Soil moisture restricts the ecological restoration in karst, but studies on soil moisture storage (SMS) in karst are lacking. Thus, this study analyzed the characteristics of SMS in the karst area of China (K) and revealed the relationships of SMS with its influencing factors. The main results are as follows: (1) Average SMS in K is higher than that in the non-karst area (N). However, when SMS is below the thresholds 12 mm (0-7 cm) and 563.6 mm (0-289 cm), SMS in K is lower than that in N. (2) SMS in K experienced a decreasing trend in 1979-2017. (3) SMSs of K and N increase with precipitation class, but the SMS in K is more sensitive to precipitation. (4) SMSs of Agriculture and Forest landcovers in K significantly reduced in 1979-2017. Ov...
Soil moisture scarcity has become the major limiting factor of vegetation restoration in the Loess P...
Drought and shortages of soil water are becoming extremely severe due to global climate change. A be...
Temporal stability of spatial distributions of soil moisture are usually observed after repeated sur...
Soil moisture restricts the ecological restoration in karst, but studies on soil moisture storage (S...
Soil hydrological characteristics are influenced by factors such as parent rock weathering, human ac...
The purpose of this study was to explore the effects of different vegetation restoration types on so...
The Qinghai–Tibet Plateau (QTP) has an important function in ensuring the water ecological security ...
The special above-ground and underground dual structure in the karst area makes the capacity of surf...
Abstract Background Karst areas in southwestern China exhibit ecological degradation in the form of ...
In this paper, we use GLDAS (Global Land Data Assimilation System) to analyze the effects of air tem...
Understanding how soil moisture changes under different land uses is essential to ensure effective u...
Soil-water storage (SWS) is an important indicator of the sustainability of regional water resources...
The effects of drought on plants have been extensively documented in water-limited systems. However,...
International audienceKarst rocky desertification is a process of land degradation involving serious ...
Drought is one of the most important but least understood issues in global environmental changes. De...
Soil moisture scarcity has become the major limiting factor of vegetation restoration in the Loess P...
Drought and shortages of soil water are becoming extremely severe due to global climate change. A be...
Temporal stability of spatial distributions of soil moisture are usually observed after repeated sur...
Soil moisture restricts the ecological restoration in karst, but studies on soil moisture storage (S...
Soil hydrological characteristics are influenced by factors such as parent rock weathering, human ac...
The purpose of this study was to explore the effects of different vegetation restoration types on so...
The Qinghai–Tibet Plateau (QTP) has an important function in ensuring the water ecological security ...
The special above-ground and underground dual structure in the karst area makes the capacity of surf...
Abstract Background Karst areas in southwestern China exhibit ecological degradation in the form of ...
In this paper, we use GLDAS (Global Land Data Assimilation System) to analyze the effects of air tem...
Understanding how soil moisture changes under different land uses is essential to ensure effective u...
Soil-water storage (SWS) is an important indicator of the sustainability of regional water resources...
The effects of drought on plants have been extensively documented in water-limited systems. However,...
International audienceKarst rocky desertification is a process of land degradation involving serious ...
Drought is one of the most important but least understood issues in global environmental changes. De...
Soil moisture scarcity has become the major limiting factor of vegetation restoration in the Loess P...
Drought and shortages of soil water are becoming extremely severe due to global climate change. A be...
Temporal stability of spatial distributions of soil moisture are usually observed after repeated sur...