4.7 Article

Spatial Gap-Filling of GK2A Daily Sea Surface Temperature (SST) around the Korean Peninsula Using Meteorological Data and Regression Residual Kriging (RRK)

期刊

REMOTE SENSING
卷 14, 期 20, 页码 -

出版社

MDPI
DOI: 10.3390/rs14205265

关键词

Geostationary Korea Multi-Purpose Satellite-2A (GK2A); sea surface temperature (SST); regression residual kriging (RRK); spatial gap-filling

资金

  1. Korea Coast Guard, Korea

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This study examined the use of regression residual kriging method to fill the gaps in satellite sea surface temperature images, resulting in improved accuracy. By removing outliers and building a multiple linear regression model, the method was able to generate gap-filled values that closely matched the in situ measurements.
Satellite remote sensing can measure large ocean surface areas, but the infrared-based sea surface temperature (SST) might not be correctly calculated for the pixels under clouds, resulting in missing values in satellite images. Early studies for the gap-free raster maps of satellite SST were based on spatial interpolation using in situ measurements. In this paper, however, an alternative spatial gap-filling method using regression residual kriging (RRK) for the Geostationary Korea Multi-Purpose Satellite-2A (GK2A) daily SST was examined for the seas around the Korean Peninsula. Extreme outliers were first removed from the in situ measurements and the GK2A daily SST images using multi-step statistical procedures. For the pixels on the in situ measurements after the quality control, a multiple linear regression (MLR) model was built using the selected meteorological variables such as daily SST climatology value, specific humidity, and maximum wind speed. The irregular point residuals from the MLR model were transformed into a residual grid by optimized kriging for the residual compensation for the MLR estimation of the null pixels. The RRK residual compensation method improved accuracy considerably compared with the in situ measurements. The gap-filled 18,876 pixels showed the mean bias error (MBE) of -0.001 degrees C, the mean absolute error (MAE) of 0.315 degrees C, the root mean square error (RMSE) of 0.550 degrees C, and the correlation coefficient (CC) of 0.994. The case studies made sure that the gap-filled SST with RRK had very similar values to the in situ measurements to those of the MLR-only method. This was more apparent in the typhoon case: our RRK result was also stable under the influence of typhoons because it can cope with the abrupt changes in marine meteorology.

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