作者简介:陈云浩(1974-),男,安徽固镇人,教授,主要从事资源与环境遥感研究.E-mail:cyh@bnu.edu.cn
收稿日期: 2017-11-30
修回日期: 2018-04-06
网络出版日期: 2018-07-23
基金资助
*国家自然科学基金项目“城市下垫面热辐射方向性的多尺度几何模型”(编号:41471348)和“面向城市场景的地表等效发射率方向性差异核驱动模型”(编号:41771448)资助.
版权
Review of the Study on Generalized Computer Simulation of Land Surface Thermal Anisotropy
First author: Chen Yunhao(1974-), male, Guzhen County, Anhui Province, Professor. Research areas include application of remote sensing in resource. E-mail:cyh@bnu.edu.cn
Received date: 2017-11-30
Revised date: 2018-04-06
Online published: 2018-07-23
Supported by
Project supported by the National Natural Science Foundation of China “A muli-scale geometric model for urban thermal anisotropy”(No.41471348) and “Surface-driven emissivity directivity difference nuclear drive model for urban scenes” (No.41771448).
Copyright
地表温度反映了地球表面的能量变化与交换过程,是研究地球科学的一个重要指标。地表的几何结构和组分温度差异是地表热辐射在不同方向上存在差异性的主要原因,因此,大部分陆面都存在不同程度的热辐射方向性。介绍了广义热辐射方向性计算机模型的研究方法和研究现状,并从模型特点、模拟对象、模拟精度和时间复杂度等方面对常见模型进行评价,评述了耦合气候模型和地表热辐射方向性模型进行热辐射方向性研究中的应用情况,指出该领域尚未解决的问题并对未来的研究方向进行了展望。
关键词： 地表温度; 热辐射方向性模型; 方向亮温; 组分温度; Envi-met模型
陈云浩 , 吴佳桐 , 王丹丹 . 广义地表热辐射方向性计算机模拟研究进展[J]. 地球科学进展, 2018 , 33(6) : 555 -567 . DOI: 10.11867/j.issn.1001-8166.2018.06.0555
Land surface temperature reflects the energy change and exchange process of land surface, which is an important index of the study on Earth science. The differences of surface geometrical structure and morphology are the main reasons for directional thermal radiant anisotropy. Therefore, there is thermal radiant directionality on most land surfaces in some degrees. The research methods and research status of the generalized thermal radiation directivity computer model were introduced. The common models were evaluated from the characteristics of the model, simulation objects, simulation accuracy and time complexity. The coupled climate model, the surface radiation directivity model and the application of radiation directionality were reviewed. The unsolved problems and the future research direction in this field were pointed.
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