Global Warming Images
 
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20130305_P3050033.jpg Scafell and Scafell Pike from the Upper Esk with a frozen tarn in the foreground, Lake District, UK.
 
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20130305_P3050037.jpg Scafell and Scafell Pike from the Upper Esk with a frozen tarn in the foreground, Lake District, UK.
 
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20130305_P3050041.jpg Bow Fell and Esk Pike from the Upper Esk with a frozen tarn in the foreground, Lake District, UK.
 
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20130313_P3130001.jpg Grains Ghyll in Borrowdale, Lake District, UK, frozen over during a cold winter snap.
 
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20130313_P3130009.jpg Grains Ghyll in Borrowdale, Lake District, UK, frozen over during a cold winter snap.
 
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20130313_P3130017.jpg A frozen waterfall in Grains Ghyll in Borrowdale, Lake District, UK.
 
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20130313_P3130027.jpg A climber in Custs Gully on Great End, a grade one winter route, Lake District, UK. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130028.jpg A climber in Custs Gully on Great End, a grade one winter route, Lake District, UK. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130031.jpg A climber in Custs Gully on Great End, a grade one winter route, Lake District, UK. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130047.jpg A climber topping out in Custs Gully on Great End, a grade one winter route, Lake District, UK, with Great Gable in the background. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130052.jpg A climber topping out in Custs Gully on Great End, a grade one winter route, Lake District, UK, with Great Gable in the background. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130055.jpg A climber topping out in Custs Gully on Great End, a grade one winter route, Lake District, UK, with Great Gable in the background. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130065.jpg A climber in Custs Gully on Great End, a grade one winter route, Lake District, UK. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130068.jpg A climber in Custs Gully on Great End, a grade one winter route, Lake District, UK. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130072.jpg A climber in Custs Gully on Great End, a grade one winter route, Lake District, UK. Climate change has reduced the likelihood of winter conditions, making winter climbing safe.
 
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20130313_P3130081.jpg Wind slab drifted snow on Great End , Lake District, Cumbria, UK.
 
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20130313_P3130097.jpg A raven flying over Great Gable in the Lake District, Cumbria, UK.
 
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20130313_P3130106.jpg A hill walker on the summit of Scafell Pike, the highest mountain in England, Lake District, UK, looking towrds the Helvellyn Range in the distance.
 
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20130313_P3130107.jpg A hill walker on the summit of Scafell Pike, the highest mountain in England, Lake District, UK, looking towrds the Helvellyn Range in the distance.
 
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20130313_P3130110.jpg A line of cairns with wind blown snow, indicating the direction of the wind when the snow fell, Scafell Pike, Lake District, Cumbria, UK.
 
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20130313_P3130120.jpg Drifting snowpack on Scafell Pike, Lake District, UK, looking towards Bow Fell and Crinkle Crags,
 
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20130313_P3130123.jpg Drifting snowpack on Scafell Pike, Lake District, UK, looking towards Bow Fell and Crinkle Crags,
 
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20130313_P3130128.jpg A spring near Esk Hause, which is the start of the River Esk, near Great End, Lake District, UK.
 
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20130313_P3130130.jpg A spring near Esk Hause, which is the start of the River Esk, near Great End, Lake District, UK.
 
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20130313_P3130135.jpg A mountaineer testing the thickness of ice on sprinkling Tarn ot see if it safe to walk on, Lake District, UK. Anything over 4 inches thick is generally safe. Climate change has affected winter weather in recent years.
 
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20130313_P3130143.jpg A mountaineer testing the thickness of ice on sprinkling Tarn ot see if it safe to walk on, Lake District, UK. Anything over 4 inches thick is generally safe. Climate change has affected winter weather in recent years.
 
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20130313_P3130144.jpg A mountaineer testing the thickness of ice on sprinkling Tarn ot see if it safe to walk on, Lake District, UK. Anything over 4 inches thick is generally safe. Climate change has affected winter weather in recent years.
 
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20130313_P3130156.jpg A mountaineer testing the thickness of ice on sprinkling Tarn ot see if it safe to walk on, Lake District, UK. Anything over 4 inches thick is generally safe. Climate change has affected winter weather in recent years.
 
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20130313_P3130162.jpg Wind drifted snow on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great End, Lake District, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130165.jpg Wind drifted snow on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great End, Lake District, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130172.jpg Wind drifted snow on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great End, Lake District, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130173.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great Gable, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130180.jpg Wind drifted snow on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great End, Lake District, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130181.jpg Wind drifted snow on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great End, Lake District, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130187.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great Gable, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130194.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great Gable, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130198.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, with drifted snow making patterns on the ice. Climate change has affected winter weather in recent years.
 
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20130313_P3130204.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, with drifted snow making patterns on the ice. Climate change has affected winter weather in recent years.
 
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20130313_P3130205.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, with drifted snow making patterns on the ice. Climate change has affected winter weather in recent years.
 
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20130313_P3130207.jpg Wind drifted snow on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, Lake District, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130208.jpg Wind drifted snow on Sprinkling Tarn at the head of Borrowdale, frozen solid, Lake District, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130210.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great Gable, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130228.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130229.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130230.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130244.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Glaramara, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130250.jpg A climber on Sprinkling Tarn at the head of Borrowdale, frozen solid, looking towards Great End, with drifted snow making patterns on the ice, Lake District, Cumbria, UK. Climate change has affected winter weather in recent years.
 
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20130313_P3130264.jpg Taylor force Gill waterfall, partially frozen above Seathwaite, in Borrowdale, Lake District, UK. Climate change has affected winter conditions in recent years.
 
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20130313_P3130266.jpg Taylor force Gill waterfall, partially frozen above Seathwaite, in Borrowdale, Lake District, UK. Climate change has affected winter conditions in recent years.
 
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20130313_P3130268.jpg Taylor force Gill waterfall, partially frozen above Seathwaite, in Borrowdale, Lake District, UK. Climate change has affected winter conditions in recent years.
 
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20130313_P3130276.jpg Taylor force Gill waterfall, partially frozen above Seathwaite, in Borrowdale, Lake District, UK. Climate change has affected winter conditions in recent years.
 
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20130313_P3130284.jpg Taylor force Gill waterfall, partially frozen above Seathwaite, in Borrowdale, Lake District, UK. Climate change has affected winter conditions in recent years.
 
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20130212_B18A9183.jpg Icicles at the closed Kirkstone slate quarry, Lake District, UK,
 
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20130212_IMG_3359.jpg Icicles at the closed Kirkstone slate quarry, Lake District, UK,
 
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20130122_B18A8322.jpg Herdwick sheep in Little Langdale, Lake District, UK, with a frozen Blea Tarn behind.
 
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20121229_B18A6198.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6204.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6207.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6211.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6218.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6221.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_B18A6224.jpg An avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_PC290076.jpg A gaping hole left where a massive block of ice detached causing an avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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20121229_PC290080.jpg A gaping hole left where a massive block of ice detached causing an avalanche on Machapuchare or Fishtail Peak in the Annapurna Himalaya, Nepal. It was caused by a massive block of glacial ice detaching from the summit cliffs of this 6993 metre tall peak on 29th December 2012. Such ice avalanches are more common in Spring and summer, as in winter, the ice is normally frozen and more stable. The avalanche descended around 12,000 feet, and covered trekkers on the valley path below in a dusting of snow.
 
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