7 results on '"Monteiro, Pedro M. S."'
Search Results
2. Southern Ocean phytoplankton dynamics and carbon export: insights from a seasonal cycle approach.
- Author
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Thomalla, Sandy J., Du Plessis, Marcel, Fauchereau, Nicolas, Giddy, Isabelle, Gregor, Luke, Henson, Stephanie, Joubert, Warren R., Little, Hazel, Monteiro, Pedro M. S., Mtshali, Thato, Nicholson, Sarah, Ryan-Keogh, Thomas J., and Swart, Sebastiaan
- Subjects
CARBON cycle ,OCEAN dynamics ,SEASONS ,ATMOSPHERIC models ,REMOTE sensing ,CARBON - Abstract
Quantifying the strength and efficiency of the Southern Ocean biological carbon pump (BCP) and its response to predicted changes in the Earth's climate is fundamental to our ability to predict long-term changes in the global carbon cycle and, by extension, the impact of continued anthropogenic perturbation of atmospheric CO
2 . There is little agreement, however, in climate model projections of the sensitivity of the Southern Ocean BCP to climate change, with a lack of consensus in even the direction of predicted change, highlighting a gap in our understanding of a major planetary carbon flux. In this review, we summarize relevant research that highlights the important role of fine-scale dynamics (both temporal and spatial) that link physical forcing mechanisms to biogeochemical responses that impact the characteristics of the seasonal cycle of phytoplankton and by extension the BCP. This approach highlights the potential for integrating autonomous and remote sensing observations of fine scale dynamics to derive regionally optimized biogeochemical parameterizations for Southern Ocean models. Ongoing development in both the observational and modelling fields will generate new insights into Southern Ocean ecosystem function for improved predictions of the sensitivity of the Southern Ocean BCP to climate change. This article is part of a discussion meeting issue 'Heat and carbon uptake in the Southern Ocean: the state of the art and future priorities'. [ABSTRACT FROM AUTHOR]- Published
- 2023
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3. The IPCC Assessment Report Six Working Group 1 report and southern Africa: Reasons to take action.
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Engelbrecht, Francois A. and Monteiro, Pedro M. S.
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EARTH system science , *PHYSICAL sciences , *CARBON cycle , *ATMOSPHERIC carbon dioxide , *CARBON emissions , *CLIMATE change mitigation , *TROPICAL cyclones - Abstract
The article focuses on the Intergovernmental Panel on Climate Change (IPCC) Assessment Report Six (AR6) Working Group I (WG1) report focus on the assessment of the global climate-carbon system with implications for adaptation and mitigation action in southern Africa. It mentions climate change attribution science is capable of quantifying the role of human influence in the occurrence of individual weather events.
- Published
- 2021
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4. Interannual drivers of the seasonal cycle of CO2 in the Southern Ocean.
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Gregor, Luke, Kok, Schalk, and Monteiro, Pedro M. S.
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CARBON dioxide ,CARBON cycle ,CLIMATE change ,MACHINE learning ,RANDOM forest algorithms - Abstract
Resolving and understanding the drivers of variability of CO
2 in the Southern Ocean and its potential climate feedback is one of the major scientific challenges of the ocean-climate community. Here we use a regional approach on empirical estimates of pCO2 to understand the role that seasonal variability has in long-term CO2 changes in the Southern Ocean. Machine learning has become the preferred empirical modelling tool to interpolate time- and locationrestricted ship measurements of pCO2 . In this study we use an ensemble of three machine-learning products: support vector regression (SVR) and random forest regression (RFR) from Gregor et al. (2017), and the self-organising-map feedforward neural network (SOM-FFN) method from Landschützer et al. (2016). The interpolated estimates of ΔpCO2 are separated into nine regions in the Southern Ocean defined by basin (Indian, Pacific, and Atlantic) and biomes (as defined by Fay and McKinley, 2014a). The regional approach shows that, while there is good agreement in the overall trend of the products, there are periods and regions where the confidence in estimated ΔpCO2 is low due to disagreement between the products. The regional breakdown of the data highlighted the seasonal decoupling of the modes for summer and winter interannual variability. Winter interannual variability had a longer mode of variability compared to summer, which varied on a 4-6-year timescale. We separate the analysis of the ΔpCO2 and its drivers into summer and winter. We find that understanding the variability of ΔpCO2 and its drivers on shorter timescales is critical to resolving the long-term variability of ΔpCO2 . Results show that ΔpCO2 is rarely driven by thermodynamics during winter, but rather by mixing and stratification due to the stronger correlation of ΔpCO2 variability with mixed layer depth. Summer pCO2 variability is consistent with chlorophyll a variability, where higher concentrations of chlorophyll a correspond with lower pCO2 concentrations. In regions of low chlorophyll a concentrations, wind stress and sea surface temperature emerged as stronger drivers of ΔpCO2 . In summary we propose that sub-decadal variability is explained by summer drivers, while winter variability contributes to the long-term changes associated with the SAM. This approach is a useful framework to assess the drivers of ΔpCO2 but would greatly benefit from improved estimates of ΔpCO2 and a longer time series. [ABSTRACT FROM AUTHOR]- Published
- 2018
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5. Mechanisms of the Sea–Air CO2 Flux Seasonal Cycle biases in CMIP5 Earth Systems Models in the Southern Ocean.
- Author
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Precious Mongwe, N., Vichi, Marcello, and Monteiro, Pedro M. S.
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ATMOSPHERIC carbon dioxide ,CARBON dioxide in seawater ,CARBON cycle ,CARBON dioxide solubility ,CLIMATE change ,MARINE ecology - Abstract
The Southern Ocean forms a key component of the global carbon cycle. Recent studies, however, show that CMIP5 Earth System Models (ESM) disagree on the representation of the seasonal cycle of the CO
2 flux (FCO2 ) and compare poorly to observations in the Southern Ocean. This model-observations bias has important implications on the ability of ESMs to predict century scale CO2 sink and related climate feedbacks. In this study, we used a specialized diagnostic analysis on 10 CMIP5 models in the Southern Ocean to discriminate the role of the major drivers, namely the temperature control and the concentration of dissolved inorganic carbon (DIC). Our analysis shows that the FCO2 biases in CMIP5 models cluster in two major groups. Group A models (MPI-ESM-MR, NorESM2 and HadGEM-ES) are characterized by exaggerated primary production such that biologically driven DIC changes mainly regulate the seasonal cycle of FCO2 . Group-B (CMCC-CESM, GFDL-ESM2M, IPSL-CM5A-MR, MRI-ESM, CanESM2, CNRS-CERFACS) overestimates the role of temperature and thus the change in CO2 solubility becomes a dominant driver of FCO2 variability. While CMIP5 models mostly show a singular dominant influence of these two extremes, observations show a modest influence of both, with a dominance of DIC regulation. We found that CMIP5 models overestimate cooling and warming rates during autumn and spring with respect to observations. Because of this, the role of solubility is overestimated, particularly during these seasons (autumn and spring) in group B models, to the extent of contradicting the biological CO2 uptake during spring. Group A does not show this solubility driven bias due to the overestimation of DIC draw down. This finding strongly implies that the inability of the CMIP5 ESMs to resolve CO2 biological uptake during spring might be crucially related to the sensitivity of the pCO2 to temperature in addition to underestimated biological CO2 uptake. [ABSTRACT FROM AUTHOR]- Published
- 2017
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6. High-resolution view of the spring bloom initiation and net community production in the Subantarctic Southern Ocean using glider data.
- Author
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Thomalla, Sandy J., Racault, Marie-Fanny, Swart, Sebastiaan, and Monteiro, Pedro M. S.
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ALGAL blooms ,OCEANOGRAPHIC research ,CLIMATE change ,BIOMASS - Abstract
In the Southern Ocean, there is increasing evidence that seasonal to subseasonal temporal scales, and meso- to submesoscales play an important role in understanding the sensitivity of ocean primary productivity to climate change. This drives the need for a high-resolution approach to resolving biogeochemical processes. In this study, 5.5 months of continuous, high-resolution (3 h, 2 km horizontal resolution) glider data from spring to summer in the Atlantic Subantarctic Zone is used to investigate: (i) the mechanisms that drive bloom initiation and high growth rates in the region and (ii) the seasonal evolution of water column production and respiration. Bloom initiation dates were analysed in the context of upper ocean boundary layer physics highlighting sensitivities of different bloom detection methods to different environmental processes. Model results show that in early spring (September to mid-November) increased rates of net community production (NCP) are strongly affected by meso- to submesoscale features. In late spring/early summer (late-November to mid-December) seasonal shoaling of the mixed layer drives a more spatially homogenous bloom with maximum rates of NCP and chlorophyll biomass. A comparison of biomass accumulation rates with a study in the North Atlantic highlights the sensitivity of phytoplankton growth to fine-scale dynamics and emphasizes the need to sample the ocean at high resolution to accurately resolve phytoplankton phenology and improve our ability to estimate the sensitivity of the biological carbon pump to climate change. [ABSTRACT FROM AUTHOR]
- Published
- 2015
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7. South African carbon observations: CO2 measurements for land, atmosphere and ocean.
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Feig, Gregor T., Joubert, Warren R., Mudau, Azwitamisi E., and Monteiro, Pedro M. S.
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CARBON dioxide , *CLIMATE change , *EMISSIONS (Air pollution) , *SURFACE temperature , *ANTHROPOGENIC effects on nature - Abstract
Carbon dioxide plays a central role in earth's atmospheric, ocean and terrestrial systems.1,2 About 40% of the total anthropogenic emissions since 1750 have remained in the atmosphere, with the balance being removed by the ocean and vegetation sinks.3 Increasing atmospheric CO2 concentrations have been well documented,3 as have widespread impacts on human and natural systems, such as warmer surface temperatures, ocean warming and decreasing pH, loss of ice mass over the cryosphere, increasing global mean sea level, and alterations in the global hydrological cycle.3,4 The impact of increased atmospheric concentrations of CO2 on the biosphere includes shifting species extent, seasonal activities, migration patterns and abundances, as well as changes in species interactions. Monitoring of atmospheric CO2 and other greenhouse gases (GHGs) has been identified as a priority by international agencies, such as the United Nations Framework Convention on Climate Change and government departments that are interested in mitigating the effects of climate change. South Africa has made a commitment to a low carbon future as part of its role in global climate policy instruments through a national low carbon development strategy.5,6 At the Conference of the Parties in November 2015 (COP21), high level of agreement by developed and developing countries encouraged stakeholders to urgent action to address climate change. The agreement emphasises the urgent mitigation pledges with respect to GHG emissions by 2020. As South Africa implements its White Paper on Climate Change, to stimulate a shift towards a low carbon economy, it faces a monitoring and evaluation challenge. Currently, the South African GHG emission inventory is based on fossil fuel emissions, as part of the National Atmospheric Emissions Inventory System, under the National Air Quality Act, 2004 (Act No. 39 of 2004). Briefly, emissions are rarely measured directly, but rather based on proxy estimates of activity, extrapolated by an emission factor for the specific activity. There is therefore a need to independently assess the effectiveness of emissions reductions within the context of natural CO2 fluxes. Understanding the changing driving forces of climate change and evaluation of the carbon emission reduction activities requires long-term and high-precision measurements of CO2 gas emissions and sinks as well as their evolution. Land can act as both a source and a sink for GHGs.7 Currently the baseline GHG emissions from land and agriculture are thought to amount to 3.03x1010 kg CO2 eq per year in South Africa. The land sector is responsible for an uptake of 2.1x1010 kg CO2 eq per year while agriculture is responsible for a release of 5.06x1010 kg CO2 eq per year.7 The GHG emissions for South African industry amounted to ~5.45x1011 kg CO2 eq in 20108,9, with approximately 79% from the energy sector -- an order of magnitude larger than the emissions from agriculture7. Under the proposed White Paper policy, South Africa's GHG peak, plateau and decline trajectory anticipates emissions to peak at 6.1x1011 kg CO2 eq between 2020 and 2025, plateau at this range for about 10 years and decline to ~4.3x1011 kg CO2 eq by 2050.6 Determining these fluxes accurately will facilitate assessment of the proposed commitments to mitigation and adaptation strategies adopted by South Africa. At present there is infrastructure deployed in South Africa for the measurement of the concentrations and fluxes of CO2, which include observations in the atmosphere, on land and in the ocean. [ABSTRACT FROM AUTHOR]
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- 2017
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