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DOI | 10.1002/2017GL075123 |
Using Noble Gas Measurements to Derive Air-Sea Process Information and Predict Physical Gas Saturations | |
Hamme, Roberta C.1; Emerson, Steven R.2; Severinghaus, Jeffrey P.3; Long, Matthew C.4; Yashayaev, Igor5 | |
2017-10-16 | |
发表期刊 | GEOPHYSICAL RESEARCH LETTERS |
ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2017 |
卷号 | 44期号:19 |
文章类型 | Article |
语种 | 英语 |
国家 | Canada; USA |
英文摘要 | Dissolved gas distributions are important because they influence oceanic habitats and Earth's climate, yet competing controls by biology and physics make gas distributions challenging to predict. Bubble-mediated gas exchange, temperature change, and varying atmospheric pressure all push gases away from equilibrium. Here we use new noble gas measurements from the Labrador Sea to demonstrate a technique to quantify physical processes. Our analysis shows that water-mass formation can be represented by a quasi steady state in which bubble fluxes and cooling push gases away from equilibrium balanced by diffusive gas exchange forcing gases toward equilibrium. We quantify the rates of these physical processes from our measurements, allowing direct comparison to gas exchange parameterizations, and predict the physically driven saturation of other gases. This technique produces predictions that reasonably match N-2/Ar observations and demonstrates that physical processes should force SF6 to be approximate to 6% more supersaturated than CFC-11 and CFC-12, impacting ventilation age calculations. Plain Language Summary Gases dissolved in the ocean are important because they influence oceanic habitats and Earth's climate. Physics and biology combine to control the amounts of gases like carbon dioxide, oxygen, and nitrogen in the ocean. Our research seeks to disentangle and quantify the competing effects of physics and biology on dissolved gases. We present very precise measurements of dissolved noble gas concentrations (neon, argon, and krypton) in the Labrador Sea, one of the few places on Earth where the surface and deep ocean communicate with each other. Because noble gases have no biological function, responding only to physical processes in the ocean, we use these measurements to discover the amounts of physical processes that affect gases during the winter at this site, like rapid cooling of the water or bubbles injected by breaking waves. From these amounts of physical processes, we calculate the concentrations of nitrogen and chlorofluorocarbons if only physical processes affected these gases. Our work will allow oceanographers to better estimate the rate that bioavailable nutrients are being removed from the ocean (a process that biologically creates nitrogen gas) and to better determine how the ocean moves from observations of changing chlorofluorocarbons in the ocean. |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000413921300043 |
WOS关键词 | LABRADOR SEA ; EXCESS HELIUM ; WATER ; OCEAN ; SOLUBILITY ; EXCHANGE ; NITROGEN ; IMPACT ; TRACER ; CCSM4 |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/28323 |
专题 | 气候变化 |
作者单位 | 1.Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC, Canada; 2.Univ Washington, Sch Oceanog, Seattle, WA 98195 USA; 3.Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA; 4.Natl Ctr Atmospher Res, Climate & Global Dynam Div, POB 3000, Boulder, CO 80307 USA; 5.Bedford Inst Oceanog, Fisheries & Oceans Canada, Dartmouth, NS, Canada |
推荐引用方式 GB/T 7714 | Hamme, Roberta C.,Emerson, Steven R.,Severinghaus, Jeffrey P.,et al. Using Noble Gas Measurements to Derive Air-Sea Process Information and Predict Physical Gas Saturations[J]. GEOPHYSICAL RESEARCH LETTERS,2017,44(19). |
APA | Hamme, Roberta C.,Emerson, Steven R.,Severinghaus, Jeffrey P.,Long, Matthew C.,&Yashayaev, Igor.(2017).Using Noble Gas Measurements to Derive Air-Sea Process Information and Predict Physical Gas Saturations.GEOPHYSICAL RESEARCH LETTERS,44(19). |
MLA | Hamme, Roberta C.,et al."Using Noble Gas Measurements to Derive Air-Sea Process Information and Predict Physical Gas Saturations".GEOPHYSICAL RESEARCH LETTERS 44.19(2017). |
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