Global Warming Images
 
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366W2948.jpg Dr Jeff Warburton of Durham University downloads data from a bed load logger from a river in Moor House National Nature Reserve in Upper Teesdale Cumbria UK. This experiment measures the movement of bed load materials over time. Most movement and erosion occurs during peak flows following wet weather. An increase in stormy weather due to global warming will lead to more frequent erosion events.
 
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366W2952.jpg Dr Jeff Warburton of Durham University downloads data from a bed load logger from a river in Moor House National Nature Reserve in Upper Teesdale Cumbria UK. This experiment measures the movement of bed load materials over time. Most movement and erosion occurs during peak flows following wet weather. An increase in stormy weather due to global warming will lead to more frequent erosion events.
 
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366W2955.jpg Dr Jeff Warburton of Durham University downloads data from a bed load logger from a river in Moor House National Nature Reserve in Upper Teesdale Cumbria UK. This experiment measures the movement of bed load materials over time. Most movement and erosion occurs during peak flows following wet weather. An increase in stormy weather due to global warming will lead to more frequent erosion events.
 
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366W2789.jpg Andy Seir from the environmental change network speaking about global warming at a Climate Change Explorer event put on by dowdales School, Barrow in Furness, Cumbria
 
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366W2812.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2813.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2818.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2820.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2823.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2826.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2827.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2832.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure carbon release from the peat bog.
 
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366W2838.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure the water table of the peat bog.
 
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366W2842.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure the carbon and methane released from the peat bog
 
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366W2846.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure the carbon and methane released from the peat bog
 
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366W2850.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure the carbon and methane released from the peat bog
 
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366W2854.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the specialist equipment used to measure the carbon and methane released from the peat bog
 
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366W2858.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Peat bogs should be carbon sinks but due to rising temperatures the carbon budget of the bogs is changeing to a carbon deficit. The picture shows the weather station that has a continuous weather record going back 50 years.
 
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366W2888.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. Warming temperatures have resulted in increased plant productivity and has lead to colonisation of once bare areas of the peat bog. This picture shows Dr Jeff Warburton who is measuring wind erosion on the peat bog checking his erosion markers. When the markers were first placed they were in bare peat but have subsequently been covered by recolonising cotton grass
 
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366W2915.jpg Moor House National Nature Reserve in the North Pennines has been a site of scientific research going back 50 years. Weather records show a gradual warming over the last 50 years and a dramatic decline in winter snow cover. This has started to alter some of the specialised arctic plant communities and has also affected the carbon budget of the upland blanket peat bog. The picture shows an experiment to measure temperatures of the stream bed over time
 
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366W2931.jpg Dr Jeff Warburton of Durham University downloads data from a bed load logger from a river in Moor House National Nature Reserve in Upper Teesdale Cumbria UK. This experiment measures the movement of bed load materials over time. Most movement and erosion occurs during peak flows following wet weather. An increase in stormy weather due to global warming will lead to more frequent erosion events.
 
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366W2932.jpg Dr Jeff Warburton of Durham University downloads data from a bed load logger from a river in Moor House National Nature Reserve in Upper Teesdale Cumbria UK. This experiment measures the movement of bed load materials over time. Most movement and erosion occurs during peak flows following wet weather. An increase in stormy weather due to global warming will lead to more frequent erosion events.
 
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IMG_0685.jpg Graph showing how global and Arctic temperatures have risen above the 1800 to 2000 average, taken from an International Arctic research Centre(IARC) document
 
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IMG_0687.jpg Global Climate modelling undertaken by the IPCC showing predicted rises in temperature by the end of this century. The model shows the Arctic being more greatly affected than other latitudes.
 
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IMG_0688.jpg A graph from the National Research Council showing how global temperatures have mirrored global C02 concentrations for the last 160,000 years, taken from a report by the International Arctic research Centre
 
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IMG_0689.jpg A graph showing the rise in permafrost ground temperature in Fairbanks since the 1960's based on research by V Romanovsky and taken from a document produced by the International Arctic research Centre.
 
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IMG_0690.jpg An aerial showing the retreat of Portage glacier in Alaska with data supplied by D Trabant and K Crossen, taken from a document published by the International Arctic Research Centre
 
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IMG_0691.jpg A graph showing the rate at which glaciers have been retreating with data by W Harrison and K Echelmeyer in a document produced by the International Arctic Research Centre
 
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366W9610_climate change_pollution.jpg An instrument for measuring airbourne dust pollution in Castle Cement Quarry in Clitheroe Lancashire UK
 
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366W9613_global warming_pollution.jpg An instrument for measuring airbourne dust pollution in Castle Cement Quarry in Clitheroe Lancashire UK
 
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