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  • 1
    Online Resource
    Online Resource
    Cambridge :Cambridge University Press,
    Keywords: Ocean-atmosphere interaction. ; Climatic changes. ; Electronic books.
    Description / Table of Contents: The sea surface, essentially the top millimetre of the ocean, is the critical interface of the sea with the atmosphere. Ozone depletion and marine pollution may have significant effects on global change via this layer. This first comprehensive account in a decade describes the properties of the sea surface and how it may influence global phenomena such as climate in the future.
    Type of Medium: Online Resource
    Pages: 1 online resource (537 pages)
    Edition: 1st ed.
    ISBN: 9780511525025
    DDC: 551.46/01
    Language: English
    Note: Cover -- Half-title -- Title -- Copyright -- Contents -- List of contributors -- Preface -- 1 Report Group 1 - Physical processes in the microlayer and the air-sea exchange of trace gases -- Surface films -- Sources, sinks, and properties of surface films -- Surface films and gas exchange -- Surface films and bulk material -- Extent and viscoelastic properties of surface films -- Physical processes in the microlayer -- Comparison of surface-renewal and boundary-layer models of near surfacetransfer -- Short capillary waves -- The relation between heat and mass transfer -- Wave breaking and bubbles -- The role of bubbles in heat flux -- The role of bubbles in gas exchange -- The effect of surfactants on bubble-mediated gas exchange -- The effects of wave breaking on microlayer composition -- Bubble floatation and aerosol formation processes -- The effect of rain on exchange processes -- Horizontal transport and deposition of surface slicks in coastal zones -- Review of experimental data on gas transfer -- Gas transfer velocities -- Discrepancy between 14C-based and inert gas exchange rates -- Do catalysts exist in the microlayer which may enhance CO2 gas exchange? -- Review of experimental techniques -- 'New' techniques for measuring air-sea gas exchange rates -- Dual tracer technique -- How can we deal with the large spatial variability ofpCQ2? -- Controlled flux technique -- Are direct measurements of the heat flux possible? -- Novel ocean-surface sampling techniques -- Parameterization of air-sea exchange processes -- Best parameterization for momentum, heat, and material fluxes -- Parameterizations including viscoelasticity of the air-sea interface -- Conclusions and recommendations -- References -- 2 Report Group 2 - Biological effects of chemical and radiative change in the sea surface -- Introduction -- Samplers and sampling techniques. , The prism-dipping technique -- The screen sampler -- Plate and drum samplers -- Techniques for sampling neuston -- Characteristics of the surface microlayer -- Enrichment factors -- Surface excess concentrations -- Variability of organisms and contaminants -- Thickness of sea-surface films -- Biology of the sea surface -- Piconeuston -- Nano- and microneuston -- Mesozooneuston -- Macroneuston -- Freshwater neuston -- Chemistry in the sea surface -- Organic components of natural origin -- Organic components of anthropogenic origin -- Trace elements -- Organotin compounds -- Radionudides -- Freshwater chemistry -- Effects of ultraviolet radiation -- Effects of chemical contamination -- Effects of greenhouse warming -- Global change and the microlayer -- Conclusions and recommendations -- References -- 3 Report Group 3 - Photochemistry in the sea-surface microlayer. -- Introduction -- Photochemistry in the upper ocean -- Major photochemical reactions -- Photoalteration and photoproducts of CDOM -- Hydrocarbon degradation -- Probable photochemical processes in the microlayer -- In situ trace gas production -- Atmospheric inputs of trace species -- In situ halogen chemistry -- Conversion of DOC -- Hydrocarbon degradation -- Global change issues -- Changes in ultraviolet radiation -- Radiation balance -- Conclusions and recommendations -- References -- 4 Transport processes in the sea-surface microlayer -- Abstract -- Introduction -- Basic concepts -- Equations of motion and boundary conditions -- Secondary motions: polygonal cells and helicoidal rolls -- Secondary motions: surface drift, waves, and wave breaking -- Surface streaming -- Observations of surface streaming -- Assessment -- Influence of rain -- Salinity -- Momentum transfer -- Rain-induced turbulence and wave damping -- Heatflux. , Experimental studies of the microlayer: miscellaneous techniques -- Early investigations -- Turbulence generation at the boundary -- Radon evasion technique -- Velocity profiles near the interface -- Temperature profiles at the interface -- Forced heat flow technique -- Conclusion -- References -- 5 The role of organic films in air-sea gas exchange -- Abstract -- Introduction -- The microlayer and air-sea processes -- Air-sea gas exchange -- The role ofbiogenous organic matter -- Surface-active matter in the marine microlayer -- Sources and chemical nature -- Surface physical properties -- Surfactants and mechanisms of gas exchange -- Static versus dynamic effects of surfactant films -- Physical models of air-water gas transfer -- Experimental studies of films in stirred systems -- Experimental studies of films in wind-wave systems -- Influence of waves on gas exchange -- Gas exchange in the presence of films -- Influence of surfactants on the wave field -- Concluding remarks -- Acknowledgments -- References -- 6 Bubbles and their role in gas exchange -- Abstract -- Introduction -- Mechanisms of air-sea gas transfer -- Properties of bubble-mediated transfer -- The oceanic distribution of bubbles -- Estimates of bubble-mediated gas transfer -- Discussion -- Summary -- References -- 7 The physical chemistry of air-sea gas exchange -- Abstract -- Introduction -- Thermodynamics: the steady-state model -- Kinetics: 1. A surface-renewal model -- Kinetics: 2. Incorporation of a turbulent air layer -- Comparison of theory and experiment -- General comments -- Detailed comparison with the data ofLiss et al. (1981) -- Detailed comparison with data of Smith and Jones (1985) -- Detailed comparison with data of Smith et al. (1991) -- Conclusions -- Acknowledgments -- References -- 8 The sea-surface microlayer and its effect on global air-sea gas transfer. , Abstract -- Introduction -- Motivation and purpose -- Background information on surfactants in the microlayer -- Processes affecting gas transfer -- Air-sea gas exchange background -- Barrier effects and changes in ∆PX> -- Scy and Kh -- Hydrodynamic effects -- Breaking waves and the microlayer -- Microlayer effects on global fluxes -- Description of model -- Global air-sea CO2 flux -- NH3flux in the Pacific Ocean -- Conclusions, implications for further research -- Acknowledgements -- References -- 9 Chemistry of the sea-surface microlayer -- Abstract -- Prologue -- Methods for sampling the microlayer -- The screen sampler -- The glass plate sampler -- Hydrophobic samplers -- Rotating drum samplers -- The prism-dipping method -- The bubble microtome -- Enrichment factors and microlayer thickness -- Enrichment factor EF -- Surface excess concentration -- Organic chemical composition of the microlayer -- Lipids and hydrocarbons -- Dissolved and particulate organic carbon -- Plant pigments -- Organic pollutants -- UV absorption and fluorescence -- Electrochemical methods -- Trace elements in the microlayer -- Dissolved trace elements -- Major cations of seawater -- Particulate trace metals -- Physico-chemical properties of sea-surface films -- Sea slicks y capillary waves and film pressures -- Film pressure-area measurements -- Epilogue -- References -- 10 Biophysics of the surface film of aquatic ecosystems -- Abstract -- Introduction -- Experimental studies -- Effects of surf ace-living organisms -- References -- 11 Biological effects of chemicals in the sea-surface microlayer -- Abstract -- The aquatic surface layer -- Sea-surface sample collection -- Membrane filter: -- Glass plate: -- Screen: -- Pump: -- Nets: -- Biology of the aquatic surface layer -- Piconeuston -- Autotrophic nano- and microneuston -- Heterotrophic nano- and microneuston. , Mesozooneuston -- Macroneuston -- Anthropogenic chemical enrichment of the sea surface -- Sources of contamination -- Metals -- Radio nuclides -- Organics -- Biological effects of sea-surface contamination -- Effects on intertidal biota -- Effects on fish eggs and larvae -- Effects on microneuston and gas exchange -- Relation of effects to visible slicks -- Global effects of sea-surface stress -- Summary -- References -- 12 Neuston of seas and oceans -- Abstract -- Introduction -- The extreme surface of the sea as a specific habitat -- Neuston and pleuston communities of marine organisms adapted to specific life conditions in the uppermost sea layer -- Structure and taxonomic composition of the neuston -- Numbers ofneustonic organisms -- Neuston as a connecting link in the biosphere -- Anthropogenic influences on neuston -- Neuston as a factor influencing the air-sea exchange -- Acknowledgements -- References -- 13 Photochemistry in the sea-surface microlayer -- Abstract -- Introduction -- Optical properties of microlayer and bulk-water chromophores -- Photochemical reactions -- Singlet dioxygen (1O2 -- 1∆g) -- Superoxide/hydroperoxyl radical (O2~/HO2) -- Hydrogen peroxide (H2O2) -- Hydroxyl radical (OH) -- Peroxy radicals (RO2) -- Low molecular weight organic compounds and trace gases -- Trace metals (Fe, Mn) -- Estimated production rates and fluxes of photochemical species in the microlayer -- Concluding remarks -- Acknowledgements -- References -- 14 Hydrocarbon breakdown in the sea-surface microlayer -- Abstract -- Microlayer samplers -- Compound groups found in the microlayer -- Sources and sinks of hydrocarbons in the microlayer -- Sensitized photooxidation of hydrocarbons -- Model experiments and natural phenomena -- References -- 15 Applications of laser technology and laser spectroscopy in studies of the ocean microlayer -- Abstract. , Introduction.
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  • 2
    Publication Date: 2019-09-23
    Description: Environmental context. Approximately 25 % of CO2 released to the atmosphere by human activities has been absorbed by the oceans, resulting in ocean acidification. We investigate the acidification effects on marine phytoplankton and subsequent production of the trace gas dimethylsulfide, a major route for sulfur transfer from the oceans to the atmosphere. Increasing surface water CO2 partial pressure (pCO2) affects the growth of phytoplankton groups to different degrees, resulting in varying responses in community production of dimethylsulfide. Abstract. The human-induced rise in atmospheric carbon dioxide since the industrial revolution has led to increasing oceanic carbon uptake and changes in seawater carbonate chemistry, resulting in lowering of surface water pH. In this study we investigated the effect of increasing CO2 partial pressure (pCO2) on concentrations of volatile biogenic dimethylsulfide (DMS) and its precursor dimethylsulfoniopropionate (DMSP), through monoculture studies and community pCO2 perturbation. DMS is a climatically important gas produced by many marine algae: it transfers sulfur into the atmosphere and is a major influence on biogeochemical climate regulation through breakdown to sulfate and formation of subsequent cloud condensation nuclei (CCN). Overall, production of DMS and DMSP by the coccolithophore Emiliania huxleyi strain RCC1229 was unaffected by growth at 900 μatm pCO2, but DMSP production normalised to cell volume was 12 % lower at the higher pCO2 treatment. These cultures were compared with community DMS and DMSP production during an elevated pCO2 mesocosm experiment with the aim of studying E. huxleyi in the natural environment. Results contrasted with the culture experiments and showed reductions in community DMS and DMSP concentrations of up to 60 and 32 % respectively at pCO2 up to 3000 μatm, with changes attributed to poorer growth of DMSP-producing nanophytoplankton species, including E. huxleyi, and potentially increased microbial consumption of DMS and dissolved DMSP at higher pCO2. DMS and DMSP production differences between culture and community likely arise from pH affecting the inter-species responses between microbial producers and consumers.
    Type: Article , PeerReviewed
    Format: text
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