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measurements within the assumed range of error. The major improvements compared to L04 , which will be presented in this paper, are the following: Instead of using only zenith observations from the MWP, we now additionally include elevation scanning measurements, which can increase the accuracy of the temperature profile significantly in the BL ( Crewell and Löhnert 2007 ). We now employ the well-established CloudNet target classification scheme ( Hogan and O’Connor 2004 ) developed at the University
measurements within the assumed range of error. The major improvements compared to L04 , which will be presented in this paper, are the following: Instead of using only zenith observations from the MWP, we now additionally include elevation scanning measurements, which can increase the accuracy of the temperature profile significantly in the BL ( Crewell and Löhnert 2007 ). We now employ the well-established CloudNet target classification scheme ( Hogan and O’Connor 2004 ) developed at the University
