PAN Guang dong, WANG Chao, ZHANG Wei guo, et al. Analysis of Seasonal Change of Land Cover Characteristics with SSM/I Data in China[J]. Journal of Remote Sensing, 2003,(6):498-503.
PAN Guang dong, WANG Chao, ZHANG Wei guo, et al. Analysis of Seasonal Change of Land Cover Characteristics with SSM/I Data in China[J]. Journal of Remote Sensing, 2003,(6):498-503. DOI: 10.11834/jrs.20030611.
By processing and analyzing space borne multi frequency microwave radiometry data acquired by SSM/I in different time
we aim at carrying out research on seasonal change of land cover characteristics in China. Through a short review on passive microwave remote sensing applications
we choose Normalized polarization index( NDPI ) to describe land cover characteristics. Because NDPI is independent of surface temperature
it diminishes difference caused by acquiring time in data in various regions. It is also shown that NDPI is actually a normalized emissivity of different polarization. Its main influence factors are vegetation biomass and soil surface moisture. With biomass increasing
NDPI increases also. Multi frequency SSM/I data acquired in April
July
October of 1997 and January of 1998(20 th and 24 th of every month )were processed and analyzed. Then the SSM/I NDPI maps over land in China were put forward for the first time. These maps express seasonal change of land cover characteristics in China. By analyzing all of these data and maps
we found that specific land cover has specific NDPI value and NDPI value changes with season.It is concluded that the NDPI maps has great potential to monitor land cover characteristics. The general trend of NDPI is (from high to low):desert
semi desert
plateau(grassland)
agricultural region and forest .The research illustrates that 19GHz NDPI is a good indicator of seasonal change of land cover characteristics. This paper also provides a new method to research on global change (such as vegetation and soil moisture change) because we have demonstrated in the paper that a NDPI map covering all of China can be formed by using only two day’s SSM/I data
and furthermore
this map is affected little by cloud and is independent of surface temperatrue.