4.7 Article

Measurements and modeling of contemporary radiocarbon in the stratosphere

期刊

GEOPHYSICAL RESEARCH LETTERS
卷 43, 期 3, 页码 1399-1406

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GL066921

关键词

radiocarbon; stratosphere; stratosphere-troposphere exchange; carbon cycle; cosmogenic radionuclides; carbon dioxide

资金

  1. NASA UARP [NNX13AH10G, NNX09AJ95G, NNX13AH20G, NNX12AH02G]
  2. UC [LF-09-118804]
  3. UC IGPP/LLNL [07-GS-019]
  4. NOAA Climate Program Office [NA05OAR4311166]
  5. Lawrence Scholar's Program
  6. U.S. Department of Energy by Lawrence Livermore National Laboratory [W-7405-Eng-48, DE-AC52-07NA27344]
  7. NASA [NNX09AJ95G, 114649, NNX13AH10G, 474047, NNX12AH02G, 19686, NNX13AH20G, 473711] Funding Source: Federal RePORTER

向作者/读者索取更多资源

\ Measurements of the C-14 content of carbon dioxide in air collected by high-altitude balloon flights in 2003-2005 reveal the contemporary radiocarbon distribution in the northern midlatitude stratosphere, four decades after the Limited Test Ban Treaty restricted atmospheric testing of nuclear weapons. Comparisons with results from a 3-D chemical-transport model show that the (CO2)-C-14 distribution is now largely governed by the altitude/latitude dependence of the natural cosmogenic production rate, stratospheric transport, and propagation into the stratosphere of the decreasing radiocarbon trend in tropospheric CO2 due to fossil fuel combustion. From the observed correlation of (CO2)-C-14 with N2O mixing ratios, an annual global mean net flux of (CO2)-C-14 to the troposphere of 1.6(0.4)x10(17)molCO(2)yr(-1) and a global production rate of 2.2(0.6)x10(26) atoms(14)Cyr(-1) are empirically derived. The results also indicate that contemporary (CO2)-C-14 observations provide highly sensitive diagnostics for stratospheric transport and residence times in models.

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