ra dio occultation (RO) refractivity with WRF 3DVAR. For sim plic ity, in the past GPS RO
refractivity was of ten as sim i lated us ing a lo cal ob ser va tion op er a tor with the as sump
tion that the GPS RO ob ser va tion was rep re sen ta tive of a model lo cal point. Such an op
er a tor did not take into ac count the ef fects of hor i zon tal inhomogeneity on the de rived
GPS RO refractivity. In or der to more ac cu rately model the observables, Sokolovskiy et …