published_or_final_version / abstract / Earth Sciences / Doctoral / Doctor of Philosophy

published_or_final_version / abstract / Transport Policy and Planning / Master / Master of Arts in Transport Policy and Planning

published_or_final_version / Geography and Geology / Doctoral / Doctor of Philosophy

published_or_final_version / Urban Planning / Master / Master of Science in Urban Planning

An important process of economic reform in China has been to promote the inflow of foreign direct investment (FDI). After more than thirty years of economic reform, China has become one of the most important destinations for cross-border direct investment. Since Taiwan has become one of the major source countries of FDI in China, Taiwanese investment has experienced changes in spatial patterns and industrial composition since the 1990s. As a result of active government promotion through various policy measures, FDI in China has grown rapidly since 1978, especially in the 1990s. Taiwanese authorities released the investment strategy, “Be patient, No hurry”in 2001, and since then China has become the biggest target of Taiwanese investment outside of Taiwan; money from Taiwan forms a significant portion of foreign capital in China. Due to coastal and other geographical advantages of the three major economic regions possessing good investment environments (that is, the Pearl River Delta, Yangtze River Delta (YRD) and Bohai Bay economic region), the landscape of Taiwanese direct investment (TDI) in recent years has been moving Northward and Westward significantly. Initially, the Taiwanese investment in labor-intensive industries mainly concentrated in southern China, including Guangdong and Fujian, because of the cheap labor and geographic proximity. Since the mid-1990s, the industries of Yangtze Rive Delta region has become a new investment hotspot for Taiwanese enterprises while their industrial nature is changing to be more technology-intensive and domestic market-oriented.

Wong Kok Ming David. / "Architecture Department, Chinese University of Hong Kong, Master of Architecture Programme 2007-2008, design report." / Abstracts in English and Chinese.

Gao, Xuehua. / Thesis (M.Phil.)--Chinese University of Hong Kong, 2010. / Includes bibliographical references (leaves 83-96). / Abstracts in English and Chinese. / List of Figures --- p.viii / List of Tables --- p.x / Symbols --- p.xi / Acronyms --- p.xiii / Chapter Chapter 1 --- Introduction --- p.1 / Chapter 1.1 --- Background and Motivation --- p.1 / Chapter 1.2 --- Study Site: Pearl River Basin --- p.3 / Chapter 1.3 --- Study Objectives --- p.4 / Chapter Chapter 2 --- Literature Review --- p.5 / Chapter 2.1 --- Methods for Determining ETa --- p.6 / Chapter 2.2 --- Limitations of Current Studies on ETa --- p.15 / Chapter Chapter 3 --- Methodology and Data --- p.17 / Chapter 3.1 --- Modelling Framework and Procedure --- p.17 / Chapter 3.2 --- Complementary Relationship Models --- p.19 / Chapter 3.3 --- Long-Term Water Balance Models --- p.22 / Chapter 3.4 --- Spatial Interpolation --- p.25 / Chapter 3.5 --- Trend Analysis --- p.26 / Chapter 3.6 --- Meteorological and Hydrological Data Sets --- p.29 / Chapter Chapter 4 --- Estimation of Actual Evapotranspiration --- p.40 / Chapter 4.1 --- Selection of Water Balance Model --- p.40 / Chapter 4.2 --- Selection of Complementary Relationship Model --- p.46 / Chapter 4.3 --- Calibration of Granger & Grey´ةs Model --- p.48 / Chapter 4.4 --- Estimation of A ctual Evapotranspiration --- p.48 / Chapter 4.5 --- Validation of Granger & Grey ´ةs Model --- p.49 / Chapter Chapter 5 --- Spatio-Temporal Variations of Actual Evapotranspiration --- p.50 / Chapter 5.1 --- Annual ETa --- p.50 / Chapter 5.2 --- Seasonal ETa --- p.56 / Chapter 5.3 --- Summary --- p.63 / Chapter 5.4 --- Discussion of the Changing Climatic Factors --- p.64 / Chapter Chapter 6 --- Sensitivity Analysis of Actual Evapotranspiration to Climatic Variables --- p.66 / Chapter 6.1 --- Sensitivity Curves and Sensitivity Coefficients --- p.66 / Chapter 6.2 --- Procedures and Results --- p.61 / Chapter 6.3 --- Implications of Sensitivity Coefficients for Water Resources Management --- p.77 / Chapter Chapter 7 --- Conclusion --- p.79 / Chapter 7.7 --- Summary --- p.79 / Chapter 7.2 --- Conclusion --- p.80 / Chapter 7.3 --- Implication --- p.81 / Chapter 7.4 --- Limitation and Future Work --- p.82 / References --- p.83 / ","

Thesis (M. A.)--University of Hong Kong, 2006. / Title proper from title frame. Also available in printed format.

Water isotope tracers and multi-proxy paleolimnological approaches are used to characterize the present and past hydrology of the Slave River Delta (SRD), NWT. This research addresses crucial gaps in knowledge about the role of major hydrological processes on the water balances of northern freshwater lakes, and responds to concerns expressed by local land users about declining flood frequency in the delta following upstream river regulation. Contemporary hydrological studies were conducted using multiple lakewater sampling campaigns from a suite of 41 delta lakes situated in three previously recognized biogeographical zones - outer delta, mid-delta and apex – that were initially sampled in fall 2002, and again immediately following the spring melt, during summer, and in the fall of 2003-2005. Paleolimnological studies aimed at reconstructing flood frequency in the Slave River focus on a sediment core obtained from a flood-susceptible lake in the active delta. Together, contemporary and past studies of SRD hydrology provide a detailed picture of environmental change and variability in an important northern freshwater ecosystem.

The Best PhD Thesis in the Faculties of Architecture, Arts, Business &Economics, Education, Law and Social Sciences (University of HongKong), Li Ka Shing Prize, 2009-2010 / published_or_final_version / Sociology / Doctoral / Doctor of Philosophy