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NASA study supports soot as cause of glacier retreat in late 1880's 11/9/2013
Several other studies have pointe to the role that soot plays in altering the earth's albedo, its ability to absorb or reflect sunlight, and its role in causing glaciers to retreat. Now a new study by NASA provides crucial evidence supporting these theories.
 
A NASA-led team of scientists has uncovered strong evidence that soot from a rapidly industrializing Europe caused the abrupt retreat of mountain glaciers in the European Alps that began in the 1860s, a period often thought of as the end of the Little Ice Age.
 
The research, published Sept. 3 in the Proceedings of the National Academy of Sciences, may help resolve a longstanding scientific debate.
In the decades following the 1850s, Europe underwent an economic and atmospheric transformation spurred by industrialization. The use of coal to heat homes and power transportation and industry in Western Europe began in earnest, spewing huge quantities of black carbon and other dark particles into the atmosphere.
 
Black carbon is the strongest sunlight-absorbing atmospheric particle. When these particles settle on the snow blanketing glaciers, they darken the snow surface, speeding its melting and exposing the underlying glacier ice to sunlight and warmer spring and summer air earlier in the year. This diminishing of the snow cover earlier in each year causes the glacier ice to melt faster and retreat.
 


 
 
 
 
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ان جميع مقالات ونصوص "البيئة والتنمية" تخضع لرخصة الحقوق الفكرية الخاصة بـ "المنشورات التقنية". يتوجب نسب المقال الى "البيئة والتنمية" . يحظر استخدام النصوص لأية غايات تجارية . يُحظر القيام بأي تعديل أو تحوير أو تغيير في النص الأصلي. لمزيد من المعلومات عن حقوق النشر يرجى الاتصال بادارة المجلة
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