Urban transformation of river landscapes in a global context
Introduction
A half century has passed since scholars convened at the International Symposium on “Man's Role in Changing the Face of the Earth” and cast sharp focus on the reality of human impacts on Earth systems (Thomas, 1956). The question explored at the symposium was: “What has been, and is, happening to the earth's surface as a result of (humans) having been on it for a long time, increasing in numbers and skills unevenly, at different places and times?” (Fejos, 1956). In relation to river landscapes, Strahler (1956) outlined erosion and aggradation as system responses when steady state is upset by human activity, and Leopold (1956) connected changes in sediment yield, driven by land-use changes, to adjustments in river channels. Significant advances have been made along those lines in the years since, with intensified research efforts producing a voluminous literature that documents a range of human impacts on fluvial geomorphology in general, and on river channels in particular (Gregory, 1977a, Gregory, 1987a, Gregory, 1987b, Gregory, this volume).
This paper assesses the progress made on understanding the impacts of urban development on river landscapes, with emphasis on the distribution of such impacts in a global comparative context. Urban development has been a major driver of change across Earth's surface, accelerating in recent decades in response to population growth (Fig. 1). In the third quarter of the twentieth century alone, urban population increased over 100% worldwide and nearly 200% in less developed regions (Gupta, 1984). These rates represent an enormous number of people increasingly living in urban areas. Whereas in 1952, the largest city in the world (New York City) had a population of less than eight million, by 2001, 17 cities had eight million inhabitants, with the largest urban area (Shanghai) exceeding a population of 14 million (United Nations, 2004). As might be expected, the development of infrastructure to accommodate expanding populations would pose formidable demands on river systems (Eyles, 1997, Douglas, 2005), a situation that will likely continue into the future.
This paper synthesizes research results published since 1956 in a range of world areas to answer three questions. First, what have been the impacts of urban development on river systems across Earth's surface? Second, how do these impacts vary with locale and hydroclimatic environment, to the extent indicated by empirical data? Third, how persistent are the impacts at different locales and environments, and what does that persistence indicate about whether rivers can truly adjust to the impacts of urban development? Lastly, the paper concludes by highlighting some challenges for managing urban river systems.
Section snippets
The database
Developing from the work of Gregory, 1977b, Gregory, 1987a, Gregory, 1987b, Gregory, 1995 and Brookes and Gregory (1988), the data for this paper include results from more than 100 published studies that document urbanization impacts on river systems over the past five decades. The investigations selected report hydrologic and sedimentologic process alterations, but emphasize those quantifying morphological change within channels and watersheds (58 studies). The publications are primarily
A conceptual model of change
A first glimpse into how rivers respond to urban development was outlined by Wolman (1967a), where three stages of urbanization were described to have repercussions on river channels: 1) a stable or equilibrium pre-development stage; 2) a period of construction during which bare land is exposed to erosion; and 3) a final stage consisting of a new urban landscape dominated by houses, rooftops, gutters, and sewers. Accompanying the construction phase is an initial increase in sediment production
Sediment production and sediment yield
Ample evidence has indicated a remarkable increase in sediment production once urbanization commences, especially for land surfaces that have been cleared for building but often remain bare for more than one year (Wolman and Schick, 1967). These surfaces can induce erosion rates up to 40,000 times pre-disturbance rates (Harbor, 1999) and produce annual sediment yields on the order of 10,000–50,000 t km− 2 yr− 1 (Piest and Miller, 1975), 60 times more than non-construction areas on average (Chen,
Imperviousness and runoff
Hydrologic changes associated with urbanization have been extensively studied, and results from these studies have clearly shown that urban development leads to larger and more frequent floods (e.g. Leopold, 1968). The main parameters demonstrated to have changed are peak discharge, lag time, flood frequency, and total runoff or water yield (see Poff et al., 2006-this volume, for a sub-continental analysis of runoff responses to urbanization). A sample of the early work from the U.S. and U.K. (
The magnitude, direction, and parameters of change
Morphological adjustments in the river system can be considered in terms of changes in the channel cross-section, reach and planform, and network and basin (Gregory, 1987a, Gregory, 1987b). These changes have been examined for a range of human impacts, including reservoir and dam construction, catchment land use changes, channelization, and urbanization (Gregory, 1987a, Gregory, 1987b, Gregory, this volume). In relation to urban development, such examination can be extended to include a
Managing and restoring urban rivers
Because urbanization is largely an irreversible process that changes Earth surfaces, urbanizing stream channels are necessarily changed through the adjustment process, regardless of how well they can adjust. Managing urban river channels poses particular challenges because, as seen in Fig. 11, most are undergoing adjustments at one stage or another. Thus, how can changing urban rivers be properly managed and potentially restored? A full treatment of this topic is beyond the scope of this paper
Conclusions
Analysis of research results from more than 100 studies (58 morphologic investigations) conducted across the world and published in the English language since 1956 permit answers to the three questions posed in this paper. First, urban development has transformed river landscapes across Earth's surface by changing hydrologic and sedimentologic regimes, causing a range of morphological adjustments. Empirical data have shown that these changes generally accord with the conceptual model outlined
Acknowledgements
The National Geographic Society (Committee for Research and Exploration, Grant No. 7905-05) provided financial support to complete portions of the analysis reported in this paper. Ken Gregory kindly read a draft of this manuscript and offered valuable insights on the urbanization process. Laura Laurencio ably assisted with compiling the database for urbanization studies and with manuscript preparation, including the production of many of the figures. Eresha DeSilva further served as research
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