4.7 Article

Exploring sandy vegetation sensitivities to water storage in China's arid and semi-arid regions

期刊

ECOLOGICAL INDICATORS
卷 136, 期 -, 页码 -

出版社

ELSEVIER
DOI: 10.1016/j.ecolind.2022.108711

关键词

The four greater sandy lands; Soil moisture; Terrestrial water storage; Solar-induced chlorophyll fluorescence; Remote sensing; Vegetation-moisture relationship

资金

  1. National Natural Science Foundation of China [41961144019, 42061070]
  2. Inner Mongolia Normal University Graduate Students Research & Innovation Fund [CXJJB21020]

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This study examines the relationship between vegetation growth and water supply in four major sandy lands in China using multi-source satellite observations. The results show the negative impact of land desertification and decreased groundwater levels on the ecological environment, emphasizing the need for continuous vegetation restoration and management. The study also highlights the limitations of vegetation index and the influence of precipitation-driven soil moisture on the vegetation-moisture relationship.
Hulunbuir, Otindag, Horqin and Mu Us are the four greater sandy lands in China. They are typical ecologically fragile areas with limited ability to resist interference and are susceptible to changes in the external environment. With climate change in recent decades, these areas have experienced severe land desertification and decreased groundwater levels. The ecological environment is at risk of further deterioration, and continuous vegetation restoration and management should be adapted to the local climate and maintain the water balance with natural precipitation. This paper combines multi-source satellite observations to explore the relationship between vegetation growth and water supply. The results show four main points. (1) Although the vegetation growth in Otindag and Horqin had degraded before 2010, it improved after 2010. The vegetation growth and soil moisture (SM) of the four sandy lands both generally increased from 2003 to 2016. The SM of the Horqin increased significantly (84% anomaly > 1.4 x 10-2 cm3/cm3). Other than the Hulunbuir, the other sandy lands show a downward trend in terrestrial water storage (TWS), especially the Mu Us declined the most (97% anomaly < -40 mm). (2) Solar-induced chlorophyll fluorescence (SIF) has specific advantages in characterizing the sandy vegetation productivity and water composition changes compared to vegetation index (EVI) or gross primary productivity (GPP). (3) The regional pattern of the vegetation-moisture relationship is mainly affected by the precipitation-driven SM and depends on the types of underlying vegetation functions. (4) Both SM and TWS have approximately one-month persistence in the four sandy lands, especially the Mu Us has the longest persistence (0.94 months and 1.1 months). The persistence in the early period is generally longer than that in the late period, implying that the resilience of water components after the mutation year is stronger than before it. This study provides a scientific basis for the management and restoration of sandy lands. It is recommended that different vegetation restoration and protection strategies should be developed for specific sandy land moisture conditions in arid/semi-arid regions of northern China, which includes the improvement of water use efficiency to maintain soil moisture and the reduction of excessive groundwater uses.

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