Research undertaken by the University of Southampton and its associates in Venice has revealed that the sea surface temperature (SST) in coastal regions is rising as much as ten times faster than the global average of 0.13 degrees per decade.
Researchers believe that this is partly as a result of a process known as the ‘urban heat island effect’; where regions experiencing rapid industrial and urban expansion produce vast amounts of heat, making the area warmer than its surroundings.
Professor Carl Amos of Ocean and Earth Sciences at the University of Southampton explains, “The urban heat island effect is a little considered problem with extreme consequences. Take London, for example, the air temperature in the capital and the SST of the Thames is always warmer than it is in the rest of the U.K. Similarly, in South Korea, an area which has seen rapid industrial expansion, the SST is rising at a rate of 0.26 degrees per decade – significantly higher than the global average. Two thirds of this rise is explained by local air temperature, which is largely driven by the urban heat island effect.”
The world’s coastal zone occupies 18 per cent of the world’s land mass and it is estimated that 1.6 billion people live in these regions world-wide. The coastal population density is three times the global average and this population is expected to increase 30 per cent by 2025, with trade and infrastructure at the coasts also increasing steadily. Research suggests that in coastal regions of high urban development, human activity is directly warming adjacent coastal waters and that this contribution to global warming at the coastal zones is equal to, or greater than, other factors such as greenhouse gasses.
Professor Amos, who is based at the National Oceanography Centre Southampton (NOCS), says, “The Marine Climate Change Impacts Partnership Report of 2006 stated that the capacity to define and predict long-term coastal changes due to human causes is ‘unknown’ and confidence in results is ‘low’. This is a major barrier to planning for inevitable changes in coastal SST. Most of these changes at coastlines are caused by human activity, but as it is complex to consider these factors accurately, the official International Panel for Climate Change (IPCC) figures do not take these coastal ‘anomalies’ into account.”
In Venice, with 22 million visitors annually and tourism a year-round source of income, the economy remains critically dependent on the city maintaining its status as one of the world’s most desirable destinations. Southampton’s research in Venice has highlighted the tension between tourism’s economic benefits and environmental repercussions. Analyses of seawater temperature trends in the Venice Lagoon have suggested an increase during winter months ten times greater than that predicted globally by the IPCC – a result directly linked to tourism.
Thousands of jobs and the Venetian economy rely on the survival of the fishing industry, which is dependent on the temperature of the coastal seawater in the Venice Lagoon. A rise in SST in the coastal zone reduces oxygen levels and displaces marine fish and associated nursery grounds, causing catastrophic fish kill phenomena. This research has helped predict the viability of clam fisheries and aquaculture habitats that serve the restaurant trade that caters for millions of tourists every year.
Professor Amos says, “The findings in Venice are the result of a 15 year partnership with the city, which are of great importance and have worldwide applications. Massive urbanization of the coastal zones means urban heat islands represent an acute problem, particularly for the fishing industry and also for the maintenance of coastal infrastructure. The Thames, like the Venice Lagoon, is a major contributor to and casualty of the urban heat island effect. The consequences of the urban heat island effect need addressing urgently to secure the future of our coastal habitats.”
The University of Southampton’s associates in the work at the Venice Lagoon are the Kuwait Institute for Scientific Research, the West Vancouver Marine Laboratory, ISMAR Venice, and the National Water Research Institute of Canada.
Source: University of Southampton.
