Influences of human activities on sediment discharge from devastated weathered granite hills of southern China: effects of 4-year elimination of human activities

CATENA ◽  
2002 ◽  
Vol 48 (4) ◽  
pp. 217-233 ◽  
Author(s):  
Akitsu Kimoto ◽  
Taro Uchida ◽  
Takahisa Mizuyama ◽  
Li Changhua
Keyword(s):  
Human Activities ◽  
Southern China ◽  
Sediment Discharge ◽  
Weathered Granite ◽  
Influences Of Human Activities

Human impacts on hydrology in the Pantanal wetland of South America

2002 ◽  
Vol 45 (11) ◽  
pp. 35-44 ◽  
Author(s):  
S.K. Hamilton
Keyword(s):  
South America ◽  
Human Activities ◽  
Human Impacts ◽  
Structure And Function ◽  
Natural State ◽  
Ecological Structure ◽  
The Past ◽  
Influences Of Human Activities ◽  
And Function ◽  
Pantanal Wetland

Inundation patterns in the Pantanal remain in a relatively natural state, yet a number of significant human influences have occurred in the past, and there is potential for more severe human impacts as development of the region continues in the future. The objectives of this paper are 1) to briefly review the linkages between hydrology and ecological structure and function in the Pantanal; 2) to review some documented cases of historical influences of human activities on hydrology in the region; and 3) to consider potential future impacts, particularly in regard to the recently proposed navigation project known as the Paraguay-Paraná Waterway (or Hidrovía).

scholarly journals Are Karst Rocky Desertification Areas Affected by Increasing Human Activity in Southern China? An Empirical Analysis from Nighttime Light Data

2019 ◽  
Vol 16 (21) ◽  
pp. 4175
Author(s):  
Shi ◽  
Yang ◽  
Li
Keyword(s):  
Human Activities ◽  
Socioeconomic Development ◽  
Infrared Imaging ◽  
Southern China ◽  
Annual Growth Rate ◽  
Karst Rocky Desertification ◽  
Rocky Desertification ◽  
Nighttime Lights ◽  
Nighttime Light ◽  
Night Lights

Due to remarkable socioeconomic development, an increasing number of karst rocky desertification areas have been severely affected by human activities in southern China. Effectively analyzing human activities in karst rocky desertification areas is a critical prerequisite for managing and restoring areas with tremendous negative impacts from desertification. At present, a timely and accurate way of quantifying the spatiotemporal variations of human activities in karst rocky desertification areas is still lacking. In this communication, we attempted to quantify human activities from the corrected Suomi National Polar-orbiting Partnership (NPP) Visible Infrared Imaging Radiometer Suite (VIIRS) Day/Night Band (DNB) nighttime light composite data from 2012 to 2018 based on statistical analysis. The results show that a significant increase of night lights could be clearly identified during the study period. The total nighttime lights (TL) related to severe karst rocky desertification (S) were particularly concentrated in Guizhou and Yunnan. The nighttime light intensity (LI) related to the S areas in Chongqing was the strongest due to its rapid socioeconomic development. The annual growth rate of nighttime lights (GL) has been slow or even negative in Guangdong because of its various karst rocky desertification restoration programs. This communication could provide an effective approach for quantifying human activities and provide useful information about where prompt attention is required for policy-making on the restoration of the karst rocky desertification areas.

scholarly journals Hydrological Response of Precipitation and Human Activities—A Case Study in the Zuli River Basin, China

2018 ◽  
Author(s):  
Chenlu Huang ◽  
Qinke Yang ◽  
Weidong Huang ◽  
Junlong Zhang ◽  
Yuru Li
Keyword(s):  
River Basin ◽  
Human Activities ◽  
Soil Conservation ◽  
Test Methods ◽  
Sediment Discharge ◽  
Contribution Rate ◽  
Conservation Measures ◽  
Reduction Effect ◽  
The Impact ◽  
Soil Conservation Measures

Precipitation and human activities are two essential forcing dynamics that influence hydrological processes. To investigate those impacts, the Zuli River Basin (ZRB, a typical tributary basin of the Yellow River in China) was chosen to identify the impact of precipitation and human activities on runoff and sediment discharge. A double mass curve (DMC) analysis and the test methods, including accumulated variance analysis, sequential cluster, Lee-Heghnian, and moving t-test methods was utilized to determine the abrupt change point based on data from 1956 to 2015. Correlation formulas and multiple regression methods were used to calculate the runoff and sediment discharge reduction effects of soil conservation measures and to estimate the contribution rate of precipitation and soil conservation measures to runoff and sediment discharge. Our results show that the runoff reduction effect of soil conservation measures (45%) is greater than the sediment discharge reduction effect (32%). Soil conservation measures were the main factor controlling the 74.5% and 75.0% decrease in runoff and sediment discharge, respectively. Additionally, the contribution rate of vegetation measures was higher than that of engineering measures. This study provides scientific strategies for water resource management and soil conservation planning at catchment scale to face future hydrological variability.

scholarly journals Changes in streamflow and sediment discharge and the response to human activities in the middle reaches of the Yellow River

2010 ◽  
Vol 7 (5) ◽  
pp. 6793-6822 ◽  
Author(s):  
P. Gao ◽  
X.-M. Mu ◽  
F. Wang ◽  
R. Li
Keyword(s):  
Human Activities ◽  
Yellow River ◽  
The Yellow River ◽  
Human Intervention ◽  
Sediment Discharge ◽  
Annual Streamflow ◽  
Dominant Position ◽  
Before And After ◽  
Double Mass ◽  
Precipitation Changes

Abstract. The objectives of this work are: (a) to statistically test and quantify the decreasing trends of streamflow and sediment discharge in the middle reaches of the Yellow River in China during 1950–2008, (b) to identify change points or transition years of the decreasing trends, and (c) to diagnose whether the decreasing trends were caused by precipitation changes or human intervention, or both. The results show that significant decreasing trends in annual streamflow and sediment discharge have existed since the late 1950s in the middle reaches of the Yellow River (P=0.01). Change-point analyses further revealed that transition years existed and that abrupt decline in streamflow and sediment discharge began in 1985 and 1981, respectively, in the middle reaches of the Yellow River (P=0.05). Adoption of conservation measures in the 1980s and 1990s corroborates the identified transition years. Double-mass curves of precipitation vs. streamflow (sediment) for the periods before and after the transition year show remarkable decreases in proportionality of streamflow (sediment) generation. Compared with the period before the transition year, cumulative streamflow and cumulative sediment discharge reduced respectively by 17.8% and 28% during 1985–2008, which was caused by human intervention, in the middle reaches of the Yellow River. It is, therefore, concluded that human activities occupied a dominant position and played a major role in the streamflow and sediment discharge reduction in the middle reaches of the Yellow River.

scholarly journals Changes in streamflow and sediment discharge and the response to human activities in the middle reaches of the Yellow River

2011 ◽  
Vol 15 (1) ◽  
pp. 1-10 ◽  
Author(s):  
P. Gao ◽  
X.-M. Mu ◽  
F. Wang ◽  
R. Li
Keyword(s):  
Human Activities ◽  
Yellow River ◽  
Series Data ◽  
The Yellow River ◽  
Sediment Discharge ◽  
Dominant Position ◽  
Precipitation Response ◽  
Before And After ◽  
Double Mass ◽  
Discharge Variation

Abstract. The changes in streamflow and sediment discharge in the middle reaches of the Yellow River are a focus. In this paper, based on the precipitation, streamflow and sediment discharge series data (1950–2008), the streamflow and sediment discharge variation and its impact on precipitation/response to human activities have been analysis. The results show that significant decreasing trends in annual streamflow and sediment discharge have existed since the late 1950s in the middle reaches of the Yellow River (P = 0.01). Change-point analyses further revealed that transition years existed and that abrupt decline in streamflow and sediment discharge began in 1985 and 1981, respectively, in the middle reaches of the Yellow River (P = 0.05). Adoption of conservation measures in the 1980s and 1990s corroborates the identified transition years. Double-mass curves of precipitation vs. streamflow (sediment) for the periods before and after the transition year show remarkable decreases in proportionality of streamflow (sediment) generation. Compared with the period before the transition year, cumulative streamflow and cumulative sediment discharge reduced respectively by 17.8% and 28% during 1985–2008, which was caused by human intervention, in the middle reaches of the Yellow River. It is, therefore, concluded that human activities occupied a dominant position and played a major role in the streamflow and sediment discharge reduction in the middle reaches of the Yellow River.

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