通过时间基准和空间基准的连接,对PSInSAR方法进行了扩展,对覆盖华北平原约20万km2的500余景Envisat ASAR数据进行了处理,获取了该地区2006~2010年的地表沉降速率。分析表明,华北平原多个沉降中心沉降速率处于较高发展态势,从北京-廊坊-天津到任丘、沧州、泊头、衡水、德州、南宫,再到邯郸,地面沉降已连成一片;天津市的静海-滨海地面沉降最为突出,两地沉降中心区的平均沉降速率分别达到62mm/a和67 mm/a,北京东部、沧州、泊头-衡水-德州、邯郸等老沉降区的沉降速率分别达到36 mm/a、34mm/a、37mm/a、29mm/a。利用天津地区同期水准测量结果检验了本文的研究结果,差值均小于10mm,表明PSInSAR方法反演结果与水准测量获得的结果是一致的。
Estimation of processes for slow change in small scale surfaces is one of the main advantages of PSInSAR technology.We present a mathematical framework for the datum connection for time-space referencing,applying it to 500 scenes composed of Envisat ASAR images covering about 200 000 km2 of the North China Plain,obtained the rate of ground subsidence in the study area during the pe-riod of 2006-2010.The experimental results show that:(1)the multiple subsidence centers in North China Plain were still in an evolving state,connecting Beijing,Langfang,Tianjin,Renqiu,Cang-zhou,Botou,Hengshui,Dezhou,Nangong and Handan into a continuous area.(2)The most promi-nent ground subsidence was in Tianjin’s Jinghai and Binhai areas having average subsidence rates of 62mm/a and 67mm/a along the line of sight,respectively.The subsidence of the old centers,to the east of Beijing,Cangzhou,Botou- Hengshui- Dezhou,Handan,had rates of 36mm/a,34mm/a, 37mm/a,29mm/a,respectively.(3 )The experimental