Abstract

Outgoing longwave radiation (OLR) is a key factor to study the radiation balance of the earth–atmosphere system. It is of great significance to explore the temporal and spatial variation characteristics over the OLR value in China region and to predict its future variation trend. We investigate the characteristic distribution of OLR value over China and predict its results in time series using the seasonal autoregressive integrated moving average (SARIMA) and long short-term memory (LSTM) methods based on the OLR data by the Atmospheric Infrared Sounder (AIRS). The Mann–Kendall (MK) mutation test was used to analyze the annual average of OLR values in China and the mutation points in the four seasons. The empirical orthogonal function (EOF) is used to decompose the spatial characteristics and temporal variation of OLR values in China. The MK mutation test is used to obtain the mutation points in the three seasons of spring, summer and autumn. The cumulative variance contribution of the four modes obtained by EOF decomposition exceeds 70%, and the variance contribution of the first mode exceeds 50%. The prediction accuracy with SARIMA model is 99% and LSTM algorithm is 97%. The results of spatiotemporal analysis show that the OLR value near the equator is significantly higher than that of the north and south poles and decreases with the increase of latitude; the OLR value in spring, summer and autumn is higher than that in winter. The results of the MK test show that there are many mutation points in autumn, and the location of the mutation points cannot be determined. The mutation points in spring and summer meet the confidence interval; the first mode of EOF decomposition has a meridional structure, and the OLR value is dropped within 18 years as a whole. The spatial characteristics of modes 1 and 3 have obvious changes in the Qinghai-Tibet Plateau and Northeast China. The prediction results show that the prediction accuracy of SARIMA is higher than that of LSTM. Therefore, the results predicted by SARIMA may provide a reference for the study of the radiation balance of the earth–atmosphere system in China.

Highlights

  • In the past ten years, the development of hyperspectral infrared atmospheric detection technology has provided a large amount of observational data for the remote sensing detection of the earth’s atmosphere [1]

  • It can be seen from the distribution of the normal distribution and the kernel density estimation (KDE) that the sum of their areas of change is 1, which basically conforms to the function change of the normal distribution, indicating that the effect of seasonal autoregressive integrated moving average (SARIMA) prediction is good and that it is worthy of reference

  • Using SARIMA and long short-term memory (LSTM) methods to study the characteristic distribution and prediction results of the China regional outgoing longwave radiation (OLR) value, the following conclusions are summarized: (1) The distribution of OLR detected by Atmospheric Infrared Sounder (AIRS) presents a zonal distribution characteristic that is symmetrical to the equator, and the OLR gradually decreases with the increase of latitude

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Summary

Introduction

In the past ten years, the development of hyperspectral infrared atmospheric detection technology has provided a large amount of observational data for the remote sensing detection of the earth’s atmosphere [1]. In the early 1960s, the TIROS satellite, the first-generation experimental meteorological satellite in the United States, began to detect OLR [4]. Until the early 1970s, after the NOAA satellite was equipped with a scanning radiometer (SR), official OLR detection began. The infrared channel of the Advanced Very High Resolution Radiometer (AVHRR) is used for the continuous detection of global OLR [6]. The AIRS carried on the Aqua satellite launched by NASA in May 2002 is a main detection instrument in atmospheric detection, and it has the characteristics of high spectral resolution, many channels and high precision [7]. AIRS can provide more comprehensive and more accurate infrared multispectral hyperspectral data reflecting the state and change characteristics of land, ocean and atmosphere, which is more beneficial to our study of OLR changes

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