Isotopic and micrometeorological ocean CO2 fluxes: Different time and space scales
Isotopic and micrometeorological ocean CO2 fluxes: Different time and space scales
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同位素和微气象海洋二氧化碳通量：不同的时间和空间尺度
DOI：
10.1029/jc091ic09p10529
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发表时间：
1986
影响因子：
--
通讯作者：
E. Jones
中科院分区：
文献类型：
--
作者：
Stuart D. Smith;E. Jones
对Smith和Jones（1985）的CO2涡动通量测量的解释的澄清是在Broecker等人的批评的背景下提供的（本期）。向下泵送二氧化碳和其他大气成分的空气夹带破碎波加压被认为是一个合理的机制。短期“涡流通量”表面交换率和长期同位素测定之间的明显差异可以解决，如果短期存储的溶解气体在上层水被认为是只影响前者。
Clarifications of the interpretation of the CO2 eddy flux measurements of Smith and Jones (1985) are offered in the context of criticisms by Broecker et al. (this issue). Downward pumping of CO2 and other atmospheric constituents by the pressurization of air entrained by breaking waves is considered to be a plausible mechanism. Apparent discrepancies between short-term “eddy flux” surface exchange rates and longer-term isotopic determinations can be resolved if short-term storage of dissolved gas in upper water layers is considered to influence only the former.