We conducted a detailed analysis of along-trench variations in the flexural bending of the subducting Pacific Plate at the Tonga-Kermadec Trench. Inversions were conducted to obtain best-fitting solutions of trench-axis loadings and variations in the effective elastic plate thickness for the analyzed flexural bending profiles. Results of the analyses revealed significant along-trench variations in plate flexural bending: the trench relief (*W*_{0}) of 1.9 to 5.1 km; trench-axis vertical loading (*V*_{0}) of –0.5×10^{12} to 2.2×10^{12} N/m; axial bending moment (*M*_{0}) of 0.1×10^{17} to 2.2×10^{17} N; effective elastic plate thickness seaward of the outer-rise region (*T*_{e}^{M}) of 20 to 65 km, trench-ward of the outer-rise (*T*_{e}^{m}) of 11 to 33 km, and the transition distance (*X*_{r}) of 20 to 95 km. The Horizon Deep, the second greatest trench depth in the world, has the greatest trench relief (*W*_{0} of 5.1 km) and trench-axis loading (*V*_{0} of 2.2×10^{12} N/m); these values are only slightly smaller than that of the Challenger Deep (*W*_{0} of 5.7 km and *V*_{0} of 2.9×10^{12} N/m) and similar to that of the Sirena Deep (*W*_{0} of 5.2 km and *V*_{0} of 2.0×10^{12} N/m) of the Mariana Trench, suggesting that these deeps are linked to great flexural bending of the subducting plates. Analyses using three independent methods, i.e., the *T*_{e}^{M}/*T*_{e}^{m} inversion, the flexural curvature/yield strength envelope analysis, and the elasto-plastic bending model with normal faults, all yielded similar average *T*_{e} reduction of 28%–36% and average *T*_{e} reduction area *S*_{ΔTe} of 1 195–1 402 km^{2} near the trench axis. The calculated brittle yield zone depth from the flexural curvature/yield strength envelope analysis is also consistent with the distribution of the observed normal faulting earthquakes. Comparisons of the Manila, Philippine, Tonga-Kermadec, Japan, and Mariana Trenches revealed that the average values of *T*_{e}^{M} and *T*_{e}^{m} both in general increase with the subducting plate age.

The rotating fan-beam scatterometer (RFSCAT) is a new type of satellite scatterometer that is proposed approximately 10 a ago. However, similar to other rotating scatterometers, relatively larger wind retrieval errors occur in the nadir and outer regions compared with the middle regions of the swath. For the RFSCAT with the given parameters, a wind direction retrieval accuracy decreases by approximately 9 in the outer regions compared with the middle region. To address this problem, an advanced wind vector retrieval algorithm for the RFSCAT is presented. The new algorithm features an adaptive extension of the range of wind direction for each wind vector cell position across the whole swath according to the distribution histogram of a retrieved wind direction bias. One hundred orbits of Level 2A data are simulated to validate and evaluate the new algorithm. Retrieval experiments demonstrate that the new advanced algorithm can effectively improve the wind direction retrieval accuracy in the nadir and outer regions of the RFSCAT swath. Approximately 1.6 and 9 improvements in the wind direction retrieval are achieved for the wind vector cells located at the nadir and the edge point of the swath, respectively.