4.7 Article

Spatio-temporal trends of dust emissions triggered by desertification in China

期刊

CATENA
卷 200, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.catena.2021.105160

关键词

Dust emission; Desertification; Gobi desert; China

资金

  1. National Natural Science Foundation of China [41930640, 41771012]
  2. National Key Research and Development Program of China [2016YFA0601900]
  3. Key Frontier Program of Chinese Academy of Sciences [QYZDJ-SSWDQC043]

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The study on potential dust emissions from severe aeolian desertified lands and Gobi desert surfaces in China revealed significant spatial and temporal variations, with both landscapes being key sources of dust emissions. The contribution of the Gobi desert surfaces to dust emissions has decreased from the 1980s to the present, while the potential dust emissions from both types of landscapes have decreased significantly after 2000 compared to the 1970s. Despite model simulations suggesting higher dust emissions, actual potential dust emissions in China are lower than expected.
The spatial and temporal trends of potential dust emissions from severe aeolian desertified lands and Gobi desert surfaces in China were investigated based on field sample collections, wind tunnel experiments, and historical wind records. The results showed that aeolian desertified lands and Gobi desert surfaces are both key landscapes for dust emissions. The dust emission rate in Gobi deserts was approximately 19% of what originated from desertified lands at the beginning of the 1970s but this ratio increased to 26% in 2015. Considering temporal variations of dust emission over aeolian desertified lands and the Gobi desert surfaces, from the 1980s to the present, the contribution of the Gobi desert surfaces on dust emissions decreased from 71% to 31% of that originating in desertified lands. From the 1970s to 2015, the average amounts of PM2.5 (particulate matter with diameter less than 2.5 mu m), PM5, PM10, and PM50 emitted from desertified lands are 17.6, 29.4, 39.6, and 65.2 Tg yr(-1), while that of PM5, PM10, and PM50 emitted from the Gobi desert surfaces are 18.4, 26.5, 40.4 Tg yr(-1), respectively. Compared with that in the 1970s, potential dust emissions after 2000 from desertified lands and the Gobi desert surfaces decreased by 75% and 71%, respectively. In addition, the wind tunnel experiment results and statistics indicate that the potential dust emissions in China are far lower than that of model simulations. There are significant spatio-temporal variations in the potential dust aerosol source areas and intensities of dust emissions in China over the past decades.

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