Identification Method for Spring Dust Intensity Levels Based on Multiple Remote Sensing Parameters

Author:

Jiang Qi1ORCID,An Linchang1ORCID,Wang Fei2,Wu Guozhou3,Wen Jianwei4,Li Bin5,Jin Yuchen3,Wei Yapeng6

Affiliation:

1. National Meteorological Centre, Beijing 100081, China

2. CMA Key Laboratory of Cloud-Precipitation Physics and Weather Modification (CPML), CMA Weather Modification Centre (WMC), Beijing 100081, China

3. Inner Mongolia Institute of Meteorological Sciences, Hohhot 010051, China

4. Inner Mongolia Meteorological Information Center, Hohhot 010051, China

5. Inner Mongolia Ecological and Agricultural Meteorological Center, Hohhot 010051, China

6. Jiu Quan Meteorological Administration, Jiuquan 735000, China

Abstract

The advancement of more precise remote sensing inversion technology for dust aerosols has long been a hot topic in the field of the atmospheric environment. In 2023, China experienced 18 dust-related weather events, predominantly in spring. These high-intensity and frequent dust events have attracted considerable attention. However, gridded observation data of dust intensity levels are not collected in current dust monitoring and forecasting operations. Based on the Himawari 9 geostationary satellite data, this study establishes a new method to identify spring dust events. This method integrates the brightness temperature difference method and the multiple infrared dust index, taking into account the response discrepancies of the multiple infrared dust index under various underlying surfaces. Furthermore, by obtaining dynamic background brightness temperature values eight times a day, threshold statistics are applied to analyze the correlation between the infrared difference dust index and ground-observed dust level, so as to establish a satellite-based near-surface dust intensity level identification algorithm. This algorithm aims to improve dust detection accuracy, and to provide more effective gridded observation support for dust forecasting and monitoring operations. The test results indicate that the algorithm can effectively identify the presence or absence of dust, with a misjudgment rate of less than 3%. With regard to dust intensity, the identification of blowing sand and floating dust aligns relatively well with ground-based observations, but notable uncertainties exist in determining a dust intensity of sand-storm level or above. Among these uncertainties, the differences between ground-based observations and satellite identification caused by non-grounded dust in the upper air, and the selection of dust identification thresholds, are two important error sources in the dust identification results of this study.

Funder

the Joint Fund of the National Natural Science Foundation of China

Weather Forecast Application under the Satellite Advancement Plan

2023 Innovation and Development Project of the China Meteorological Administration

Publisher

MDPI AG

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