CAJ | 학술논문

[目的]研究不同土地利用类型的地表亮温变化规律。[方法]基于2008年的MODIS数据,以长三角为研究区,结合IGBP土地分类体系,计算地表亮温,总结规律,并对原因进行探讨。[结果]不同土地利用类型有其独特的亮温变化。白天亮温大小为草地、建筑用地〉农田、林地和荒地〉湿地和水体;夜间亮温大小为水体、湿地、荒地〉建筑用地、草地〉林地、农田。亮温全年呈现冬低夏高、春增秋减的趋势。夜间亮温更能反映地表热辐射特点。太阳辐射、混合像元、比热容、含水量等是导致不同地类亮温差异的主要原因。[结论]不同土地利用类型的亮温变化特点对于土壤含水量分析、土地利用动态监测等具有重要意义。
[목적]연구불동토지이용류형적지표량온변화규률。[방법]기우2008년적MODIS수거,이장삼각위연구구,결합IGBP토지분류체계,계산지표량온,총결규률,병대원인진행탐토。[결과]불동토지이용류형유기독특적량온변화。백천량온대소위초지、건축용지〉농전、임지화황지〉습지화수체;야간량온대소위수체、습지、황지〉건축용지、초지〉임지、농전。량온전년정현동저하고、춘증추감적추세。야간량온경능반영지표열복사특점。태양복사、혼합상원、비열용、함수량등시도치불동지류량온차이적주요원인。[결론]불동토지이용류형적량온변화특점대우토양함수량분석、토지이용동태감측등구유중요의의。
[Objective] The aim of this study is to investigate the surface brightness temperature variation of different land use types.[Method] Based on MODIS data in 2008 and IGBP land classification system,the surface brightness temperature in the Yangtze River Delta area was calculated,and its rules and reasons were also discussed in this study.[Result] Different land use types had its own special brightness temperature variation.During the day,the brightness temperature was as follows：grassland or urban and built-up landcropland,forest land and barrenwetland and water.During the night,the brightness temperature was as follows：water,wetland and barrengrassland or urban and built-up landforest land and cropland.Brightness temperature showed the trend of high in summer and low in winter or increasing in spring and decreasing in fall.The characteristics of surface thermal radiation could be reflected better by brightness temperature at night.Solar radiation,mixed pixel,heat capacity,water content were the main reasons for the difference of brightness temperature in different land types.[Conclusion] The brightness temperature variation of different land use types has significance for water content analysis in soil and dynamic monitoring of land use.