Considering the dynamics of water surface boundaries to measure the evolution of hydrological connectivity in the Yangtze River Delta, China

Author:

Li Zhenya1,Kong Fanhua1ORCID,Yin Haiwei2,Meadows Michael E13ORCID,Yang Xiaojun4,Zhou Kejing1,Su Jie2

Affiliation:

1. School of Geography and Ocean Science, Nanjing University, Nanjing, China

2. School of Architecture and Urban Planning, Nanjing University, Nanjing, China

3. Department of Environmental & Geographical Science, University of Cape Town, Cape Town, South Africa

4. Department of Geography, Florida State University, Tallahassee, Florida, USA

Abstract

Dynamics of the terrestrial water surface impact hydrological connectivity. Compared with traditionally deployed water surface parameters, changes in the water-boundary more effectively account for the dynamics of water surface and depth resulting from hydrological variations. However, previous studies of hydrological connectivity generally applied only connectivity length or width parameters using the center line of the water body and therefore fail to fully capture the impact of water boundary dynamics. In this study, optimized water body extraction indices based on data obtained from remote sensing imagery are used to develop a novel metric that indicates water surface boundary dynamics and reveal surface hydrological connectivity changes in the Yangtze River Delta from 1990 to 2020. Detailed inter-annual and seasonal changes in the evolution of water body boundaries from a water surface perspective indicate an overall decline in hydrological connectivity against the background of climate change, increased urbanization, and dam construction. The declining trend in connectivity occurs in three phases, viz. from 1990 to 2003, a gradual decline is exhibited but with a very marked degree of inter-seasonal variability; between 2003 and 2012, connectivity remains relatively constant but with a reduced amplitude between seasons; further reductions in the magnitude of seasonal variations characterize the third phase, to 2020. Meanwhile, the stability of hydrological connectivity, indicated by the coefficient of variation, also exhibits marked spatial heterogeneity. Parts of the delta with more tributaries, including the Huaihe and southeastern basins, have lower stability (7.33 and 6.59, respectively) than the Yangtze basin (6.22). This study presents a novel metric to achieve greater precision in the monitoring of hydrological connectivity. Such information can be harnessed to improve regional ecological and water resource management.

Funder

National Natural Science Foundation of China

National Key Research and Development Program of China

Publisher

SAGE Publications

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous),Geography, Planning and Development

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