4.7 Article

Regional air-sea fluxes of anthropogenic carbon inferred with an Ensemble Kalman Filter

期刊

GLOBAL BIOGEOCHEMICAL CYCLES
卷 23, 期 -, 页码 -

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2008GB003247

关键词

-

资金

  1. European Union through the Integrated Project CarboOcean [511106-2]
  2. Swiss National Science Foundation
  3. Swiss Staatsekretariat fur Bildung und Forschung [C07.0068
  4. COST Action 735]

向作者/读者索取更多资源

Regional air-sea fluxes, ocean transport, and storage of anthropogenic carbon (C-anth) are quantified. Observation-based Canth data from the ocean interior are assimilated into the Bern3D dynamic ocean model using an Ensemble Kalman Filter. Global uptake of Canth is estimated to be 131 +/- 18 GtC over the period 1770 to 2000. Uncertainties from systematic biases in the reconstruction of Canth are assessed by assimilating data from four global and six Atlantic reconstructions and found to be comparable or larger than uncertainties from ocean transport. Aggregated fluxes for the southern high-latitude, tropical and midlatitude, and northern high-latitude ocean agree within 0.11 GtC a(-1) for the two reconstructions with the highest skill score, whereas regional uptake rates are up to a factor of three different. Results indicate that uptake and regional partitioning of anthropogenic carbon in the Southern Ocean remains uncertain.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.7
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

Article Geosciences, Multidisciplinary

A climate database with varying drought-heat signatures for climate impact modelling

Elisabeth Tschumi, Sebastian Lienert, Karin van Der Wiel, Fortunat Joos, Jakob Zscheischler

Summary: This study presents six climate scenarios with varying drought-heat signatures to investigate their impacts on vegetation and the terrestrial carbon cycle. These scenarios show moderate differences in global mean climate without any long-term trends. The research findings may be useful for understanding the differential impacts of droughts and heatwaves in various other areas.

GEOSCIENCE DATA JOURNAL (2022)

Article Environmental Sciences

Radiocarbon in the Land and Ocean Components of the Community Earth System Model

Tobias Frischknecht, Altug Ekici, Fortunat Joos

Summary: Large amounts of C-14 isotopes were released into the atmosphere during atomic bomb tests in the 1950s and 1960s, affecting the carbon cycle. Land component simulations showed a mismatch with observed C-14 uptake, suggesting biases in forest productivity or carbon allocation. Ocean component simulations matched observations, but indicated slow deep ocean ventilation, causing biases in biogeochemical tracers and global warming projections. This study highlights the importance of C-14 observations for improving representations of carbon fluxes and transport timescales in Earth system models.

GLOBAL BIOGEOCHEMICAL CYCLES (2022)

Article Environmental Sciences

What Controls the Large-Scale Efficiency of Carbon Transfer Through the Ocean's Mesopelagic Zone? Insights From a New, Mechanistic Model (MSPACMAM)

Ashley Dinauer, Charlotte Laufkoetter, Scott C. Doney, Fortunat Joos

Summary: A new and cost-efficient model is proposed in this paper to simulate the penetration of sinking particulate organic carbon (POC) into the ocean interior. The model considers various factors such as particle size, density, dissolved oxygen, and seawater temperature, to explicitly represent the gravitational settling and removal/transformation processes. The model shows good agreement with observed POC flux attenuation in the North Atlantic and North Pacific, and reveals that high latitudes exhibit higher transfer efficiencies compared to low latitudes due to the abundance of large-sized, rapidly sinking particles and slower rate of remineralization.

GLOBAL BIOGEOCHEMICAL CYCLES (2022)

Article Environmental Sciences

Ocean acidification in emission-driven temperature stabilization scenarios: the role of TCRE and non-CO2 greenhouse gases

Jens Terhaar, Thomas L. Froelicher, Fortunat Joos

Summary: Future ocean acidification depends on continuous ocean uptake of CO2, which is influenced by climate policies. Traditional climate models have low uncertainties in projected acidification but high uncertainties in global warming. Converging climate simulations to given temperature levels reveals that uncertainties in acidification are much larger than reported, and are dominated by the reduction of non-CO2 greenhouse gases and TCRE.

ENVIRONMENTAL RESEARCH LETTERS (2023)

Article Environmental Sciences

Adaptive emission reduction approach to reach any global warming target

Jens Terhaar, Thomas L. Frolicher, Mathias T. Aschwanden, Pierre Friedlingstein, Fortunat Joos

Summary: This study proposes an adaptive approach based on past observations to quantify global emissions reductions and achieve temperature targets, demonstrating its robustness against uncertainties.

NATURE CLIMATE CHANGE (2022)

Article Environmental Sciences

Underestimated Interannual Variability of Terrestrial Vegetation Production by Terrestrial Ecosystem Models

Shangrong Lin, Zhongmin Hu, Yingping Wang, Xiuzhi Chen, Bin He, Zhaoliang Song, Shaobo Sun, Chaoyang Wu, Yi Zheng, Xiaosheng Xia, Liyang Liu, Jing Tang, Qing Sun, Fortunat Joos, Wenping Yuan

Summary: This study found that current TEMs substantially underestimate the interannual variability (IAV) of GPP, especially in nonforest ecosystem types. One possible cause is that the models underestimate the changes of canopy physiology responding to climate change. The differences between the simulated and observed interannual variations of leaf area index (LAI) also contribute to the underestimation of IAV.

GLOBAL BIOGEOCHEMICAL CYCLES (2023)

Article Biodiversity Conservation

Observational constraints reduce model spread but not uncertainty in global wetland methane emission estimates

Kuang-Yu Chang, William J. Riley, Nathan Collier, Gavin McNicol, Etienne Fluet-Chouinard, Sara H. Knox, Kyle B. Delwiche, Robert B. Jackson, Benjamin Poulter, Marielle Saunois, Naveen Chandra, Nicola Gedney, Misa Ishizawa, Akihiko Ito, Fortunat Joos, Thomas Kleinen, Federico Maggi, Joe McNorton, Joe R. Melton, Paul Miller, Yosuke Niwa, Chiara Pasut, Prabir K. Patra, Changhui Peng, Sushi Peng, Arjo Segers, Hanqin Tian, Aki Tsuruta, Yuanzhi Yao, Yi Yin, Wenxin Zhang, Zhen Zhang, Qing Zhu, Qiuan Zhu, Qianlai Zhuang

Summary: The recent rise in atmospheric methane concentrations has negative effects on climate change and mitigation efforts. Estimates of global wetland methane emissions vary widely among different approaches, but using better-performing models can reduce the spread of these estimates. However, discrepancies in the estimates increase when using the top 20% models. It is important to expand benchmark sites to account for environmental variability and encourage the development of wetland methane models to focus on site-specific and ecosystem-specific variabilities.

GLOBAL CHANGE BIOLOGY (2023)

Article Geosciences, Multidisciplinary

Multi-proxy constraints on Atlantic circulation dynamics since the last ice age

Frerk Poppelmeier, Aurich Jeltsch-Thommes, Joerg Lippold, Fortunat Joos, Thomas F. Stocker

Summary: According to a reassessment of proxy records and model simulations, the Atlantic meridional overturning circulation was shallow and weak during the Last Glacial Maximum, and it took time for water masses to adjust to circulation shifts during the Last Deglaciation. However, uncertainties still exist in understanding the Atlantic circulation and its response to external perturbations.

NATURE GEOSCIENCE (2023)

Article Environmental Sciences

Large Variability in Simulated Response of Vegetation Composition and Carbon Dynamics to Variations in Drought-Heat Occurrence

Elisabeth Tschumi, Sebastian Lienert, Ana Bastos, Philippe Ciais, Konstantin Gregor, Fortunat Joos, Juergen Knauer, Philip Papastefanou, Anja Rammig, Karin van der Wiel, Karina Williams, Yidi Xu, Soenke Zaehle, Jakob Zscheischler

Summary: The frequency of heatwaves and droughts vary greatly in different climate models. Understanding the response of vegetation models to different climate conditions during these extreme events is important. Previous work has developed six different climate scenarios to study the effects of single and compound extremes on vegetation and carbon dynamics. Using these scenarios, six global vegetation models were tested, and the results showed significant variation in their responses. The findings highlight the need to improve the representation of compound events in climate models to reduce uncertainties in future carbon cycle projections.

JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES (2023)

Article Geosciences, Multidisciplinary

Carbon Cycle Responses to Changes in Weathering and the Long-Term Fate of Stable Carbon Isotopes

A. Jeltsch-Thoemmes, F. Joos

Summary: The causes of CO2 variations over the past million years are still not well understood. Imbalances between rock weathering input and the removal of elements from the atmosphere-ocean-biosphere system likely play a role in these changes. Our study shows that carbon-climate responses reach equilibrium within tens of thousands of years, but several hundred thousand years are required for carbon isotope ratio equilibrium. Changes in dissolved CO2 affect carbon isotope fractionation and burial flux, highlighting the significant impact of weathering-burial imbalances.

PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY (2023)

Article Geosciences, Multidisciplinary

Anthropogenic Attribution of the Increasing Seasonal Amplitude in Surface Ocean pCO2

Fortunat Joos, Angelique Hameau, Thomas L. Frolicher, David B. Stephenson

Summary: This study analyzes historical climate simulations to determine the cause of the positive trend in the seasonal amplitude of surface ocean pCO(2) and finds evidence of anthropogenic forcing. The results indicate that the trends in mid-latitudes are attributable to human activities, while no trends are detected in the tropics and the Southern Ocean.

GEOPHYSICAL RESEARCH LETTERS (2023)

Article Geosciences, Multidisciplinary

Cold-Season Methane Fluxes Simulated by GCP-CH4 Models

A. Ito, T. Li, Z. Qin, J. R. Melton, H. Tian, T. Kleinen, W. Zhang, Z. Zhang, F. Joos, P. Ciais, P. O. Hopcroft, D. J. Beerling, X. Liu, Q. Zhuang, Q. Zhu, C. Peng, K. -Y Chang, E. Fluet-Chouinard, G. McNicol, P. Patra, B. Poulter, S. Sitch, W. Riley

Summary: The cold-season methane emissions in wetland models are poorly constrained. We evaluated 16 models participating in the Global Carbon Project model intercomparison and found that they underestimated the cold-season methane emissions, especially during the months with subzero air temperatures. However, due to winter warming, the contribution of cold-season emissions is expected to increase. There is a need for model refinement, as the variability among models suggests different parameterizations of processes.

GEOPHYSICAL RESEARCH LETTERS (2023)

Article Geosciences, Multidisciplinary

Evaluating nitrogen cycling in terrestrial biosphere models: a disconnect between the carbon and nitrogen cycles

Sian Kou-Giesbrecht, Vivek K. Arora, Christian Seiler, Almut Arneth, Stefanie Falk, Atul K. Jain, Fortunat Joos, Daniel Kennedy, Jurgen Knauer, Stephen Sitch, Michael O'Sullivan, Naiqing Pan, Qing Sun, Hanqin Tian, Nicolas Vuichard, Sonke Zaehle

Summary: Terrestrial carbon (C) sequestration is limited by nitrogen (N), an empirically established constraint that could intensify under CO2 fertilization and future global change. The ability of terrestrial biosphere models to reproduce observations of nitrogen (N) cycling and its regulation of terrestrial C sequestration has been largely unexplored. Our evaluation of an ensemble of terrestrial biosphere models reveals significant variability in the simulation of N cycling, indicating that the processes regulating terrestrial C sequestration operate differently across models and are uncoupled from the simulation of C cycling. The overestimation of C storage per unit N suggests biases in projections of the future terrestrial C sink under CO2 fertilization and future global change.

EARTH SYSTEM DYNAMICS (2023)

Article Ecology

Observation-constrained estimates of the global ocean carbon sink from Earth system models

Jens Terhaar, Thomas L. Frolicher, Fortunat Joos

Summary: The ocean plays a significant role in slowing down global warming by absorbing CO2 emissions. However, estimates of ocean anthropogenic carbon uptake vary. In this study, the researchers found that the ocean carbon sink can be constrained by specific physical and biogeochemical parameters. By using these constraints with observations, they provided a new estimate of the global ocean anthropogenic carbon sink, which is larger than previously estimated. This constraint also reduces uncertainties in past, present, and future ocean carbon sink estimates, enhancing our understanding of the global carbon cycle and guiding climate and ocean policies.

BIOGEOSCIENCES (2022)

Article Ecology

The effects of varying drought-heat signatures on terrestrial carbon dynamics and vegetation composition

Elisabeth Tschumi, Sebastian Lienert, Karin van der Wiel, Fortunat Joos, Jakob Zscheischler

Summary: This study examines the effects of different drought-heat climate scenarios on vegetation distribution and land carbon dynamics. The findings show that climate without extreme events increases tree coverage and ecosystem productivity, while more heatwaves lead to increased tree coverage in higher latitudes. Drought and particularly hot-dry scenarios reduce tree coverage and ecosystem productivity. The study highlights the importance of correctly simulating compound extremes for future impact assessment.

BIOGEOSCIENCES (2022)

暂无数据