Global Warming Images
 
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IMG_9722_gps.jpg PHD scientist Ian Bartholomews GPS equipment measuring the speed of the Russelll Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster.
 
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IMG_9724_scientific research.jpg Water samples taken from the meltwater river at the snout of the Russell Glacier near Kangerlussuaq in Greenland. These samples were taken by the scientist Ian Bartholemew as part of a PHD study by Edinburgh University. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster.
 
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IMG_9725_science notes.jpg Water samples taken from the meltwater river at the snout of the Russell Glacier near Kangerlussuaq in Greenland. These samples were taken by the scientist Ian Bartholemew as part of a PHD study by Edinburgh University. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster.
 
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IMG_9742_measurement.jpg PHD scientist Ian Bartholomew using a theodolite to measure the speed of the Russelll Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_9745_solar.jpg PHD scientist Ian Bartholomews theodolite tripod being used to measure the speed of the Russelll Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_9752_scientific equipment.jpg PHD scientist Ian Bartholomew taking measurements as part of a study to measure the speed of the Russelll Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_9757_research.jpg PHD scientist Ian Bartholomew taking measurements as part of a study to measure the speed of the Russelll Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_9848_sampling.jpg Water samples taken from the meltwater river at the snout of the Russell Glacier near Kangerlussuaq in Greenland. These measurments were taken by the scientist Ian Bartholemew as part of a PHD study by Edinburgh University. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster.
 
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IMG_a9902_dye trace.jpg PHD scientist Ian Bartholomew using dye tracing techniques as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_a9905_dye test.jpg PHD scientist Ian Bartholomew using dye tracing techniques as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_a9909_dye tracing.jpg PHD scientist Ian Bartholomew using dye tracing techniques as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_a9930_science.jpg PHD scientist Ian Bartholomew using dye tracing techniques as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_a9932_dye tracing.jpg PHD scientist Ian Bartholomew using dye tracing techniques as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_a9936_science.jpg PHD scientist Ian Bartholomew taking measurements as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_a9949_field science.jpg PHD scientist Ian Bartholomew taking measurements as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_a9954_laptop.jpg PHD scientist Ian Bartholomew taking measurements as part of a study to measure the speed of the Russell Glacier near Kangerlussuag Greenland. The study is looking at how increasing quantities of melt water caused by climate change are affecting the glaciers speed which like most glaciers in Greenland has speeded up considerably in the last 20 years. It is thought that the meltwater helps lubricates the glaciers base enabling it to flow faster. As part of the study reflective poles were drilled 4 metres into the ice to measure their speed at various positions on the glacier. Within a month all the poles had fallen over as the glacier melted down over 4 metres
 
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IMG_8305_scientist.jpg.jpg Scientists Anthony Long and Sarah Woodroffe of Durham University Geography Department study maps of Greenland where they are going to study the impact of global warming induced ice sheet melt and isostatic rebound.
 
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IMG_8308_greenland.jpg.jpg Scientists Anthony Long and Sarah Woodroffe of Durham University Geography Department study maps of Greenland where they are going to study the impact of global warming induced ice sheet melt and isostatic rebound.
 
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IMG_8311_research.jpg.jpg Scientists Anthony Long and Sarah Woodroffe of Durham University Geography Department study maps of Greenland where they are going to study the impact of global warming induced ice sheet melt and isostatic rebound.
 
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366W2845.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. Here Dr Jeff Warburton from Durham University inspects a device for measuring the solar radiation falling on the bog.
 
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366W2866.jpg A research project by Dr Jeff Warburton of Durham University measuring wind erosion on the upland blanket peat bog at Moor House Upper Teesdale. As global warming leads to an increase in stormy weather and associated high winds it is expected that wind erosion of the peat bog will increase
 
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366W2869.jpg A research project by Dr Jeff Warburton of Durham University measuring wind erosion on the upland blanket peat bog at Moor House Upper Teesdale. As global warming leads to an increase in stormy weather and associated high winds it is expected that wind erosion of the peat bog will increase
 
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366W2889.jpg A research project by Dr Jeff Warburton of Durham University measuring wind erosion on the upland blanket peat bog at Moor House Upper Teesdale. As global warming leads to an increase in stormy weather and associated high winds it is expected that wind erosion of the peat bog will increase
 
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366W2918.jpg Dr Jeff Warburton of Durham University removed 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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366W2921.jpg Dr Jeff Warburton of Durham University removed 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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366W2923.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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366W2926.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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366W2928.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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366W2934.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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366W2937.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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366W2942.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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366W2945.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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