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            聯系我們 英文版

            Luncheon Seminar #151: Ocean biogeochemistry with ECCO and Darwin

            時間:2019年06月26日 00:00

            來源:

            瀏覽:

            時 間:2019-7-1 (星期一) 1:00pm-2:00pm

            主 講:Dimitris Menemenlis,Research Scientist

            地 點:周隆泉樓A3-206 A3-206 Zhou Long Quan Building

            【來訪單位 Institution】:California Institute of Technology,USA    

            【邀請人 Host】:劉志宇  Zhiyu Liu      【聯絡人 Contact】:黃迎   Ying Huang 2181571

            Abstract

            Quantifying variability in the ocean CO2 sink remains problematic due to sparse observations and large spatiotemporal variability in surface-ocean p CO2. To address this challenge, we have developed a global ocean biogeochemistry model called ECCO-Darwin that is constrained by both physical and biogeochemical observations. The model is based on a physical ocean data synthesis provided by the Estimating the Circulation and Climate of the Ocean (ECCO) and on an ecological model provided by the Darwin project. A Green’s Function approach is used to adjust a small number (six) of empirical parameters and initial conditions for the biogeochemical component of the model. We compare ECCO-Darwin global and biome-scale air-sea CO2 fluxes to a suite of interpolation-based products over seasonal to multi-decadal timescales (1995–2017). ECCO-Darwin produces air-sea CO2 fluxes that exhibit broad-scale consistency with the interpolation-based products in many biomes, particularly in the subtropical and equatorial regions. The largest differences between estimates in long-term ocean CO2 uptake occur in subpolar seasonally-stratified biomes, where ECCO-Darwin produces stronger winter uptake. Compared to the Global Carbon Project (GCP) ocean biogeochemistry models, ECCO-Darwin has global CO2 sink (time-mean of -2.52 +/- 0.49 Pg C / yr) and interannual variability that is more consistent with the interpolation-based products. Contrary to interpolation-based products, ECCO-Darwin is less sensitive to sparse and uneven observational sampling and it permits full attribution of the inferred air-sea CO2 flux spatiotemporal variability.

            Bio

            Dr. Dimitris Menemenlis is a research scientist at the Jet Propulsion Laboratory, California Institute of Technology with over 25 years of experience working with ocean circulation models and state estimation technology.  He is a developer of the Massachusetts Institute of Technology general circulation model (MITgcm) and a contributor to the Estimating the Circulation and Climate of the Oceans (ECCO) and Carbon Monitoring System Flux (CMS-Flux) projects.


            上一篇: Luncheon Seminar #150: Why is there a major (~1,000 km long) mud belt system on the inner shelf along the energetic Zhi-Min Coast? 下一篇: 聆海文化沙龍第一講:地球系統中的湍流現象 —— 從細菌的主動運動到青藏高原的地表變形

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