Whether processes in the natural world are dependent or independent
of the scale at which they operate is one of the major issues in
hydrologic science. In this volume, leading hydrologists present
their views on the role of scale effects in hydrologic phenomena
occurring in a range of field settings, from the land surface to
deep fractured rock. Self-contained and thought-provoking chapters
cover both theoretical and applied hydrology. They provide critical
insights into important topics such as general circulation models,
floods, river networks, vadose zone processes, groundwater
transport, and fluid flow through fractured media. This book is
intended as an accessible introduction for graduate students and
researchers to some of the most significant questions and
challenges that will face hydrologic science in the twenty-first
century.
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