JpGU-AGU Joint Meeting 2017

講演情報

[EE] 口頭発表

セッション記号 A (大気水圏科学) » A-OS 海洋科学・海洋環境

[A-OS14] [EE] Marine ecosystems and biogeochemical cycles: theory, observation and modeling

2017年5月22日(月) 15:30 〜 17:00 303 (国際会議場 3F)

コンビーナ:平田 貴文(北海道大学地球環境科学研究院)、伊藤 進一(東京大学大気海洋研究所)、Eileen E Hofmann(Old Dominion University)、Enrique N Curchitser(Rutgers University New Brunswick)、座長:伊藤 進一(東京大学大気海洋研究所)、座長:平田 貴文(北海道大学)

16:30 〜 16:45

[AOS14-15] Biogeochemical implications of potential future changes in shelf sea circulation

*Jason T Holt1Sarah Wakelin1Yuri Artioli2James Harle1Jeff Polton1Momme Butenschon2John Siddorn3Enda O'Dea3Jerry Blackford2Icarus Allen2 (1.National Oceanography Centre, Liverpool、2.Plymouth Marine Laboratory、3.Met Office)

キーワード:Climate impacts, Shelf sea ecosystems, Ocean shelf coupling

Simulations of the NEMO-ERSEM Atlantic Margin Model (AMM7) of the NW European continental shelf driven by climate models out to 2100 have shown the potential for substantial changes to the ocean-shelf exchange and shelf scale circulation, drawing on simulations from the ROAM and RECICLE projects. In one realisation of future conditions the inflows into the North Sea through the Fair Isle channel and east of Shetland are found to substantially decrease, and the Shetland shelf current largely by-passes the North Sea. This significantly reduces the cyclonic North Sea circulation and shifts the balance between oceanic and terrestrial influence in this region, seen by a substantial decrease in salinity. In this presentation we consider what the biogeochemical implications of this might be. Using output from the ERSEM model in this simulation, we explore the spatial distribution of these changes and consequent changes in nutrient ratios, and other factors in play that may mitigate or aggravate this view (Holt et al 2016). We use the driving ¼o global NEMO model (Yool et al 2015) to explore whether other semi-enclosed shelf sea basins around the world might show similar behaviour under this future scenario. The long-term nutrient budgets in shelf-seas are set by the relative balance of oceanic and riverine inputs, augmented by atmospheric inputs and modulated by exchanges between benthic and pelagic systems. A simple mixing box estimate suggests that in the North Sea case, this change in circulation leads to an increase in nitrate by 15% and the flushing time increases from 1.8 years to 2.5 years; this potentially mitigates against the effects of a reduction in oceanic nutrient concentrations being advected on-shelf, which have previously been identified (Holt et al 2012).

Holt, J., Butenschon, M., Wakelin, S.L., Artioli, Y., Allen, J.I., 2012. Oceanic controls on the primary production of the northwest European continental shelf: model experiments under recent past conditions and a potential future scenario. Biogeosciences, 9, 97-117.

Holt, J., Corinna, S., Cannaby, H., Daewel, U., Allen, I., Artioli, Y., Bopp, L., Butenschon, M., Fach, B., Harle, J., Pushpadas, D., Salihoglu, B., Wakelin, S., 2016. Potential impacts of climate change on the primary production of regional seas: a comparative analysis of five European seas Progress in Oceanography, 140, 91-115.

Yool, A., Popova, E.E., Coward, A.C., 2015. Future change in ocean productivity: Is the Arctic the new Atlantic? Journal of Geophysical Research: Oceans, 120, 7771-7790.