2026-09-20T08:53:54Z https://www.ideals.illinois.edu/oai-pmh

oai:www.ideals.illinois.edu:2142/16722 2023-07-10 col_2142_5131 col_2142_14770 com_2142_5130 com_2142_3518 com_2142_234

Cai, Ximing Roug��, Charles J. 2010-08-20T17:55:57Z 2010-08-20T17:55:57Z 2010-08-20T17:55:57Z 2010-08 Urban and economic development and climate change have made the non-stationarity of stream flow records an emerging phenomenon in hydrology. This thesis studies the systematic shifts in stream flow that have been observed in urban, suburban and agricultural watersheds in and around the Greater Chicago area. A novel statistical method, the Procedure for Change Pattern and Signi ficance (PCPS), is developed to detect non-stationarity and identify the timing and duration of these shifts in hydrologic records. This method uses the rank correlations of the Mann-Kendall statistics to extract information that can be interpreted to identify the timing and duration of a detected shift, while it also adopts the Mann-Kendall test to determine whether the change is statistically signi ficant. It is also shown that incorporating the aspects of timing, duration and signi ficance in a consistent analytical framework enables the issue of serial correlation to be tackled better. The proposed statistical framework is associated with conceptual modeling tools to understand how adaptive human responses to urbanization mitigate and sometimes even o ffset the e ffects of land-use change in a large urban area, such as the Greater Chicago area. Results of PCPS, along with an analysis of the recession process, show that while impervious surfaces increase flooding, stormwater management facilities mitigate or even counter this impact over a wide range of scales. On the other hand, an urban water balance shows that low flows have increased since the impacts of e ffluent discharges, pipe leakage and garden irrigation from municipal water systems using water from Lake Michigan outweigh the reduction of basefl ow due to impervious surfaces. In addition, the increasing trend of the mean flow in the area can be explained by the combined impacts of water withdrawals from Lake Michigan, land-use change and climatic variability. Finally, it is found that a step increase in rainfall coincides with a step increases in streamfl ow around 1970. Thus, PCPS detects the impacts of climate and urbanization on stream flow throughout the Greater Chicago area. Item withdrawn by Mark Zulauf (zulauf@illinois.edu) on 2010-07-19T20:34:04Z Item was in collections: University of Illinois Theses & Dissertations (ID: 1) No. of bitstreams: 2 rouge_charles_latex_code.zip: 3121461 bytes, checksum: 94c43d35bd7d507a0ff7f141d183843c (MD5) rouge_charles.pdf: 4243925 bytes, checksum: fef8a6fb8a1955519ddf6050ccb94d12 (MD5) Made available in DSpace on 2010-08-20T17:55:57Z (GMT). No. of bitstreams: 3 rouge_charles_latex_code.zip: 3121461 bytes, checksum: 94c43d35bd7d507a0ff7f141d183843c (MD5) rouge_charles.pdf: 4243925 bytes, checksum: fef8a6fb8a1955519ddf6050ccb94d12 (MD5) license.txt: 4061 bytes, checksum: 41e40f09a1613097a0559c217c67ff85 (MD5) http://hdl.handle.net/2142/16722 en Copyright 2010 by Charles Jacques Rougé. All rights reserved. shift timing duration statistical significance urbanization water withdrawals detention basins land-use change climate variability Understanding Streamflow Change at the Scale of a Major City: Chicago Civil & Environmental Eng 1251 Civil Engineering 0106 University of Illinois at Urbana-Champaign Thesis M.S. MS:Civil Engineering -UIUC 10KS0106MS