Global Warming Images
 
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IMG_3262_p.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3272_p.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3275_p.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3280_p.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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366W6261_balloon.jpg Funafuti atol Tuvalu on the front line of the battle against global warming Only 15 feet above sea level at the highest point with many parts of the island lying at or barely above current sea levels rising sea levels are increasingly putting the island population of 10 000 Tuvaluans at risk It seems likely that this island nation will be the first country to disapear completely as a result of climate change global warming Sea levels in the Pacific have risen slowly over the last 20 years and the rate of rise seems likely to increase as ice sheets and glaciers melt more rapidly with ever warming temperatures Tuvalu is the smallest country in the world only 26 Km2 and most vulnerable to sea level rise It lies close to the equator and virtually on the international date line Ever rising seas threaten to make the island uninhabitable Already during the highest tides sea water is forced up through the porous coral atol and floods many low lying areas of the island during the highest tides This salt water incursion poisons the thin soils and makes growing crops increasingly difficult leaving the Tuvaluans increasingly dependant on expensive imports As well as sea level rise the weather patterns are altering with a shift in the cyclone period by a month and an increase in stormy weather The stormy weather is creating greater wave erosion and many parts of the island are suffering land loss as palm trees are washed into the sea as the island is undercut by wave action
 
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366W6261_tern.jpg Funafuti atol Tuvalu on the front line of the battle against global warming Only 15 feet above sea level at the highest point with many parts of the island lying at or barely above current sea levels rising sea levels are increasingly putting the island population of 10 000 Tuvaluans at risk It seems likely that this island nation will be the first country to disapear completely as a result of climate change global warming Sea levels in the Pacific have risen slowly over the last 20 years and the rate of rise seems likely to increase as ice sheets and glaciers melt more rapidly with ever warming temperatures Tuvalu is the smallest country in the world only 26 Km2 and most vulnerable to sea level rise It lies close to the equator and virtually on the international date line Ever rising seas threaten to make the island uninhabitable Already during the highest tides sea water is forced up through the porous coral atol and floods many low lying areas of the island during the highest tides This salt water incursion poisons the thin soils and makes growing crops increasingly difficult leaving the Tuvaluans increasingly dependant on expensive imports As well as sea level rise the weather patterns are altering with a shift in the cyclone period by a month and an increase in stormy weather The stormy weather is creating greater wave erosion and many parts of the island are suffering land loss as palm trees are washed into the sea as the island is undercut by wave action
 
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366W6429_tern.jpg Funafuti atol Tuvalu on the front line of the battle against global warming Only 15 feet above sea level at the highest point with many parts of the island lying at or barely above current sea levels rising sea levels are increasingly putting the island population of 10 000 Tuvaluans at risk It seems likely that this island nation will be the first country to disapear completely as a result of climate change global warming Sea levels in the Pacific have risen slowly over the last 20 years and the rate of rise seems likely to increase as ice sheets and glaciers melt more rapidly with ever warming temperatures Tuvalu is the smallest country in the world only 26 Km2 and most vulnerable to sea level rise It lies close to the equator and virtually on the international date line Ever rising seas threaten to make the island uninhabitable Already during the highest tides sea water is forced up through the porous coral atol and floods many low lying areas of the island during the highest tides This salt water incursion poisons the thin soils and makes growing crops increasingly difficult leaving the Tuvaluans increasingly dependant on expensive imports As well as sea level rise the weather patterns are altering with a shift in the cyclone period by a month and an increase in stormy weather The stormy weather is creating greater wave erosion and many parts of the island are suffering land loss as palm trees are washed into the sea as the island is undercut by wave action
 
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366W7905_tuvalu.jpg Funafuti atol, Tuvalu, on the front line of the battle against global warming. Only 15 feet above sea level at the highest point (with many parts of the island lying at or barely above current sea levels) rising sea levels are increasingly putting the island population of 10,000 Tuvaluans at risk. It seems likely that this island nation will be the first country to disapear completely as a result of climate change/global warming. Sea levels in the Pacific have risen slowly over the last 20 years and the rate of rise seems likely to increase as ice sheets and glaciers melt more rapidly with ever warming temperatures. Tuvalu is the smallest country in the world, only 26 Km2, and most vulnerable to sea level rise. It lies close to the equator and virtually on the international date line. Ever rising seas threaten to make the island uninhabitable. Already during the highest tides, sea water is forced up through the porous coral atol and floods many low lying areas of the island during the highest tides. This salt water incursion poisons the thin soils and makes growing crops increasingly difficult, leaving the Tuvaluans increasingly dependant on expensive imports. As well as sea level rise the weather patterns are altering with a shift in the cyclone period by a month and an increase in stormy weather. The stormy weather is creating greater wave erosion and many parts of the island are suffering land loss, as palm trees are washed into the sea as the island is undercut by wave action.
 
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IMG_3272_holiday park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3280_caravan park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3262_coastal protection.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3268_Kinmel Bay.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3275_caravan park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. The rocks have been placed to try and strengthen the sea wall.
 
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IMG_3369_pumping station.jpg A sign for a pumping station at Talacre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3408_coastal pumping.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3414_Talacre.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3416_Point of Ayr.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3418_pumping.jpg A pumping station at Talachre on the North Wales coast. This section of coast is reclaimed salt marsh and is only kept dry by pumping. It is increasingly threatened by climate change driven sea level rise.
 
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IMG_3554_bungalow.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
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IMG_3556_insurance risk.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
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IMG_3557_Prestatyn.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
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IMG_3559_flood risk.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
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IMG_3566_bungalow.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These bungalows in Prestatyn are part of the area at risk.
 
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IMG_3575_flood evacuation.jpg A flood evacuation sign on a caravan park in Towyn, which is very susceptible to coastal flooding.
 
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IMG_3582_holiday park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay.
 
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IMG_3584_caravan park.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay.
 
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IMG_3593_sea wall.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These rocks have been placed to try and re-inforce the sea wall.
 
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IMG_3598_coastal defences.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These rocks have been placed to try and re-inforce the sea wall.
 
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IMG_3606_low lying.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These rocks have been placed to try and re-inforce the sea wall.
 
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IMG_3619_Kinmel Bay.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay.
 
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IMG_3621_sea defences.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay. These rocks have been placed to try and re-inforce the sea wall.
 
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IMG_3627_Towyn.jpg The area of the North Wales coast between Prestatyn and Abergele was reclaimed from an ancient salt marsh. As such it is flat, low lying and susceptible to coastal flooding. Climate change driven sea level rise increases the risk making it one of the most at risk coastal areas in the British Isles. In 1990 a combination of strong westerly winds a high tide and a 1.5m storm surge breached 400 metres of the sea wall and inundated 2800 properties in Towyn and Kinmel Bay.
 
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