中文摘要：

在由有单个 time/dual 隧道裂口窗户算法的 GMS-5/VISSR 热红外线的数据的这份报纸的检索结果揭示特征日报、季节几代表性的陆地表面的清楚天空的陆地表面温度( LST )的变化录入中国包括 Tarim 盆，Qinghai西藏的高原， Hunshandake 沙，诺思中国平原，并且华南。在上面的区域的清楚天空的 LST 的季节的变化由太阳的放射为影响的不同表面反照率，土壤水内容，和程度清楚地变化。每月的一般水准日报 LST 的范围在一年里有二座山峰和二条山谷。在东亚和在台湾海峡和黄海的南方的海表面温度(SST ) 的大多数土地的 LST 的特征也作为比较被分析。Tarim 盆和 Hunshandake 沙有可观的 LST 不仅日报周期而且显著季节的变化。在 2000，最大的每月的一般水准日报在两个区域的 LST 的范围在 Hunshadake 沙活动范围是超过 30 K，和年度范围 58.50 K。在 Qinghai 西藏的高原的 LST 的季节的变化是在东亚， Tarim 盆，和 Hunshandake 沙的不到那些。然而，最大值日报范围在这个区域存在。每年的一般水准日报范围是在在 2000 的 Qinghai 西藏的高原的 28.05 K。特征日报、季节、年度从 1998 ～ 2000 的变化也在这研究被显示出。所有结果将对为陆地表面类型的变化的气候变化，放射平衡，和评价的研究珍贵。[出版摘要]

英文摘要：

The retrieved results in this paper by GMS-5/VISSR thermal infrared data with single time/dual channel Split-Window Algorithm reveal the characteristics of diurnal and seasonal variation of clear-sky land surface temperature （LST） of several representative land surface types in China, including Tarim Basin, QinghaiTibetan Plateau, Hunshandake Sands, North China Plain, and South China. The seasonal variation of clear-sky LST in above areas varies distinctly for the different surface albedo, soil water content, and the extent of influence by solar radiation. The monthly average diurnal ranges of LST have two peaks and two valleys in one year. The characteristics of LST in most land of East Asia and that of sea surface temperature （SST） in the south of Taiwan Strait and the Yellow Sea are also analyzed as comparison. Tarim Basin and Hunshandake Sands have not only considerable LST diurnal cycle but also remarkable seasonal variation. In 2000, the maximum monthly average diurnal ranges of LST in both areas are over 30 K, and the annual range in Hunshadake Sands reaches 58.50 K. Seasonal variation of LST in the Qinghai-Tibetan Plateau is less than those in East Asia, Tarim Basin, and Hunshandake Sands. However, the maximum diurnal range exists in this area. The yearly average diurnal range is 28.05 K in the Qinghai-Tibetan Plateau in 2000. The characteristics of diurnal, seasonal, and annual variation from 1998 to 2000 are also shown in this research. All the results will be valuable to the research of climate change, radiation balance, and estimation for the change of land surface types.