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Responses of aeolian desertification to a range of climate scenarios in China
Wang X. M.; Hua, T.; Ma, W. Y.
Source PublicationSolid Earth
2016
Volume7
Issue3
Pages959-964
Keywordkarst rocky desertification wind erosion global desertification colorado plateau semiarid china north china vegetation desert impact dust
AbstractAeolian desertification plays an important role in earth-system processes and ecosystems, and has the potential to greatly impact global food production. The occurrence of aeolian desertification has traditionally been attributed to increases in wind speed and temperature and decreases in rainfall. In this study, by integrating the aeolian desertification monitoring data and climate and vegetation indices, we found that although aeolian desertification is influenced by complex climate patterns and human activities, increases in rainfall and temperature and decreases in wind speed may not be the key factors of aeolian desertification controls in some regions of China. Our results show that, even when modern technical approaches are used, different approaches to desertification need to be applied to account for regional differences. These results have important implications for future policy decisions on how best to combat desertification.
Indexed BySCI
Language英语
ISSN1869-9510
DOI10.5194/se-7-959-2016
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Document TypeSCI/SSCI论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/43285
Collection历年回溯文献
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GB/T 7714
Wang X. M.,Hua, T.,Ma, W. Y.. Responses of aeolian desertification to a range of climate scenarios in China. 2016.
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