The two moisture sources have quite different oxygen isotope signatures, and this ratio is faithfully preserved in the stalagmites. During strong monsoon years, however, atmospheric circulation brings copious amounts of moisture to this area all the way from the southern Indian Ocean. Our previous research in this area showed that variations in oxygen isotope ratios in rainwater, and consequently, in stalagmites, track changes in the relative abundance of different moisture sources that contribute to summer monsoon rainfall.ĭuring years when monsoon circulation is weak, rainfall here is primarily derived from the moisture that evaporated from the nearby Arabian Sea. Subtle variations in this ratio can arise from a range of climatic conditions at the time the rainwater originally fell. As stalagmites grow, they lock into their structure the oxygen isotope ratios of the percolating rainwater that seeps into the cave. The oxygen in rainwater molecules comes in two primary types of isotopes: heavy and light. Over time, uranium trapped in stalagmites decays into thorium at a predictable pace, so we can figure out the age of each stalagmite growth layer by measuring the ratio of uranium to thorium. Trapped within their growth layers are minute amounts of uranium and other elements that were acquired as rainwater infiltrated the rocks and soil above the cave. Stalagmites are cone-like structures that grow slowly from the ground up, typically at a rate of about one millimeter every 10 years. Stalagmites marked for study inside Mawmluh Cave. To reconstruct past variations in rainfall, we analyzed stalagmites from Mawmluh Cave, near the town of Cherrapunji in the state of Meghalaya- one of the wettest locations in the world. It also raises questions about the region’s current water resources, sustainability, and mitigation policies that discount the possibility of protracted droughts in the future.
Everlasting summer guide cave full#
It indicates that the short instrumental period does not capture the full range of Indian monsoon variability. However, the stalagmite evidence of prolonged, severe droughts over the past 1,000 years paints a different picture. This seemingly reassuring view currently informs the region’s present-day water resource infrastructure. The apparent stability of the Indian monsoon in that data might lead one to surmise that neither protracted droughts lasting multiple years nor frequent droughts are intrinsic aspects of its variability.
Among them, only one-1985 to 1987-was a three-year consecutive drought or worse. Since then, India has experienced about 27 regionally widespread droughts. Scientists began systematically measuring India’s monsoon rainfall with instruments around the 1870s. Our findings have important implications today for water planning in a warming world, particularly for India, which, with its vast monsoon-reliant agriculture industry, is on pace to soon be the most populous country on the planet. Buland Darwaza (Door of Victory) at Fatehpur Sikri, the one-time capital of the Mughal Empire. Around the same time, the elaborate Mughal capital of Fatehpur Sikri was abandoned and the Guge Kingdom collapsed in western Tibet. The depth and duration of the drought would have caused widespread crop failures and the level of famine discussed in written documents at the time.Īnother long drought encompasses the 1630-1632 Deccan famine, one of the most devastating droughts in India’s history. They show how the decline of the Mughal Empire and India’s textile industries in the 1780s and 1790s coincided with the most severe 30-year period of drought over the millennium. The drought periods we detected are in striking synchrony with historical accounts of droughts, famines, mass mortality events, and geopolitical changes in the region. It documents how the Indian subcontinent frequently experienced long, severe droughts unlike any observed in the last 150 years of reliable monsoon rainfall measurements.
They also carry a warning about the potential for catastrophic multiyear droughts in the future.īy analyzing the geochemistry of these stalagmites in a new study published this month in the Proceedings of the National Academy of Sciences, we were able to create the most precise chronology yet of the summer Indian monsoon over the past millennium. These stalagmites are more than geological wonders-like tree rings, their layers record the region’s rainfall history. With each drop, minerals in the water accumulate on the floor below, slowly growing into calcium carbonate towers known as stalagmites. In a remote cave in northeast India, rainwater has slowly dripped from the ceiling in the same spots for over 1,000 years. This story was originally published on The Conversation and appears here under a Creative Commons license.
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