Potential wind erosion rate response to climate and land-use changes in the watershed of the Ningxia-Inner Mongolia reach of the Yellow River, China, 1986-2013

被引:42
作者
Du, Heqiang [1 ]
Wang, Tao [1 ]
Xue, Xian [1 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Desert & Desertificat, Lanzhou, Gansu, Peoples R China
关键词
climate change; land-use change; potential wind erosion rate; wind erosion models; PARKS CENTRAL SYSTEM; LAS BATUECAS-SIERRA; SOIL-MOISTURE; SIMPLE-MODEL; DYNAMICS; RISK; PREDICTION; SALTATION; FRANCIA; SCALE;
D O I
10.1002/esp.4146
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Climate and land-use changes could strongly affect wind erosion and in turn cause a series of environmental problems. Thus, the objective of this study was to assess potential wind erosion rate (PWER) response to climate and land-use changes in the watershed of the Ningxia-Inner Mongolia Reach of the Yellow River (NIMRYR), China. The watershed of NIMRYR suffers from serious wind erosion hazards, and over recent decades, wind erosion intensity and distribution has changed, following climate and land-use changes. To understand these processes in the NIMRYR watershed, the Integrated Wind Erosion Modelling System (IWEMS) and the Revised Wind Erosion Equation (RWEQ) were used to calculate the PWER under different climate conditions and land-use scenarios, and to assess the influences of climate and land-use changes on the PWER. The results show the PWER in the whole watershed had a significant declining trend from 1986 to 2013. The results of the relationship among PWER, climate change, and land-use changes showed that climate change was the dominant control on the PWER change in this watershed. Compared to the period 1986-1995, the average PWER decreased 23.32% and 64.98% as a result of climate change in the periods 1996-2005 and 2006-2013, respectively. In contrast with climate change, the effects of land-use changes on the average PWER were much lower, and represented a change in PWER of less than 3.3% across the whole watershed. The study method we used could provide some valuable reference for wind erosion modelling, and the research results should help climate and land-use researchers to develop strategies to reduce wind erosion. Copyright (c) 2017 John Wiley & Sons, Ltd.
引用
收藏
页码:1923 / 1937
页数:15
相关论文
共 62 条
[1]  
Allen R. G., 1998, FAO Irrigation and Drainage Paper
[2]  
[Anonymous], 1997, WORLD ATLAS DESERTIF
[3]   Sand dune mobility under climate change in the Kalahari and Australian deserts [J].
Ashkenazy, Y. ;
Yizhaq, H. ;
Tsoar, Haim .
CLIMATIC CHANGE, 2012, 112 (3-4) :901-923
[4]  
Baumhardt RL., 2003, ENCY WATER SCI
[5]  
Boardman J., 2006, Soil Erosion in Europe Editors, DOI DOI 10.1002/0470859202
[6]   Validation of WEQ, RWEQ and WEPS wind erosion for different arable land management systems in the Argentinean Pampas [J].
Buschiazzo, Daniel E. ;
Zobeck, Ted M. .
EARTH SURFACE PROCESSES AND LANDFORMS, 2008, 33 (12) :1839-1850
[7]   Geomorphologic approach for modelling the surface features of arid environments in a model of dust emissions: application to the Sahara desert [J].
Callot, Y ;
Marticorena, B ;
Bergametti, G .
GEODINAMICA ACTA, 2000, 13 (05) :245-270
[8]   Assessment of wind and water erosion risk in the watershed of the Ningxia-Inner Mongolia Reach of the Yellow River, China [J].
Du, Heqiang ;
Dou, Shentang ;
Deng, Xiaohong ;
Xue, Xian ;
Wang, Tao .
ECOLOGICAL INDICATORS, 2016, 67 :117-131
[9]   Assessment of wind-erosion risk in the watershed of the Ningxia-Inner Mongolia Reach of the Yellow River, northern China [J].
Du, Heqiang ;
Xue, Xian ;
Wang, Tao ;
Deng, Xiaohong .
AEOLIAN RESEARCH, 2015, 17 :193-204
[10]   Estimation of the quantity of aeolian saltation sediments blown into the Yellow River from the Ulanbuh Desert, China [J].
Du, HeQiang ;
Xue, Xian ;
Wang, Tao .
JOURNAL OF ARID LAND, 2014, 6 (02) :205-218