A threshold and fewer delivery days
A peer-reviewed PNAS study reconstructs a transient warming event inside the Late Palaeozoic Ice Age from rock cores and reports global sea surface temperatures rising by more than 7 degrees Celsius. The event sits about 304 million years ago; the reconstruction gives a rate of roughly 0.1 degrees Celsius per 1,000 years. The present pace is roughly 1 degree Celsius per 100 years; the two rates stand side by side without being reduced to a single ratio. Le Yao of the Nanjing Institute of Geology and Palaeontology and Thomas Algeo of the University of Cincinnati read the sequence as a modest carbon release crossing a threshold and setting off a larger one. The reconstruction rests on geochemical proxies; the background was an icehouse world with an atmosphere unlike today's. The paper supports the existence of a feedback threshold. On a second physical line, Nishchal Sigdel and colleagues at Virginia Tech (Communications Earth & Environment) reconstruct daily suspended-sediment transport for 175 U.S. rivers back to 1985 with turbidity-based models. The window carrying 90 per cent of the annual load narrows from about 69 days to about 50 days. Only 15 per cent of rivers show both a rising annual load and a narrowing window; some rivers carry more sediment each year, while others deliver roughly the same load in sharper bursts. The shared stress is pace: a threshold-crossing release beside sediment delivered in fewer days.[1], [2]
