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Many cultural heritage sites are suffering damage or loss due to anthropogenic climate change. Causes include sea rises and coastal erosion, the increased incidence of extreme weather events such as storms and cyclones, changes in rainfall patterns, extreme periods of drought, and bushfires. [1]
Climate change is an increasing focus of cultural heritage organisations such as the International Council on Monuments and Sites (ICOMOS). [2] UNESCO's List of World Cultural Heritage in Danger includes "threatening impacts of climatic, geological or other environmental factors" as a category of threat. [3]
Sites at risk of loss or damage due to climate change are often also at risk from other social and political factors, such as war, land use and agricultural practices, and tourism.
Sea level rise and coastal erosion are causing loss of structures and archaeological material in the historic port city of Kilwa Kisiwani. Portions of some monuments are already underwater. Mitigation strategies under development include engineered structures (gabions) to minimise the effect of wave action. [4]
The ancient city site of Chan Chan has experienced both more extreme rainfall and periods of drought, due to El Nino weather patterns. This area has always experienced extreme weather events, but the frequency of events is increasing. Rising groundwater is destabilising building foundations. [5] Mitigation has included strategies to control the rising water table, stabilisation of perimeter walls, architectural documentation, local skills development and awareness-building campaigns, and a disaster preparedness plan. [6]
Due to decrease of sea areas and higher exposure to storms, the 19th century whalers' settlement of Hershel Island had to be relocated inland to keep the buildings dry and avoid flooding of low lying structures. If coastal erosion continues another relocation might be needed and lead to the abandonment of some structures. The deterioration of the permafrost compromises graves structures and leads to buried caskets tumbling and breakage. (Case studies on climate change and World Heritage, Unesco) [7]
Building structures in the Mosque City of Bagerhat are decaying due to rising water and soil salinity. Salt crystals that become embedded in the rock expand in the presence of moisture and hasten the disintegration and weathering of stone buildings. [8]
Also known as Easter Island, Rapa Nui has been a World Heritage Site since 1995. The stone statues on Rapa Nui are threatened by sea level rises and coastal damage from storms. [9] An increase in ocean swells and wave heights causes undercutting and erosion of rock faces and loss of archaeological remains. [10]
Increased coastal erosion and rising sea levels threaten several historic castles in Great Britain, including Hurst Castle in Hampshire, Tintagel in Cornwall, Piel Castle in Cumbria, Bayard's Cove Fort in Devon, Garrison Walls in the Isles of Scilly and Calshot Castle in Southampton. According to site managers English Heritage, it will be necessary to repair walls and improve defences against storms to prevent further damage. [11]
Increased rainfall and extreme weather events are also increasing the risk of flooding and slope instability in the old city of Edinburgh. Annual rainfall has increased 13% since 1970. Increased wetting and drying is eroding the sandstone used to build Edinburgh Castle and eroding the volcanic rock on which it is built. [12]
Rising sea water and inundation threaten the city of Venice and its lagoon. [13]
A flood is an overflow of water that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are of significant concern in agriculture, civil engineering and public health. Human changes to the environment often increase the intensity and frequency of flooding. Examples for human changes are land use changes such as deforestation and removal of wetlands, changes in waterway course or flood controls such as with levees. Global environmental issues also influence causes of floods, namely climate change which causes an intensification of the water cycle and sea level rise. For example, climate change makes extreme weather events more frequent and stronger. This leads to more intense floods and increased flood risk.
Chan Chan, sometimes itself called Chimor, was the capital city of the Chimor kingdom. It was the largest city of the pre-Columbian era in South America. It is now an archeological site in the department of La Libertad five kilometers (3.1 mi) west of Trujillo, Peru.
Kilwa District is one of six administrative districts of Lindi Region in Tanzania. The District covers an area of 15,000 km2 (5,800 sq mi). The district is comparable in size to the land area of the nation state of East Timor. Kilwa district is bordered to the north by Rufiji District in Pwani Region, to the east by the Indian Ocean, to the south by the Lindi District, Nachingwea District together with Ruangwa District, and to the west by the Liwale District. The district borders every other district in Lindi Region except Lindi Municipal District. The district seat (capital) is the town of Kilwa Masoko. The district is named after the medieval Swahili city state of Kilwa Kisiwani. According to the 2012 census, the district has a total population of 190,744. By 2022, the population had increased to 297,676.
Rapa Nui National Park is a national park and UNESCO World Heritage Site located on Easter Island, Chile. Rapa Nui is the Polynesian name of Easter Island; its Spanish name is Isla de Pascua. The island is located in the southeastern Pacific Ocean, at the southeastern extremity of the Polynesian Triangle. The island was taken over by Chile in 1888. Its fame and World Heritage status arise from the 887 extant stone statues known by the name "moai", whose creation is attributed to the early Rapa Nui people who inhabited the island starting between 300 and 1200 AD. Much of the island has been declared as Rapa Nui National Park which, on 22 March 1996, UNESCO designated a World Heritage Site under cultural criteria (i), (iii), & (v). Rapa Nui National Park is now under the administrative control of the Ma´u Henua Polynesian Indigenous Community, which is the first autonomous institute on the island. The indigenous Rapa Nui people have regained authority over their ancestral lands and are in charge of the management, preservation and protection of their patrimony. On the first of December 2017, the ex-President Michelle Bachelet returned ancestral lands in the form of the Rapa Nui National Park to the indigenous people. For the first time in history, the revenue generated by the National Park is invested in the island and used to conserve the natural heritage.
The Australian environment ranges from virtually pristine Antarctic territory and rainforests to degraded industrial areas of major cities. Forty distinct ecoregions have been identified across the Australian mainland and islands. Central Australia has a very dry climate. The interior has a number of deserts while most of the coastal areas are populated. Northern Australia experiences tropical cyclones while much of the country is prone to periodic drought. This dry and warm environment and exposure to cyclones, makes Australia particularly vulnerable to climate change -- with some areas already experiencing increases in wildfires and fragile ecosystems.
Heart of Neolithic Orkney is a group of Neolithic monuments on the Mainland of the Orkney Islands, Scotland. The name was adopted by UNESCO when it proclaimed these sites as a World Heritage Site in December 1999.
Orongo is a stone village and ceremonial center at the southwestern tip of Rapa Nui. It consists of a collection of low, sod-covered, windowless, round-walled buildings with even lower doors positioned on the high south-westerly tip of the large volcanic caldera called Rano Kau. Below Orongo on one side a 300-meter barren cliff face drops down to the ocean; on the other, a more gentle but still very steep grassy slope leads down to a freshwater marsh inside the high caldera.
The North Shore, in the context of geography of the Island of Oʻahu, refers to the north-facing coastal area of Oʻahu between Kaʻena Point and Kahuku. The largest settlement is Haleʻiwa.
The effects of climate change on small island countries are affecting people in coastal areas through sea level rise, increasing heavy rain events, tropical cyclones and storm surges. These effects of climate change threaten the existence of many island countries, their peoples and cultures. They also alter ecosystems and natural environments in those countries. Small island developing states (SIDS) are a heterogenous group of countries but many of them are particularly at risk to climate change. Those countries have been quite vocal in calling attention to the challenges they face from climate change. For example, the Maldives and nations of the Caribbean and Pacific Islands are already experiencing considerable impacts of climate change. It is critical for them to implement climate change adaptation measures fast.
Climate change in Alabama encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Alabama.
Climate change in Delaware encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Delaware.
Climate change in Louisiana encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of Louisiana.
Climate change has had large impacts on the ecosystems and landscapes of the US territory Puerto Rico. According to a 2019 report by Germanwatch, Puerto Rico is the most affected by climate change. The territory's energy consumption is mainly derived from imported fossil fuels.
Climate change in South Carolina encompasses the effects of climate change, attributed to man-made increases in atmospheric carbon dioxide, in the U.S. state of South Carolina.
Climate changein the Caribbean poses major risks to the islands in the Caribbean. The main environmental changes expected to affect the Caribbean are a rise in sea level, stronger hurricanes, longer dry seasons and shorter wet seasons. As a result, climate change is expected to lead to changes in the economy, environment and population of the Caribbean. Temperature rise of 2°C above preindustrial levels can increase the likelihood of extreme hurricane rainfall by four to five times in the Bahamas and three times in Cuba and the Dominican Republic. A rise in sea level could impact coastal communities of the Caribbean if they are less than 3 metres (10 ft) above the sea. In Latin America and the Caribbean, it is expected that 29–32 million people may be affected by the sea level rise because they live below this threshold. The Bahamas is expected to be the most affected because at least 80% of the total land is below 10 meters elevation.
Climate change is having serious impacts in the Philippines such as increased frequency and severity of natural disasters, sea level rise, extreme rainfall, resource shortages, and environmental degradation. All of these impacts together have greatly affected the Philippines' agriculture, water, infrastructure, human health, and coastal ecosystems and they are projected to continue having devastating damages to the economy and society of the Philippines.
Climate change in Ghana is impacting the people in Ghana in several ways as the country sits at the intersection of three hydro-climatic zones. Changes in rainfall, weather conditions and sea-level rise will affect the salinity of coastal waters. This is expected to negatively affect both farming and fisheries. Low precipitation, drought and wild fires are also some major effects associated with climate change in Ghana.
Climate change in Senegal will have wide reaching impacts on many aspects of life in Senegal. Climate change will cause an increase in average temperatures over west Africa by between 1.5 and 4 °C by mid-century, relative to 1986–2005. Projections of rainfall indicate an overall decrease in rainfall and an increase in intense mega-storm events over the Sahel. The sea level is expected to rise faster in West Africa than the global average. Although Senegal is currently not a major contributor to global greenhouse gas emissions, it is one of the countries most vulnerable to climate change.
Climate change in Fiji is an exceptionally pressing issue for the country - as an island nation, Fiji is particularly vulnerable to rising sea levels, coastal erosion and extreme weather. These changes, along with temperature rise, will displace Fijian communities and will prove disruptive to the national economy - tourism, agriculture and fisheries, the largest contributors to the nation's GDP, will be severely impacted by climate change causing increases in poverty and food insecurity. As a party to both the Kyoto Protocol and the Paris Climate Agreement, Fiji hopes to achieve net-zero emissions by 2050 which, along with national policies, will help to mitigate the impacts of climate change.
Getbol (Korean: 갯벌) are mudflats, or tidal flats, coastal sedimentary systems. They are important habitats for different types of organisms, including migrating birds and marine fauna such as clams, crabs, octopuses, and snails. In 2021, four getbol sites in South Korea were listed as a UNESCO World Heritage Site due to their outstanding natural properties. Each of these sites represent a different type of getbol.