CAJ | 학술논문

本文以地球系统科学和地球力学为理论基础,以遥感(RS)、地理信息系统(GIS)、全球定位系统(GPS)为技术支撑,利用亚东-格尔木-锡铁山走廊域的地学剖面实测温度数据和青藏高原MODIS遥感影像数据,分析研究了青藏高原亚东-格尔木-锡铁山走廊域的热环境特征.通过研究表明,研究区域内热环境总体分布规律为中东部最高,东南部次之,西北部最低.
본문이지구계통과학화지구역학위이론기출,이요감(RS)、지리신식계통(GIS)、전구정위계통(GPS)위기술지탱,이용아동-격이목-석철산주랑역적지학부면실측온도수거화청장고원MODIS요감영상수거,분석연구료청장고원아동-격이목-석철산주랑역적열배경특정.통과연구표명,연구구역내열배경총체분포규률위중동부최고,동남부차지,서북부최저.
With the earth system science and earth mechanics as the theoretical foundation, the technologies of Remote Sensing (RS), Geographic Information System (GIS) and Global Positioning System (GPS) as the technical support, and the field geoscience transection temperature measured in the Yadong-Golmud-Xitieshan corridor and the MODIS data of Qinghai-Tibet Plateau as the basic data, the authors made a detailed investigation and analysis of the thermal environment characteristics of the Yadong-Golmud-Xitieshan corridor. It is shown that the thermal environment distribution in the study area is the highest in the central eastern part, intermediate in the southeastern part, and the lowest in the northwestern part.