Abstract

We report on the development of a machine learning approach to improving sea surface temperature (SST) retrievals based on satellite-based microwave channel measurements at frequencies higher than 23 GHz. The approach uses a deep neural network (DNN) trained using Microwave Integrated Retrieval System physical retrievals as inputs and collocated European Centre for Medium-Range Weather Forecasts analyses for training and validation. The DNN was designed to characterize SST retrieval residual and then used to correct the original retrieval. Evaluation based on one year of independent data showed reduction in retrieval residual standard deviation from 3.22 to 1.80 K in January and 3.02 to 1.92 K in July and reduction in mean residual from 0.30 to 0.08 K in January and 0.61 to 0.22 K in July. Comparisons with multilinear regression and machine learning approaches that used measured brightness temperatures as inputs were significantly less effective in retrieving SST directly, although the DNN used brightness temperature also showed improvements. This indicates that physical retrieval provides valuable information useful in characterizing retrieval residual beyond that of the measured radiances. The DNN approach also effectively removed scan angle dependence of retrieval residuals—an important consideration with cross-track instruments. Sensitivity tests indicated that skill declines with time as time increases from training month, but that skill in the same month, one year later is nearly the same as that of the original training month. This suggests that it may be sufficient to pretrain a stratified model with monthly or seasonal dependence using one full annual cycle, which could then be used in subsequent years with continued good performance.

Highlights

  • DUE to the longer wavelengths at which they operate, microwave sensors have inherent advantages in observing clouds and precipitation dynamics, monitoring land and sea surface properties, and estimating profiles of atmospheric temperature and water vapor under most weather conditions

  • In this study we focus on the core retrieval variable skin temperature, and investigate a means of improving its retrieval over ocean surfaces which, for the purposes of this discussion, we refer to by the commonly used term, sea surface temperature (SST)

  • Liu et al Improvement of MiRS Sea Surface Temperature Retrievals Using a Machine Learning Approach section 2 describes the data sets used and the deep neural network methodology employed for the SST improvement, section 3 discusses the results from several retrieval experiments that were conducted, and section 4 summarizes the work and points to possible future efforts that build on the results shown here

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Summary

Introduction

DUE to the longer wavelengths at which they operate, microwave sensors have inherent advantages in observing clouds and precipitation dynamics, monitoring land and sea surface properties, and estimating profiles of atmospheric temperature and water vapor under most weather conditions. The MiRS uses a one-dimensional variational (1DVAR) algorithm to iteratively find the optimal solution based on minimizing a cost function comprised of two terms: departure of the retrieved state vectors from an a priori climatology background and departure of forward model simulated radiances from the satellite observed radiances [1,2]. The parameters directly retrieved in MiRS include: temperature and water vapor vertical profiles, cloud and precipitation parameter vertical profiles, skin temperature, and emissivity spectrum. These parameters are retrieved simultaneously, and self-consistency among different parameters is maintained via both the background a priori constraints and the use of EOFs. The measurement constraint ensures that the retrieved solution is consistent with the observed radiances.

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