1) earth thermometer
地温表;地温计
2) land surface temperature
地表温度
1.
Study on land surface temperature vegetation cover relationship in urban region:a case in Shenzhen City;
城市地域地表温度-植被覆盖定量关系分析——以深圳市为例
2.
Methodology to retrieve land surface temperature from MODIS datafor agricultural drought monitoring in China;
农业旱灾监测中的地表温度遥感反演方法——以MODIS数据为例
3.
Retrieving land surface temperature-based on TM data from Kenli County,Shandong Province;
基于TM图像反演垦利县地表温度
3) LST
[英][,eles'ti:] [美][,ɛlɛs'ti]
地表温度
1.
Urban ground surface has an important effect on the energy exchange between air and land,which leads to an inhomogeneous distribution of land surface temperature(LST).
城市下垫面对地表能量交换的影响巨大,引起地表温度分布的不均一性。
2.
Split-window algorithm is the main method to retrieve the LST by thermal infrared data.
大气透过率和地表比辐射率是求解地表温度的两个关键参数。
4) brightness temperature
地表亮温
1.
The brightness temperature data,whose reliability is verified by the observed air temperature,and NDVI data of Hangzhou urban city was acquired from ETM+ image.
通过对杭州市区ETM+遥感影像数据的处理,提取该区域地表亮温和NDVI数据,并结合实测温度对亮温数据的可靠性进行了验证。
5) ground surface temperature
地表温度
1.
The NCEP/ NCAR reanalyzed climate data and NCAR ground surface temperature (GST) data are used to analyze the area index, longitude and latitude of the subtropical high in the western Pacific in summer and their relation with the Asia GST.
利用 ＮＣＥＰ／ ＮＣＡＲ再分析资料中的 ５００ ｈＰａ高度场资料和 ＮＣＡＲ地温资料，分析了６～８月西太平洋副热带高压的面积指数、西伸的经度和脊线的纬度等与亚洲地表温度之关系。
2.
Based on the simulation test and observation of ground surface temperature and total radiation on the hillside,a regression equation is obtained.
通过坡地地表温度和坡地总辐射的模拟试验观测,建立了推算丘陵山区地表温度与总辐射的回归关系式。
6) surface temperature
地表温度
1.
Estimate of soil moisture through surface temperature;
地表温度估测土壤含水量
2.
Vegetation index-surface temperature feature space and its application in the regional drought monitoring;
植被指数—地表温度特征空间研究及其在旱情监测中的应用
3.
Inversion and verification of land surface temperature with remote sensing TM/ETM~+ data;
针对TM/ETM~+遥感数据的地表温度反演与验证
补充资料：地温
地面及其以下的土壤温度。地面温度直接受太阳辐射的影响，白天高，夜间低；夏季高，冬季低。土壤温度的变化随深度增大而逐渐减小，约在1米深处，温度的日变化已消失。土壤深达20米以下时，地温的年变化也消失了。井水冬暖夏凉就是地温终年少变所致。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条