Dynamically downscaled projections of ocean acidification for the Bering Sea

被引:20
作者
Pilcher, D. J. [1 ,2 ]
Cross, J. N.
Hermann, A. J. [1 ,2 ]
Kearney, K. A. [1 ,3 ]
Cheng, W. [1 ,2 ]
Mathis, J. T. [4 ]
机构
[1] Univ Washington, Joint Inst Study, Atmosphere & Ocean, Seattle, WA 98195 USA
[2] NOAA Pacific Marine Environm Lab, Seattle, WA USA
[3] NOAA Alaska Fisheries Sci Ctr, Seattle, WA USA
[4] Georgetown Univ, Sch Foreign Serv, Washington, DC USA
关键词
Bering sea; Dynamical downscaling; Regional modeling; Ocean acidification; ARCTIC-OCEAN; ANTHROPOGENIC CO2; 21ST-CENTURY PROJECTIONS; HIGH-LATITUDES; CLIMATE-CHANGE; CARBONIC-ACID; FRESH-WATER; MODEL; SYSTEM; SEAWATER;
D O I
10.1016/j.dsr2.2022.105055
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
A regional ocean biogeochemical model for the Bering Sea is used to dynamically downscale three Earth System Models from the CMIP5 archive under the RCP 8.5 and RCP 4.5 scenarios. These continuous model runs, completed in conjunction with the Alaska Climate Integrated Modeling Project (ACLIM), span the 2006-2100 timeframe and project continued warming, freshening, and ocean acidification (OA) for the Bering Sea shelf region over the 21st Century, with larger magnitude changes in the RCP 8.5 scenario. The downscaled projections suggest that annual average surface seawater aragonite saturation state (Omega(arag)) for the Bering Sea shelf will decrease by 0.63-0.86 under RCP 8.5 and 0.18-0.43 under RCP 4.5 by 2100. Surface pH values decrease by 0.31-0.35 under RCP 8.5 and 0.07-0.13 under RCP 4.5. Seasonally, Omega(arag) < 1 conditions start to emerge for similar to 2 months per year during winter between 2015 and 2030 under both climate change scenarios. Under RCP 8.5, the duration of these undersaturated conditions grows to similar to 5 months per year by 2100, occurring from mid-October through mid-March. Under RCP 4.5, these conditions remain constrained to 2-3 months per year by 2100. In both scenarios, summer months maintain conditions of Omega(arag) > 1 due to primary productivity, though the maximum in Omega(arag) is greatly reduced under RCP 8.5. Spatially, the regions of greatest pH and Omega(arag) decline are the southeastern Bering Sea shelf and the outer shelf domain near the shelf break. Linear trends in carbonate variables between our downscaled simulations and the Earth System Model (ESM) output are comparable and indistinguishable compared to the model spread. However, bottom water trends differ somewhat between the ESM and our downscaled simulations, with the latter more consistently resolving the different shelf domains. The OA information provided by these downscaled simulations can help inform biological sensitivity experiments and longterm strategic planning for marine fisheries management.
引用
收藏
页数:15
相关论文
共 88 条
[1]  
[Anonymous], 2010, ARCTIC RIVER BIOGEOC
[2]   Continued increases in Arctic Ocean primary production [J].
Arrigo, Kevin R. ;
van Dijken, Gert L. .
PROGRESS IN OCEANOGRAPHY, 2015, 136 :60-70
[3]  
Askren D.R., 1972, THESIS U WASH SEATTL, P104
[4]   Integrated Assessment of Ocean Acidification Risks to Pteropods in the Northern High Latitudes: Regional Comparison of Exposure, Sensitivity and Adaptive Capacity [J].
Bednarsek, Nina ;
Naish, Kerry-Ann ;
Feely, Richard A. ;
Hauri, Claudine ;
Kimoto, Katsunori ;
Hermann, Albert J. ;
Michel, Christine ;
Niemi, Andrea ;
Pilcher, Darren .
FRONTIERS IN MARINE SCIENCE, 2021, 8
[5]   Multiple stressors of ocean ecosystems in the 21st century: projections with CMIP5 models [J].
Bopp, L. ;
Resplandy, L. ;
Orr, J. C. ;
Doney, S. C. ;
Dunne, J. P. ;
Gehlen, M. ;
Halloran, P. ;
Heinze, C. ;
Ilyina, T. ;
Seferian, R. ;
Tjiputra, J. ;
Vichi, M. .
BIOGEOSCIENCES, 2013, 10 (10) :6225-6245
[6]   Arctic Ocean Freshwater Dynamics: Transient Response to Increasing River Runoff and Precipitation [J].
Brown, Nicola Jane ;
Nilsson, Johan ;
Pemberton, Per .
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS, 2019, 124 (07) :5205-5219
[7]   Eastern Bering Sea shelf environmental and lower trophic level responses to climate forcing: Results of dynamical downscaling from CMIP6 [J].
Cheng, Wei ;
Hermann, Albert J. ;
Hollowed, Anne B. ;
Holsman, Kirstin K. ;
Kearney, Kelly A. ;
Pilcher, Darren J. ;
Stock, Charles A. ;
Aydin, Kerim Y. .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2021, 193
[8]   Calcium carbonate saturation in the surface water of the Arctic Ocean: undersaturation in freshwater influenced shelves [J].
Chierici, M. ;
Fransson, A. .
BIOGEOSCIENCES, 2009, 6 (11) :2421-2431
[9]   CIRCULATION, WATER MASSES, AND FLUXES ON THE SOUTHEASTERN BERING SEA SHELF [J].
COACHMAN, LK .
CONTINENTAL SHELF RESEARCH, 1986, 5 (1-2) :23-108
[10]   Conservative and non-conservative variations of total alkalinity on the southeastern Bering Sea shelf [J].
Cross, Jessica N. ;
Mathis, Jeremy T. ;
Bates, Nicholas R. ;
Byrne, Robert H. .
MARINE CHEMISTRY, 2013, 154 :100-112