scholarly journals Revealing a Maritime Cultural Landscape of Hong Kong: The Sai Kung Case Study

2021 ◽  
Vol 17 (2) ◽  
pp. 107-133
Author(s):  
Bill Jeffery ◽  
Joyce Ho-ching Kam

Hong Kong island is located in Southern China at the mouth of the Pearl River. Its coastal location down river from the significant port-city of Guangzhou (formerly Canton), is strategically located in the trade route known as the Maritime Silk Road, the 2,000-year-old trade between China, Southeast Asia, India and Arabia. It was because of this trade that the waters and islands at the Pearl River mouth were frequented by many nations, and where the Portuguese had their port-city, Macau from 1557, and the British were based on Hong Kong island from 1842. Over the next 60 years, the British leased further surrounding territories and the arrangement eventually led to the establishment of the Hong Kong Special Administrative Region, hereafter called the Hong Kong region. A significant maritime cultural landscape was built up, which included sites from earlier periods. An example of this maritime cultural landscape can be seen in the Sai Kung (eastern) district of the Hong Kong region. Many ships travelled along this coastline between the northern China ports and Guangzhou, and a number of coastal facilities were established. Beginning in 2009, a group of Hong Kong residents (Hong Kong Underwater Heritage Group) implemented a series of maritime archaeological projects in the Sai Kung district in collaboration with the Hong Kong Maritime Museum (HKMM). The results of this work can be seen in three maritime archaeology survey and excavation projects implemented from 2014 to 2017, including the discovery of a 1,000-year-old underwater cultural heritage (UCH) site. They complement the many coastal cultural heritage in the Sai Kung district to reveal its maritime cultural landscape.

The Holocene ◽  
2011 ◽  
Vol 22 (6) ◽  
pp. 705-715 ◽  
Author(s):  
Fengling Yu ◽  
Yongqiang Zong ◽  
Jeremy M Lloyd ◽  
Melanie J Leng ◽  
Adam D Switzer ◽  
...  

Author(s):  
Xiangbo Feng ◽  
Wei Zhang ◽  
Zhenglei Zhu ◽  
Amulya Chevuturi ◽  
Wenlong Chen

AbstractUnderstanding water level (WL) fluctuations in river deltas is of importance for managing water resources and minimizing the impacts of floods and droughts. Here, we demonstrate the competing effects of atmospheric and oceanic forcing on multi-timescale variability and changes in the Pearl River Delta (PRD) WLs in southern China, using 52 years (1961–2012) of in-situ observations at 13 hydrological stations. PRD WL presents significant seasonal to decadal variations, with large amplitudes upstream related to strong variability of southern China rainfall, and with relatively small amplitudes at the coastal stations determined by sea level (SL) fluctuations of the northern South China Sea. We find that the strengths of atmospheric and oceanic forcing in PRD are not mutually independent, leading to a distinct contrast of WL–forcing relationships at upstream and coastal stations. In the transition zone, because of counteracts of atmospheric and oceanic forcing, no robust relationships are identified between WL and either of the forcing. We further show that in the drought season of the warm ENSO and PDO epochs, the effect of atmospheric (oceanic) forcing on PRD WL is largely enhanced (weakened), due to increased southern China rainfall and negative SL anomalies. Over the observation period, WL significantly decreased at upstream stations, by up to 28–42 mm/year for flood season, contrasting with the upward trends of <4.3 mm/year at coastal stations across all seasons. Southern China rainfall explains little of the observed WL trends, whilst SL rise is mostly responsible for the WL trends at coastal stations.


2012 ◽  
Vol 9 (1) ◽  
pp. 1-9 ◽  
Author(s):  
Yongfeng Wang ◽  
Yingmin Wang ◽  
Qiang Xu ◽  
Dong Li ◽  
Haiteng Zhuo ◽  
...  

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