大气中二氧化碳上升引起的洪水

Q1 Earth and Planetary Sciences
GSA Today Pub Date : 2020-10-01 DOI:10.1130/gsatg427a.1
G. Retallack, G. Conde
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引用次数: 2

摘要

二氧化碳上升的一个直接后果是毁灭性的洪水日益增加,因为大气中的二氧化碳为光合作用提供了更多的碳,而每年落叶植物部署的气孔减少了。当植物的蒸腾作用减少时,更多的水以溪流和洪水的形式流走。在这里,我们量化了这种影响与高分辨率的观察变化的密度和气孔的大小,自1754年以来的一种树,银杏。观测到的最大潜在蒸腾的下降与密西西比河水位的上升相对应,并表示从1829年到2015年的潜在蒸腾下降为18 mL - 1 m-2:减少29%。大气中二氧化碳的增加和蒸腾作用的减少促进了洪水,这阻碍了低地的种植,并使诸如百年一遇的洪水之类的保险和分区概念变得无关紧要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Flooding Induced by Rising Atmospheric Carbon Dioxide
A direct consequence of rising CO2 is increasingly devastating flooding, because deciduous plants deploy fewer stomates each year as the atmospheric CO2 supplies more carbon for photosynthesis. When plants transpire less, more water runs off in streams and floods. Here we quantify this effect with highresolution observations of changing density and size of stomates of a mesic tree, Ginkgo, since 1754. The observed decline in maximum potential transpiration corresponds with rising water levels in the Mississippi River and represents a potential transpiration decline from 1829 to 2015 of 18 mL s–1 m–2: a reduction of 29%. Rising atmospheric CO2 and declining transpiration promote flooding, which handicaps lowland cultivation and renders irrelevant insurance and zoning concepts such as the 100-year flood.
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来源期刊
GSA Today
GSA Today Earth and Planetary Sciences-Geology
CiteScore
4.90
自引率
0.00%
发文量
20
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