Supra-glacial Water not only reflects the diversity of polar environmental changes,but also plays an important role in the study of global climate and environmental changes.In this paper,we chose northern Greenland as the research area,and constructed a Normalized Enhanced Water Index(NEWI)based on the high-precision WorldView-2 images of different phases during the ablation period in northern Greenland,followed by a statistical analysis on the spectral characteristics of the images were for the typical features in the study area.Then the fuzzy areas with similar gray values of thin sea ice and shallow ice water bodies were located,according to the distribution rules of ground objects and histogram graphic features of the images,so as to enhance the contrast of ground objects between the regions,and finally the extraction of the fine range of water bodies on the ice surface.Experimental results showed that the proposed index effectively highlighted the ice water with the water of the reflectivity difference,compared with the commonly used water index NDWI,etc.,especially in shallow water,which contributes to differentiation from other objects.The precision evaluation showed that the applied method of extraction has higher degree of refinement compared with other methods,by which the ice water can get complete ice water effectively.
