A211-0003
Retrieving Water Vapor in the Marine Boundary Layer using GNSS Radio Occultation and Passive Microwave Radiance Sounding
Abstract:
We attempt a retrieval of water vapor in the BL by fusing RO data with collocated microwave data, taking a systematic approach wherein strong assumption are gradually relaxed. First, a well-mixed moist, unsaturated adiabat with two degrees of freedom in the BL is assumed. The method is found to be robust and convergent but inefficient and uninformative: inefficient because the independent coordinates of the microwave and RO differ, imprecise because a well-mixed adiabat washes out interesting information. Second, a constant temperature lapse rate is assumed and high vertical resolution water vapor is retrieved using a strong reglurizer. This method shows immense promise: it can retrieve water vapor anomalies on vertical scales as small as 200 m with near-perfect accuracy; however, this method is unstable. In half of the cases, steep and unrealistic water vapor gradients are retrieved erroneously.
Our ongoing investigation into fusing passive microwave with GNSS RO will be presented.