Using Global-Scale Earth System Models for Regional Fisheries Applications

被引:23
|
作者
Kearney, Kelly A. A. [1 ,2 ]
Bograd, Steven J. J. [3 ]
Drenkard, Elizabeth [4 ]
Gomez, Fabian A. A. [5 ,6 ]
Haltuch, Melissa [7 ]
Hermann, Albert J. J. [1 ]
Jacox, Michael G. G. [3 ,8 ,9 ]
Kaplan, Isaac C. C. [7 ]
Koenigstein, Stefan [3 ,10 ]
Luo, Jessica Y. Y.
Masi, Michelle [11 ]
Muhling, Barbara [3 ,10 ]
Buil, Mercedes Pozo [3 ,10 ]
Woodworth-Jefcoats, Phoebe A. A. [12 ]
机构
[1] Univ Washington, JISAO, CICOES, Seattle, WA 98195 USA
[2] NOAA Alaska Fisheries Sci Ctr, Seattle, WA 98115 USA
[3] NOAA Southwest Fisheries Sci Ctr Monterey & La Jo, Los Angeles, CA USA
[4] NOAA Geophys Fluid Dynam Lab, Princeton, NJ USA
[5] Mississippi State Univ, Northern Gulf Inst, Stennis Space Ctr, Starkville, MS USA
[6] NOAA Atlantic Oceanog & Meteorol Lab, Miami, FL USA
[7] NOAA Northwest Fisheries Sci Ctr, Seattle, WA USA
[8] NOAA Pacific Marine Environm Lab, Seattle, WA USA
[9] NOAA Earth Syst Res Lab, Boulder, CO USA
[10] Univ Calif Santa Cruz, Inst Marine Studies, Santa Cruz, CA USA
[11] NOAA Southeast Fisheries Sci Ctr, Galveston Lab, Galveston, TX USA
[12] NOAA Pacific Islands Fisheries Sci Ctr, Honolulu, HI USA
关键词
living marine resources; earth system models; modeling; primary production; biogeochemistry; CMIP6; climate change; GULF-OF-MEXICO; OCEAN BIOGEOCHEMICAL MODEL; FRESH-WATER DISCHARGE; CLIMATE-CHANGE; NORTHERN GULF; 21ST-CENTURY PROJECTIONS; PHYTOPLANKTON GROWTH; FUNCTIONAL-RESPONSES; NATURAL ASSEMBLAGES; MARINE ECOSYSTEMS;
D O I
10.3389/fmars.2021.622206
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Climate change may impact ocean ecosystems through a number of mechanisms, including shifts in primary productivity or plankton community structure, ocean acidification, and deoxygenation. These processes can be simulated with global Earth system models (ESMs), which are increasingly being used in the context of fisheries management and other living marine resource (LMR) applications. However, projections of LMR-relevant metrics such as net primary production can vary widely between ESMs, even under identical climate scenarios. Therefore, the use of ESM should be accompanied by an understanding of the structural differences in the biogeochemical sub-models within ESMs that may give rise to these differences. This review article provides a brief overview of some of the most prominent differences among the most recent generation of ESM and how they are relevant to LMR application.</p>
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页数:27
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