This book is a printed edition of the Special Issue "Hillslope and Watershed Hydrology" that was published in Water

Hillslope and Watershed Hydrology.

A complete guide to the behavior of water on graded land Hillslope Hydrology provides a comprehensive introduction to the behavior of water on a slope. Describing the fates of precipitation, the mechanics of runoff, and the calculations involved in assessment, this book clarifies the complex interplay of soils, sediment, subsurface flow, overland flow, saturation, erosion, and more. An ideal resource for graduate students of Earth science, environmental science, civil engineering, architecture, landscape management, and related fields, this informative guide provides the essential information needed to work effectively with graded land or predict outcomes of precipitation.

An comprehensive working reference, Watershed Hydrology begins with an overview of the hydrologic cycle and examines the basic concepts of storage in that cycle. The well-organized chapters cover topics such as: water and energy, storage of water in the atmosphere, water in the vegetative zone, water in the terrasphere (soil), water in the hydrosphere, and watershed management.

This new edition is a major revision of the popular introductory reference on hydrology and watershed management principles, methods, and applications. The book's content and scope have been improved and condensed, with updated chapters on the management of forest, woodland, rangeland, agricultural urban, and mixed land use watersheds. Case studies and examples throughout the book show practical ways to use web sites and the Internet to acquire data, update methods and models, and apply the latest technologies to issues of land and water use and climate variability and change.

Hydrology is the branch of science that is concerned with the movement and management of water on the surface of Earth, beneath the surface of Earth, as well as in the atmosphere. Hillslopes make up the flanks of valleys and the margins of eroding uplands. Hillslope hydrology is a scientific study to understand the hillslope runoff processes and the contribution of groundwater to storm runoff. Such hydrologic organization brings in distinct characteristics in soil and vegetation of hilltops, valleys and between sunny and shady slopes. The topographic gradients present on the hillslopes drive water, sediments and biogeochemical fluxes down the hillslopes. Hydrologic processes are traditionally studied at hillslope-to-catchment scales (tens of meters to kilometers). An important area of study in this field is the interplay of sediments, subsurface flow, soil erosion and overland flow. This book provides significant information of this discipline to help develop a good understanding of hillslope hydrology and its related fields. From theories to research to practical applications, case studies related to all contemporary topics of relevance to this field have been included herein. This book will help new researchers by foregrounding their knowledge in this branch.

The book provides a comprehensive insight into watersheds and modeling of the hydrological processes in the watersheds. It covers the concepts of watershed hydrology and watershed management in depth. The basic types, of soil erosion and its measurement and estimation of runoff and soil loss from the small and large watersheds are discussed. Recent advances in the watershed management like the application of remote sensing and GIS and hydrological models are a part of the book. The book serve as a guide for professional and competitive examinations for undergraduate students of Agriculture and Agricultural Engineering and graduate students of Soil Science, Soil and Water Engineering, Agricultural Physics, Hydrology and Watershed Management.

This book examines one of the most important and complex of the world's tropical rainforest regions: the greater Panama Canal Watershed. The Rio Chagres is the primary water source for operating the Canal, and supplies potable water for municipal use and electricity generation, but science has left this important national resource largely unstudied. The text promotes understanding of the physical and ecological components of an isolated and largely pristine tropical rainforest.

Landslides are caused by a failure of the mechanical balance within hillslopes. This balance is governed by two coupled physical processes: hydrological or subsurface flow and stress. The stabilizing strength of hillslope materials depends on effective stress, which is diminished by rainfall. This book presents a cutting-edge quantitative approach to understanding hydro-mechanical processes across variably saturated hillslope environments and to the study and prediction of rainfall-induced landslides. Topics covered include historic synthesis of hillslope geomorphology and hydrology, total and effective stress distributions, critical reviews of shear strength of hillslope materials and different bases for stability analysis. Exercises and homework problems are provided for students to engage with the theory in practice. This is an invaluable resource for graduate students and researchers in hydrology, geomorphology, engineering geology, geotechnical engineering and geomechanics and for professionals in the fields of civil and environmental engineering and natural hazard analysis.