Complex anthropogenic interaction on vegetation greening in the Chinese Loess Plateau
Graphical abstract
Introduction
The Loess Plateau in China, a global hotspot of land degradation, was covered by dense vegetation in the ancient past (Chen et al., 2001). But, excessive logging about 3000 years ago in the region has resulted in the present nature of the fragile ecological environment of the Loess Plateau (Xu et al., 2004; Fu and Gulinck, 1994; Kaiser, 2004). In order to restore the status of the ecological environment of the Loess Plateau, the Chinese government has been implementing a series of ecological missions including the Grain for Green (GFG) Project since 1999, one of the largest greening plans in the world (Hua et al., 2016). The main goal of the GFG project is to alleviate the continuous soil and water loss, and desertification (Xu, 2001; Chen et al., 2015; Liang et al., 2019). The GFG Project also greatly supports the ambitious plan of the Chinese government to achieve carbon neutrality by 2060 (Fuhrman et al., 2020).
The most intuitive change after the GFG implementation is that more than 2 × 106 ha of farmland has been converted to grassland and forests (Chen et al., 2015; Deng et al., 2014). Arnon et al. (2014) studies observed that even in the most desertic areas with little vegetation coverage before, there have been varying degrees of greening recently. In 2018 alone, the afforestation area of the Loess Plateau reached 2.83 million ha (Han et al., 2020). A large number of studies thus indisputably shown that the Loess Plateau is becoming significantly greener (e.g., Chen et al., 2019).
Complex factors such as climate, irrigation, urban expansion, land-use management, and various conservation programs are the major decisive factors that cause vegetation changes in the Loess Plateau (Fehmi and Kong, 2012; Lu et al., 2015; Feng et al., 2016; Qu et al., 2018; Spracklen et al., 2012; Fang and Pomeroy, 2010; Raut et al., 2010; Liu et al., 2017; Rochedo et al., 2018). For instance, climatic variables including rainfall, temperature, evapotranspiration, and solar radiation can naturally control the vegetation growth, in which rainfall is considered generally a major driving factor leading to greening (Cai et al., 2020; Shao et al., 2019). Fehmi and Kong (2012) reported that vegetation is generally lush in areas with abundant rainfall. On the other hand, the regional long-term rainfall changes are rather a slow process (Ge et al., 2020). Other than the rainfall, land use management and irrigation-based water supply increase the greening prospects. Easy to grow plants such as shrubs and grasses grow plenty in the Loess Plateau supported by artificial irritation, thus contributing to the partial greening of the Loess Plateau (Raut et al., 2010). However, considering the constant requirement of water supply, and the increasing cost caused by irrigation distance, such models can only be adapted to local conditions (Huang et al., 2005). Snowmelt-induced runoff is another practical irrigation method that significantly promotes the distribution and growth of local vegetation (Bandyopadhyay et al., 2019).
After the launch of the national Chinese projects that aim at improving the ecosystem stability, a widespread increase in vegetation cover was reported in both satellite and field inventory data (Sun et al., 2015). The government also promotes greening by providing “subsidies” to farmers, and making the local eco-tourism industry a main economic growth model, thereby improves the income of local farmers (Wang et al., 2019a). However, with the rapid growth of vegetation, groundwater reserves in the Loess Plateau have decreased significantly, which has resulted in the occurrence of more drought in places where rainfall is scarce. This contradiction is particularly significant in areas of intense greening (Han et al., 2020). Furthermore, soil moisture is an important factor for the normal operation of ecosystem functionalities in arid areas (Liu et al., 2020), which determines the urgent issue of sustainability of the greening process (Jin et al., 2007). The driving factors of greening in the Loess Plateau are therefore very complex.
Dynamic changes in vegetation for any region can be easily carried using multi-phase satellite image difference analysis (Murray et al., 2019). Because of their long archived images, Moderate Resolution Imaging Spectroradiometer (MODIS) based vegetation indexes has been popular to evaluate the spatio-temporal changes in vegetation (Lu et al., 2015; Clark et al., 2010). Normalized Difference Vegetation Index (NDVI), the most widely used product of MODIS, is typically used to assess the changes in vegetation cover (Wu et al., 2018). However, due to the interference of complex spectral properties of soil components, the NDVI results are uncertain (Leeuwen et al., 2006). Therefore, a fractional vegetation cover (FVC) solution based on linear spectral unmixing was proposed (Rundquist, 2002). FVC reflects the intuitive measurement of vegetation cover changes (Wu et al., 2014), which provides the possibility for the study of the relationship between vegetation changes and main control factors.
Multi-period FVC based datasets alone however are inconclusive to support the causes of vegetation changes in the Loess Plateau. While a few studies noticed that rainfall is the most important driver for greening processes in the Loess plateau (e.g., Fehmi and Kong, 2012), some other studies explained the variation in soil type reflects the land use management on vegetation to a certain extent (e.g., Carter, 2002). Jiang et al. (2017a) on the other hand noticed that Gross Domestic Product (GDP) can quantify the relationship between human economic activities and greening. Considering contrasting findings, we therefore assessed the vegetation greening and browning in the Chinese Loess plateau by quantifying the relationship between satellite-derived FVC with rainfall, soil type, and GDP data. This allowed us to assess the dynamic differences in greening and browning since the GFG project in different locations to explore three outstanding issues: (i) quantify the areal percentage of Loess Plateau that has turned to green since the implementation of the GFG project? (ii) understand the regional differences in vegetation cover changes and identify the key location for future greening?, and (iii) assess and quantify the human activities that affect greening and browning. Our study further explores a major knowledge gap of driving factors of greening, supports the sustainable development goal 15 of united nations ‘protect, restore and promote sustainable use of terrestrial ecosystems, sustainably manage forests, combat desertification and halt and reverse land degradation and halt biodiversity loss’ (https://sdgs.un.org/goals).
Section snippets
MODIS and SPOT vegetation products
The MODIS NDVI product types used in this study are from Terra and Aqua satellites, which were downloaded from the publically available Geospatial Data Cloud (http://www.gscloud.cn/sources/index?pid=333&ptitle=MODIS%20%E4%B8%AD%E5%9B%BD%E5%90%88%E6%88%90%E4%BA%A7%E5%93%81&rootid=1). In this work, we chose the MODIS data having low cloud cover, snow, and aerosol to improve the results. The MODIS instrument was launched onboard the Terra satellite in 1999, and the Aqua in 2002. The data was a
Fractional vegetation cover changes in Loess Plateau
Fractional vegetation cover (FVC) analysis shown in Fig. 2 exhibits that about 79.16% of the study area was turned in to greening between 1998 and 2018. FVC generally exhibited upward trends at most places from ~49% in 1998 to 63% in 2018, and the greening cover gradually expanded to the northwest (Fig. 2a–d; Supplementary Fig. 1). Nevertheless, significant differences in average annual FVC were observed between provinces, with the largest increase noticed in Henan Province (average FVC:
Drivers of vegetation greening
Since the GFG implementation, the FVC values of greening areas have increased across a major part of the Loess Plateau, in particular for Shaanxi and Gansu province (Fig. 2, Fig. 3, Fig. 4, Fig. 5), indicating that the Loess plateau was gradually becoming greener in the period of 1998–2018. This is in agreement with the results presented in several other previous studies (Yang et al., 2019; Zhou et al., 2019; Schwärzel et al., 2020). Although, the correlation between vegetation greening and
Conclusions
Our study shows that nearly 80% of the Loess Plateau was turned to green between 1998 and 2018, but the factors driving and restricting greening are complex. At present, greening is most prominent in areas where anthropogenic water gathers in arid areas. Contrarily, vegetation browning is maximum in the areas of urban expansion. This indicates that human activities are the main driving force of rapid vegetation change in the Loess plateau. For the policymakers of the GFG project, a pressing
CRediT authorship contribution statement
Pinglang Kou: Conceptualization, Methodology, Software, Writing – original draft. Qiang Xu: Writing – review & editing. Zhao Jin: Writing – review & editing. Ali P. Yunus: Visualization, Writing – review & editing, Methodology. Xiaobo Luo: Data curation. Minghao Liu: Investigation.
Declaration of competing interest
The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
Acknowledgements
The Major Program of the National Natural Science Foundation of China (Grant No. 41790445), the National Natural Science Foundation of China (41790444), the National Natural Science Foundation of China (41871226), and the Key Program of National Natural Science Foundation of China (Grant No. 41630640) supported this research. Acknowledgement for the soil type classification and average annual rainfall data support from “National Earth System Science Data Center, National Science & Technology
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