The formation of groups of these objects is influenced by changes in the dry adiabatic lapse rate caused by large mountain mass elevations, according to the Massenerhebung effect.
The formation of groups of these objects is influenced by changes in the dry adiabatic lapse rate caused by large mountain mass elevations, according to the Massenerhebung effect. Remote sensing of these objects during geographic surveys primarily uses the attributes of ABG, LAI, and DBH to determine their allometry. When partially destroyed, these objects regenerate in a process called coppicing and the appearance of these objects can be altered by severe wind, as seen in Krummholz formations. These objects can also be damaged externally by frost cracking and sun scalding. Modern analysis divides their development into at least two seral stages and the growth of large types of these signal the end of ecological succession and arrival at a climax community. FTP, name these objects, some common examples of which include the cypress and the oak.  
The formation of groups of these objects is influenced by changes in the dry adiabatic lapse rate caused by large mountain mass elevations, according to the Massenerhebung effect.
trees [reverse prompt on "forests" or "plants" until "regenerate in a process"]