Demonstration of an efficient interpolation technique of inverse time and distance for Oceansat-2 wind measurements at 6-hourly intervals. Issue 3 (December 2017)

• Record Type: Journal Article
• Authors: Swain, J; Umesh, P A; Murty, A S N
• Is Part Of: International journal of ocean and climate systems. Volume 8:Issue 3(2017)
• Page Start: 101
• Page End: 112
• Publication Date: 2017-12
• Subjects: Oceansat-2 winds -- spatio-temporal interpolation -- satellite winds -- inverse distance and time interpolation -- RAMA buoy; Marine meteorology -- Periodicals; Ocean temperature -- Periodicals; Ocean-atmosphere interaction -- Periodicals; Marine meteorology; Ocean-atmosphere interaction; Ocean temperature; Periodicals; 551.524605
• DOI: 10.1177/1759313117736596
• Languages: English
• ISSNs: 1759-314X

Abstract

Indian Space Research Organization had launched Oceansat-2 on 23 September 2009, and the scatterometer onboard was a space-borne sensor capable of providing ocean surface winds (both speed and direction) over the globe for a mission life of 5 years. The observations of ocean surface winds from such a space-borne sensor are the potential source of data covering the global oceans and useful for driving the state-of-the-art numerical models for simulating ocean state if assimilated/blended with weather prediction model products. In this study, an efficient interpolation technique of inverse distance and time is demonstrated using the Oceansat-2 wind measurements alone for a selected month of June 2010 to generate gridded outputs. As the data are available only along the satellite tracks and there are obvious data gaps due to various other reasons, Oceansat-2 winds were subjected to spatio-temporal interpolation, and 6-hour global wind fields for the global oceans were generated over 1 × 1 degree grid resolution. Such interpolated wind fields can be used to drive the state-of-the-art numerical models to predict/hindcast ocean-state so as to experiment and test the utility/performance of satellite measurements alone in the absence of blended fields. The technique can be tested for other satellites, which provide wind speed as well as direction data. However, the accuracy of input winds is obviously expected to have a perceptible influence on the predicted ocean-state parameters. Here, some attempts are also made to compare the interpolated Oceansat-2 winds with available buoy measurements and it was found that they are reasonably in good agreement with a correlation coefficient of R > 0.8 and mean deviation 1.04 m/s and 25° for wind speed and direction, respectively.