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A new method of constructing a sea level pressure field from satellite microwave scatterometer measurements is presented.It is based on variational assimilation in combination with a regularization method using geostrophic vorticity to construct a sea level pressure field from scatterometer data that are given in this paper,which offers a new idea for the application of scatterometer measurements.Firstly,the geostrophic vorticity from the scatterometer data is computed to construct the observation field,and the vorticity field in an area and the sea level pressure on the borders are assimilated.Secondly,the gradient of sea level pressure(semi-norm) is used as the stable functional to educe the adjoint system,the adjoint boundary condition and the gradient of the cost functional in which a weight parameter is introduced for the harmony of the system and the Tikhonov regularization techniques in inverse problem are used to overcome the ill-posedness of the assimilation.Finally,the iteration method of the sea level pressure field is developed.
A new method of constructing a sea level pressure field from satellite microwave scatterometer measurements is presented. It is based on variational assimilation in combination with a regularization method using geostrophic vorticity to construct a sea level pressure field from scatterometer data that are given in this paper, which offers a new idea for the application of scatterometer measurements. Firstly, the geostrophic vorticity from the scatterometer data is computed to construct the observation field, and the vorticity field in an area and the sea level pressure on the borders are assimilated. Secondarily, the gradient of sea level pressure (semi-norm) is used as the stable functional to educe the adjoint system, the adjoint boundary condition and the gradient of the cost functional in which a weight parameter is introduced for the harmony of the system and the Tikhonov regularization techniques in inverse problem are used to overcome the ill-posedness of the assimilation .Finally, the iterat ion method of the sea level pressure field is developed.