In this study, we will present an SSM/I cross-calibration algorithm using a simultaneous conical overpassing (SCO) data set from a pair of DMSP satellites. The double difference method is used to calibrate all the SSM/I data to the F13 satellite which is used as a reference sensor. This cross-calibration algorithm has improved the consistency of the monthly SDR's time series from different SSM/I sensors. Total precipitable water biases between sensors are reduced by 75% over the global ocean and 20% over the tropical ocean, respectively. The TPW climate trend is 1.59% per decade (or 0.34 mm decade-1) for the global ocean and 1.39% per decade (or 0.63 mm decade-1) for the tropical ocean, indicating a related trend decrease of 38% and 54% respectively from the uncalibrated SDRs.
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