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DOI | 10.1002/2017GB005753 |
Dynamic Biological Functioning Important for Simulating and Stabilizing Ocean Biogeochemistry | |
Buchanan P.J.; Matear R.J.; Chase Z.; Phipps S.J.; Bindoff N.L. | |
发表日期 | 2018 |
ISSN | 0886-6236 |
EISSN | 1944-9224 |
起始页码 | 565 |
结束页码 | 593 |
卷号 | 32期号:4 |
英文摘要 | The biogeochemistry of the ocean exerts a strong influence on the climate by modulating atmospheric greenhouse gases. In turn, ocean biogeochemistry depends on numerous physical and biological processes that change over space and time. Accurately simulating these processes is fundamental for accurately simulating the ocean's role within the climate. However, our simulation of these processes is often simplistic, despite a growing understanding of underlying biological dynamics. Here we explore how new parameterizations of biological processes affect simulated biogeochemical properties in a global ocean model. We combine 6 different physical realizations with 6 different biogeochemical parameterizations (36 unique ocean states). The biogeochemical parameterizations, all previously published, aim to more accurately represent the response of ocean biology to changing physical conditions. We make three major findings. First, oxygen, carbon, alkalinity, and phosphate fields are more sensitive to changes in the ocean's physical state. Only nitrate is more sensitive to changes in biological processes, and we suggest that assessment protocols for ocean biogeochemical models formally include the marine nitrogen cycle to assess their performance. Second, we show that dynamic variations in the production, remineralization, and stoichiometry of organic matter in response to changing environmental conditions benefit the simulation of ocean biogeochemistry. Third, dynamic biological functioning reduces the sensitivity of biogeochemical properties to physical change. Carbon and nitrogen inventories were 50% and 20% less sensitive to physical changes, respectively, in simulations that incorporated dynamic biological functioning. These results highlight the importance of a dynamic biology for ocean properties and climate. ©2018. American Geophysical Union. All Rights Reserved. |
英文关键词 | carbon cycle; carbon dioxide; climate change; marine ecosystem; nitrogen cycle; phytoplankton |
语种 | 英语 |
scopus关键词 | biogeochemistry; carbon cycle; carbon dioxide; climate change; environmental conditions; global ocean; marine ecosystem; model; nitrogen cycle; parameterization; phytoplankton; simulation |
来源期刊 | Global Biogeochemical Cycles
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/129842 |
作者单位 | Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, TAS, Australia; CSIRO Oceans and Atmosphere, CSIRO Marine Laboratories, Hobart, TAS, Australia; ARC Centre of Excellence in Climate System Science, University of Tasmania, Hobart, TAS, Australia; Antarctic Climate and Ecosystems Cooperative Research Centre, University of Tasmania, Hobart, TAS, Australia |
推荐引用方式 GB/T 7714 | Buchanan P.J.,Matear R.J.,Chase Z.,et al. Dynamic Biological Functioning Important for Simulating and Stabilizing Ocean Biogeochemistry[J],2018,32(4). |
APA | Buchanan P.J.,Matear R.J.,Chase Z.,Phipps S.J.,&Bindoff N.L..(2018).Dynamic Biological Functioning Important for Simulating and Stabilizing Ocean Biogeochemistry.Global Biogeochemical Cycles,32(4). |
MLA | Buchanan P.J.,et al."Dynamic Biological Functioning Important for Simulating and Stabilizing Ocean Biogeochemistry".Global Biogeochemical Cycles 32.4(2018). |
条目包含的文件 | 条目无相关文件。 |
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