Ground-based radar reflectivity mosaic of mei-yu precipitation systems over the Yangtze River–Huaihe River basins

2016 ◽  
Vol 33 (11) ◽  
pp. 1285-1296
Author(s):  
Yali Luo ◽  
Weimiao Qian ◽  
Yu Gong ◽  
Hongyan Wang ◽  
Da-Lin Zhang

<em>Abstract</em>.—Bighead Carp <em>Hypophthalmichthys nobilis </em>and Silver Carp <em>H. molitrix </em>are native in the Yangtze River and extremely important economically and culturally as food fishes; however, the two species have declined due to overfishing and anthropogenic modifications to hydrology and water quality. Bighead Carp and Silver Carp were imported to North America in the early 1970s, escaped confinement, and have now become undesirable and problematic invasive species. The two carps have become the most abundant fish species in many portions of their invaded range, which continues to expand. We compare the biology, status, and management of these species between their natal range in the Yangtze River and their invaded habitats of the Mississippi River basin.


Soil Research ◽  
2020 ◽  
Vol 58 (6) ◽  
pp. 540
Author(s):  
Yan Yang ◽  
Qiuan Zhu ◽  
Jinxun Liu ◽  
Mingxu Li ◽  
Minshu Yuan ◽  
...  

Soil erosion by water affects soil organic carbon (SOC) migration and distribution, which are important processes for defining ecosystem carbon sources and sinks. Little has been done to quantify soil carbon erosion in the three major basins in China, the Yangtze River, Yellow River and Pearl River Basins, which contain the most eroded areas. This research attempts to quantify the lateral movement of SOC based on spatial and temporal patterns of water erosion rates derived from an empirical Unit Stream Power Erosion Deposition Model (USPED) model. The water erosion rates simulated by the USPED model agreed reasonably with observations (R2 = 0.43, P &lt; 0.01). We showed that regional water erosion ranged within 23.3–50 Mg ha–1 year–1 during 1992–2013, inducing the lateral redistribution of SOC caused by erosion in the range of 0.027–0.049 Mg C ha–1 year–1, and that caused by deposition of 0.0079–0.015 Mg C ha–1 year–1, in the three basins. The total eroded SOC was 0.006, 0.002 and 0.001 Pg year–1 in the Yangtze River, Yellow River and Pearl River Basins respectively. The net eroded SOC in the three basins was ~0.0075 Pg C year–1. Overall, the annual average redistributed SOC rate caused by erosion was greater than that caused by deposition, and the SOC loss in the Yangtze River Basin was greatest among the three basins. Our study suggests that considering both processes of erosion and deposition – as well as effects of topography, rainfall, land use types and their interactions – on these processes are important to understand SOC redistribution caused by water erosion.


2020 ◽  
Vol 12 (17) ◽  
pp. 7085
Author(s):  
Junfeng Zhang ◽  
Anlu Zhang ◽  
Min Song

The ecological benefit of cultivated land is the non-market value or ecological service value created by cultivated land protection. Based on the trinity concept of comprehensive protection of quantity, quality, and ecology of cultivated land, this study calculates the ecological benefits of cultivated land protection in the Yangtze River Economic Belt. Through the theory of ecological supply and demand balance, the study estimated the ecological benefit spillover of cultivated land protection in the basin. The amounts and paths of ecological financial transfers for cultivated land are then examined by balancing the protection responsibilities and financial power of cultivated land. We found that overall the ecological benefits of cultivated land protection in the Yangtze River Economic Belt increased, reaching 773.224 billion RMB in 2017. Therein the upper, middle, and lower reaches compose 20.81%, 53.89%, and 25.30% of the ecological benefits. There are significant differences in the ecological benefits, respectively. There are significant differences in the ecological benefits and their variations of cultivated land within the River Basins. The ecological benefits of cultivated land in the Yangtze River Economic Belt demonstrated spatial spillovers within and between the upper, middle, and lower reaches. The middle reaches of the economic belt are the main ecological surplus areas of cultivated land. The ecological deficit areas of cultivated land are mainly distributed in the lower reaches. The spillover effect of the ecological benefits is evident between provinces. The increase of regional economy and ecological compensation policy for cultivated land can effectively stimulate the ecological benefits whereas the pressure of cultivated land protection and power spillovers are adverse to cultivated land ecological protection. The vertical and horizontal fiscal transfers in 2017 respectively amounted to 230.14 billion RMB and 27.24 billion RMB. Particularly, the upper, middle, and lower reaches received 13.07%, 58.41% and 28.52% of the ecological fiscal transfers, respectively. It is important to strengthen spatial spillovers and improve the horizontal and vertical ecological fiscal transfers for protecting ecology of cultivated land.


Author(s):  
Liu Liu ◽  
Zongxue Xu ◽  
Rong Li ◽  
Youzhi Wang

Climate change is a global issue that draws widespread attention from the international society. As an important component of the climate system, the water cycle is directly affected by climate change. Thus, it is very important to study the influences of climate change on the basin water cycle with respect to maintenance of healthy rivers, sustainable use of water resources, and sustainable socioeconomic development in the basin. In this study, by assessing the suitability of multiple General Circulation Models (GCMs) recommended by the Intergovernmental Panel on Climate Change, Statistical Downscaling Model (SDSM) and Automated Statistical Downscaling model (ASD) were used to generate future climate change scenarios. These were then used to drive distributed hydrologic models (Variable Infiltration Capacity, Soil and Water Assessment Tool) for hydrological simulation of the Yangtze River and Yellow River basins, thereby quantifying the effects of climate change on the basin water cycle. The results showed that suitability assessment adopted in this study could effectively reduce the uncertainty of GCMs, and that statistical downscaling was able to greatly improve precipitation and temperature outputs in global climate mode. Compared to a baseline period (1961&ndash;1990), projected future periods (2046&ndash;2065 and 2081&ndash;2100) had a slightly decreasing tendency of runoff in the lower reaches of the Yangtze River basin. In particular, a significant increase in runoff was observed during flood seasons in the southeast part. However, runoff of the upper Yellow River basin decreased continuously. The results provide a reference for studying climate change in major river basins of China.


2019 ◽  
Vol 39 (3) ◽  
Author(s):  
孔令桥 KONG Lingqiao ◽  
王雅晴 WANG Yaqing ◽  
郑华 ZHENG Hua ◽  
肖燚 XIAO Yi ◽  
徐卫华 XU Weihua ◽  
...  

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