基于MODIS数据的陕西省地表温度时空分布特征研究
emporal and spatial distribution characteristics of land surface temperature in Shaanxi province using MODIS data
利用2001-2011年MODIS地表温度(LST)数据,采用最大值合成法、均值法、差值法对陕西省11a的LST的时空分布特征进行了分析。结果表明:11a间,陕西省的LST呈现上下波动的变化趋势,总体比较稳定,陕北、陕南、关中三区域的均值LST表现为:陕北>关中>陕南;LST的年内变化陕北最为剧烈,陕南最为平缓,关中次之,且具有明显的季节性,夏季最大,冬季最小,春季和秋季相当,南北LST差值夏季最大,冬季最小,在6月份达到LST全年最大。在空间分布上,随着纬度的增加,年均LST由南至北逐渐增加,陕北的变化最为显著,关中和陕南的变化较小;年内LST的变化有所差异,冬时段的LST沿南至北减少,春季-秋季的LST的变化特征则相反。这些特征都是受气候、地形、下垫面地表覆盖类型等因素共同影响的结果。
his paper is mainly on analyzing the temporal and spatial distribution characteristics of Land Surface Temperature (LST) in Shaanxi province using MODIS/LST time series data from 2001 to 2011. The results show that the LSTs are relatively stable in most areas of Shaanxi province in the past 11 years. The yearly average values of LST in Shaanbei are larger than those in Guanzhong plain, and the values in Shaannan are the smallest. In the three areas, the inner-annual variations of LSTs in Shaanbei are much stronger that those in Quanzhong and Shaanan, and the variations of LST appear obvious seasonal differences during the past years. The values of LSTs are highest in summer, lowest in winter, and are similar in spring and autumn, meanwhile, and the value of LSTs reach their maximum in June. In spatial distribution, the annual changes of average LSTs increase gradually from south to north. The changes of LST are significant in Shaanbei, and are steady in Guanzhong and Shaannan. Meanwhile, the variations of LST in a year are different. The LSTs decrease gradually from south to north in the period of winter, but those in the other periods are opposite. All these temperature characteristics are affected by climate, topography, land surface coverage types and urban heat island effect factors.
王小华、王鹏新、田苗、景毅刚、张树誉
自然地理学
MODIS地表温度时空变化陕西省
MODISLand Surface TemperatureTemporal and spatial variationShaanxi province
王小华,王鹏新,田苗,景毅刚,张树誉.基于MODIS数据的陕西省地表温度时空分布特征研究[EB/OL].(2012-05-18)[2025-05-10].http://www.paper.edu.cn/releasepaper/content/201205-331.点此复制
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