Time-Lagged Correlation between Soil Moisture and Intra-Annual Dynamics of Vegetation on the Mongolian Plateau

• Published in: Remote sensing (Basel, Switzerland) Vol. 13; no. 8; p. 1527
• Main Authors: Bao, Yongbin, Zhang, Jiquan
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 15.04.2021
• Subjects: arid and semiarid regions; Arid regions; Arid zones; Browning; Central Asia; Climate change; Coniferous forests; Correlation; Data assimilation; Datasets; Deserts; different vegetation types; Forests; Grasslands; Investigations; Moisture content; normalized difference vegetation index; Normalized difference vegetative index; phenology period; Plant growth; Precipitation; R&D; Remote sensing; Research & development; Semi arid areas; Semiarid zones; Soil dynamics; Soil layers; Soil moisture; soil water; soil water content; Terrestrial ecosystems; Vegetation; Vegetation index; Water content; Water resources; Northern Hemisphere; China; Inner Mongolia China; Central Asia
• DOI: 10.3390/rs13081527
• ISSN: 2072-4292

Soil moisture is a reliable water resource for plant growth in arid and semi-arid regions. Characterizing the interaction between soil moisture and vegetation is important for assessing the sustainability of terrestrial ecosystems. This study explores the spatiotemporal characteristics of four soil moisture layers (layer 1: 0–7 cm, layer 2: 7–28 cm, layer 3: 28–100 cm, and layer 4: 100–289 cm) and the time-lagged correlation with the normalized difference vegetation index (NDVI) for different vegetation types on an intra-annual scale on the Mongolian Plateau (MP). The most significant results indicated that: (1) the four layers of soil moisture can be roughly divided into rapid change (layers 1 and 2), active (layer 3), and stable (layer 4) layers. The soil moisture content in the different vegetation regions was forest > grassland > desert vegetation. (2) The soil moisture in layer 1 showed the strongest positive correlation with NDVI in the whole area; meanwhile, the soil moisture of layers 2 and 3 showed the strongest negative correlation with the NDVI mainly in grassland and desert, and layer 4 showed the strongest negative correlation with the NDVI in the forest. (3) Mutual responses of NDVI and deep layer soil moisture required a longer time compared with the shallow layer. In the annual time scale, the NDVI was affected by the change in soil moisture in most of the study area, except for coniferous forest and desert vegetation regions. (4) Under the different stages of vegetation change, the soil moisture changes advance than NDVI about 3 months during the greening stage, while the NDVI changes advance than soil moisture by 0.5 months during the browning stage. Regardless of the stage, changes in soil moisture are initiated from the shallow layer and advance to the deep layer. The results of this study provide deep insight into the relationship between soil moisture and vegetation in arid and semi-arid regions.