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城市地表温度遥感:从方向温度、全表面温度到三维表面温度

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城市地表温度是城市下垫面能量收支和局地气候变化的重要参数,较大范围的城市地表温度一般通过遥感技术手段获取。城市地表显著的三维结构,使其具有较强的热辐射方向性。热红外遥感通常可以提供传感器在特定方向视场中所有组分表面的平均温度(即方向温度),方向温度随传感器观测角度变化,且与城市表面温度的真实分布状况存在差异。为更好地表征城市下垫面与大气的能量交换,已有研究常采用"全表面温度"代表城市表面温度特征。目前,"全表面温度"仅在描述城市表面温度的平均状况方面有所突破,但无法体现城市表面温度的高时空分辨率特征,不能满足精细城市热环境评估的需求。本文梳理了城市地表温度从"方向温度"(二维)到"全表面温度"(2。5维)再到"三维表面温度"(三维)的发展脉络;概括了目前利用遥感方向观测获取城市地表不同维度温度的进展;厘清了不同维度城市地表温度的差异及其相互关系;阐述了不同维度城市地表温度的应用。在总结存在的问题的基础上,指出了城市地表温度遥感的未来发展趋势:(1)面向应用的城市三维表面温度定义;(2)面向城市三维表面温度重建的立体化观测;(3)三维表面温度产品与城市气候模型的耦合。
Remotely sensed urban surface temperature:From directional temperature,complete surface temperature to three-dimensional surface temperature
Urban land surface temperature is an important indicator of the energy budget of urban underlying surface and local climate change.Remote sensing is an important tool to obtain urban land surface temperature at a large spatial scale.Remarkable urban three-dimensional structure and complex urban surface materials substantially influence the directional variation in upwelling thermal radiance.Thermal infrared remote sensing typically provides an average temperature(i.e.,directional temperature)of all component surfaces in a sensor's field of view at a specific viewing direction.The directional temperature varies with the sensor's observation angle and differs from the true distribution of urban surface temperature.The term"complete surface temperature"was proposed to represent the characteristics of urban surface temperature to characterize the energy exchange between the urban underlying surface and the atmosphere.Currently,"complete surface temperature"has only made a breakthrough in describing the average state of urban surface temperature,but it still cannot reflect the high-resolution spatiotemporal characteristics of urban surface temperature and cannot meet the needs of fine-scale assessments of urban thermal environment.In this review,we summarize the development of urban surface remote sensing temperature from"directional temperature"(2-dimensional)to"complete surface temperature"(2.5-dimensional)and then to"3-dimensional surface temperature"(3-dimensional)and the current progress in using remote sensing directional observations to obtain urban surface temperature in different dimensions.We also clarify the differences and interrelationships of different dimensions.The application of remotely sensed urban surface temperature in different dimensions is also elaborated.On the basis of the existing problems,the future development trend of remotely sensed urban surface temperature is determined as follows:(1)definition of three-dimensional urban surface temperature for different application purposes,(2)stereoscopic observation for the reconstruction of three-dimensional urban surface temperature,and(3)coupling of three-dimensional surface temperature products and urban climate models.

urban remote sensingland surface temperaturedirectional temperaturecomplete surface temperaturethree-dimensional surface temperature

陈云浩、王丹丹、占文凤、周纪、胡德勇、全金玲、孙灏、郭徵、夏海萍、代秀娟、姜璐

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北京师范大学地理科学学部遥感科学国家重点实验室,北京 100875

中国地质大学(北京)土地科学技术学院,北京 100083

南京大学江苏省地理信息技术重点实验室/南京大学国际地球系统科学研究所,南京 210023

江苏省地理信息资源开发与利用协同创新中心,南京 210023

电子科技大学资源与环境学院,成都 611731

首都师范大学资源环境与旅游学院,北京 100048

中国科学院地理科学与资源研究所资源与环境信息系统国家重点实验室,北京 100101

中国矿业大学(北京)地球科学与测绘工程学院,北京 100083

中国气象局中国遥感卫星辐射测量和定标重点开放实验室/国家卫星气象中心(国家空间天气监测预警中心),北京 100081

气象卫星创新中心,北京 100081

杭州师范大学遥感与地球科学研究院,杭州 311121

南京邮电大学地理与生物信息学院,南京 210023

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城市遥感 地表温度 方向温度 全表面温度 三维表面温度

国家自然科学基金国家自然科学基金国家自然科学基金

4217131642101333U23A2018

2024

遥感学报
中国地理学会环境遥感分会 中国科学院遥感应用研究所

遥感学报

CSTPCD北大核心
影响因子:2.921
ISSN:1007-4619
年,卷(期):2024.28(6)