Titlebook: Landscape and Ecosystem Diversity, Dynamics and Management in the Yellow River Source Zone; Gary John Brierley,Xilai Li,Jay Gao Book 2016

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Hydrology of the Yellow River Source Zone, same time, environmental deterioration, soil erosion, land desertification, shrinkage of wetlands and lakes, glacier ablation, deterioration of grasslands, rodent infestation, degradation of biological diversity and other environmental and ecological problems have arisen. As a result, the regional

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Hillslope Stability in the Yellow River Source Zone,llow River. Steep ravines and gullies are restricted to mountain ranges at the northern and southern margins. This contrasts starkly with the deeply dissected landscapes at the eastern margin of the Qinghai–Tibet Plateau. Although the high elevation induces low mean annual temperatures, diurnal temp

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Range-Of-Motion

,Modelling Vegetation–Erosion Dynamics in the Mugetan Desert, Yellow River Source Zone,the geomorphic tendency of desertification areas. This chapter presents a dynamic model of vegetation and aeolian sand erosion and its application in the Mugetan desertification area in the source region of Yellow River. Vegetation–erosion dynamics are assessed to develop a coupling equation of vege

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Wetland Ecosystems of the Yellow River Source Zone,cosystems in the source zone of the Yellow River. Field surveys (2010–2014) and interpretations of remote sensing images are used to provide insights into the distribution of wetlands in this region and associated notions of landscape connectivity. Ruoergai Swamp (Zoige) at the eastern margin of the

Introduction

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Fish of the Upper Yellow River,he Cobitidae (loach family). These species have adapted and evolved over millions of years to the highland environment. They play significant roles in the trophic web of freshwater communities. This chapter presents an overview of fish from the Upper Yellow River. The chapter is structured as follow

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