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  • 1
    Online Resource
    Online Resource
    Dordrecht :Springer Netherlands,
    Keywords: Dust. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (526 pages)
    Edition: 1st ed.
    ISBN: 9789401789783
    DDC: 551.304
    Language: English
    Note: Intro -- Preface -- Personal Notes by the Editors -- Peter Knippertz -- Jan-Berend W. Stuut -- Acknowledgements -- Contents -- Contributors -- About the Editors -- 1 Introduction -- 1.1 Why Study Dust? -- 1.2 A Short History of Dust Research -- 1.3 Recent Developments: Timeliness of This Book -- 1.4 Outline and Structure of This Book -- References -- 2 On Composition, Morphology, and Size Distribution of Airborne Mineral Dust -- 2.1 Introduction -- 2.2 Composition -- 2.2.1 Mineralogical Data -- 2.2.2 Isotope Data -- 2.2.3 Elemental Data -- 2.3 Individual-Particle Analysis -- 2.3.1 Particle Shape and Morphology -- 2.4 Size Distributions -- 2.5 Discussion and Conclusions -- 2.5.1 Direct Radiative Forcing -- 2.5.2 Indirect Radiative Forcing -- 2.5.3 Ecosystem Nutrient Supply and Human Health Effects -- References -- 3 Identifying Sources of Aeolian Mineral Dust: Present and Past -- 3.1 Introduction -- 3.2 Processes of Dust Particle Formation -- 3.3 Methods of Identifying Contemporary Dust Sources -- 3.3.1 Geomorphic Perspectives on Dust Sources -- 3.3.2 Aerosol Indexes (AI) Derived from the Orbiting TOMS (Total Ozone Mapping Spectrometer) -- 3.3.3 MODIS and MISR Imagery from the Terra and Aqua Satellites -- 3.3.4 Back-Trajectory Analyses to Identify Dust Sources -- 3.4 Identification of Past Dust Sources -- 3.4.1 Geomorphic Evidence of Past Dust Sources -- 3.4.2 Physical Properties of Dust Deposits -- 3.4.3 Mineralogy as a Guide to Dust Sources -- 3.4.4 Geochemical Methods of Identifying Dust Sources -- 3.4.5 Isotopic Methods of Identifying Dust Sources -- 3.4.6 Biologic Methods of Identifying Dust Sources -- 3.5 Conclusion -- References -- 4 Processing and Ageing in the Atmosphere -- 4.1 Introduction -- 4.2 Physical Processing -- 4.3 Chemical Processing -- 4.3.1 Impacts on Physical Properties of Dust -- 4.3.2 Impacts on Dust Reactivity. , 4.3.3 Impacts on Atmospheric Composition -- Nitric Acid and Nitrogen Oxides -- Sulphur Species -- Ozone -- Other Inorganic and Organic Species -- 4.4 Conclusion -- References -- 5 Dust Production Mechanisms -- 5.1 Introduction -- 5.2 General Understanding -- 5.3 Erosion Threshold -- 5.3.1 Influence of Soil Particle Size -- 5.3.2 Influence of Soil Moisture -- 5.3.3 Influence of Surface Roughness -- 5.3.4 Other Factors -- 5.4 Saltation -- 5.5 Dust Emission -- 5.5.1 Empirical Approaches -- 5.5.2 Physically Based Models -- 5.5.3 Models Versus Observations -- 5.6 Conclusion -- References -- 6 Meteorological Aspects of Dust Storms -- 6.1 Introduction -- 6.2 Large-Scale Circulations -- 6.3 Synoptic-Scale Aspects -- 6.3.1 Cyclone Dominated Dust Events -- 6.3.2 Anticyclone Dominated Dust Events -- 6.3.3 Dynamics and Character of Dust Fronts -- 6.4 Moist Convection -- 6.5 Dry Convection -- 6.6 Diurnal Variations -- 6.7 Topographic Effects -- 6.8 Modelling -- 6.9 Conclusion -- References -- 7 Dust Observations and Climatology -- 7.1 Introduction -- 7.2 Observational Systems -- 7.3 Applications -- 7.3.1 Source Regions -- Regional Data from Geostationary Satellite -- Global Data from Polar-Orbiting Satellite -- 7.3.2 Transport -- General Features -- AOD, Dust Discrimination and Dust Above Clouds -- 7.3.3 Interannual Variability and Trends -- 7.3.4 Vertical Structure -- 7.4 Conclusion -- References -- 8 Dust Deposition -- 8.1 Introduction -- 8.2 Deposition Processes -- 8.2.1 Dry Deposition -- Gravitational Settling Velocity -- Aerodynamic and Quasi-laminar Resistances -- 8.2.2 Wet Deposition -- Brownian Diffusion -- Interception -- Inertial Impaction -- 8.2.3 Particle Size Distribution and Deposition in Dust Models -- 8.3 Dust Deposition Measurements -- 8.4 The Uncertainties in the Simulated Dust Mass Budget -- 8.5 Conclusion -- References. , 9 Numerical Dust Models -- 9.1 Introduction -- 9.2 Dust Emission Modelling -- 9.3 Model Representation of Dust Source Properties -- 9.4 Role of Meteorology in Dust Emission and Transport -- 9.5 Deposition -- 9.6 Optical Properties of Dust Used in Dust Models -- 9.7 Regional Dust Models -- 9.8 Global Dust Models -- 9.9 Conclusion -- References -- 10 Operational Dust Prediction -- 10.1 Introduction -- 10.1.1 Motivation for Dust Forecasting -- 10.1.2 A Brief History of Dust Forecasting -- 10.1.3 Specific Challenges in Dust Prediction -- 10.2 Dust Prediction Models -- 10.2.1 Global Models -- ECMWF/MACC Aerosol Prediction System -- FNMOC Navy Aerosol Analysis and Prediction System -- JMA Operational Dust Forecast Model -- Met Office Dust Prediction System -- NASA GEOS-5 Aerosol Forecasting System -- NCEP/NGAC Global Aerosol Forecasting System -- NMMB/BSC-Dust Model -- 10.2.2 Regional Models -- CHIMERE Model -- CUACE/Dust -- The DREAM/BSC-DREAM8b Models -- FNMOC Coupled Ocean-Atmosphere Mesoscale Prediction System (COAMPS) -- Regional Mineral Dust Forecast Model in Taiwan -- 10.3 Multi-model Ensembles -- 10.3.1 The International Cooperative for Aerosol Prediction (ICAP) Multi-model Ensemble -- 10.3.2 WMO SDS Regional Dust Prediction Multi-model Ensemble -- 10.4 Data Assimilation for Dust Prediction -- 10.4.1 Introduction -- 10.4.2 Main Concepts -- 10.5 Evaluation of Atmospheric Dust Prediction Models -- 10.5.1 General Concepts -- 10.5.2 Observational Data for Evaluation -- 10.5.3 Metrics -- 10.5.4 Examples of Near Real-Time Evaluation -- The WMO SDS-WAS Dust Model Evaluation Initiative -- The MACC-II Evaluation -- Case Study Evaluation -- 10.6 Conclusion -- Appendix A: Technical Aspects of Data Assimilationfor Dust Prediction -- A10.1 Assimilation Techniques -- Variational Methods (CMA, ECMWF, FNMOC/NRL, Met Office, NASA GMAO). , Kalman Filter and Ensemble Kalman Filter Methods (MRI/JMA, NRL) -- A10.2 Observations Used for the Dust Analyses -- Main Products -- Data Quality Aspects and Bias Correction -- A10.3 Definitions of Background and Observational Errors -- Background Error Covariance Matrices -- Flow-Dependent Background Error Covariance Matrix -- Observation Errors -- References -- 11 Radiative Effects of Dust -- 11.1 Introduction -- 11.2 Optical Properties of Dust -- 11.2.1 Definition of Optical Properties -- 11.2.2 Methods of Characterising Dust Optical Properties -- 11.2.3 Sensitivity of Optical Properties to Size and Composition: An Illustrative Example -- 11.2.4 Measurements of Single-Scattering Albedo -- 11.3 Measurements and Estimates of Radiative Effect -- 11.4 Implications of Dust-Radiation Interactions for Satellite Retrievals -- 11.5 Dust and Visibility -- 11.6 Implications for Including the Radiative Impact of Dust in Models -- References -- 12 Mineral Dust and its Microphysical Interactions with Clouds -- 12.1 CCN, IN, and Their Impacts on Clouds, the Hydrological Cycle, and Climate -- 12.2 The CCN Activity of Mineral Dust -- 12.3 The IN Activity of Mineral Dust -- 12.4 Field Observations of Dust CCN Activity/Hygroscopicity -- 12.5 Field Observations of Mineral Dust as IN -- 12.6 Laboratory Experiments on Mineral Dust CCN -- 12.7 Laboratory Experiments on Mineral Dust IN -- 12.8 Modeling Studies on the Interaction of Dust with Clouds -- 12.9 Conclusion -- References -- 13 Impact of Dust Radiative Forcing upon Climate -- 13.1 Introduction -- 13.2 Radiative Forcing by Dust Aerosols -- 13.3 Dust Radiative Impacts upon Climate -- 13.3.1 Temperature -- 13.3.1.1 Temperature Adjustment in Convectively Mixed Regions -- 13.3.1.2 Temperature Adjustment in Subsiding Regions -- 13.3.2 Precipitation -- 13.3.2.1 The Global Anomaly -- 13.3.2.2 Regional Anomalies. , 13.4 Feedback of Climate Anomalies upon the Dust Cycle -- 13.4.1 Surface Wind Speed and Dust Mobilization -- 13.4.2 Vegetation and Dust Source Extent -- 13.5 Conclusion -- References -- 14 Biogeochemical Impacts of Dust on the Global Carbon Cycle -- 14.1 Introduction -- 14.2 Biogeochemical Impacts of Dust on Terrestrial Systems -- 14.2.1 Soil Formation -- 14.2.2 Nutrient Supply -- 14.3 Biogeochemical Impacts of Dust Deposition on the Oceans -- 14.4 Conclusion -- References -- 15 Dust and Human Health -- 15.1 Introduction -- 15.2 Review of Air Pollution Basics -- 15.3 Human Exposure Pathways -- 15.4 Characteristics That Contribute to Observed Health Effects -- 15.4.1 Particle Size and Composition -- 15.4.2 Microorganisms in Dust -- 15.4.3 Mechanisms of Action -- 15.4.4 Exposure and Susceptibility -- 15.5 Ailments Associated with Airborne Dusts -- 15.5.1 Asthma -- 15.5.2 Meningitis -- 15.5.3 Hospitalization and Mortality Related to Intercontinental Dust -- 15.5.4 Exposures to Agricultural Dusts -- 15.5.5 Other Potential Risks Related to MD Exposures: Pneumoconioses -- 15.6 Conclusion -- References -- 16 Loess Records -- 16.1 Introduction -- 16.2 Definition of Loess -- 16.3 Mineralogy and Geochemistry of Loess -- 16.4 Genesis of Loess Deposits -- 16.5 Loess Stratigraphy -- 16.6 Loess Geochronology -- 16.7 Paleoclimatic and Paleoenvironmental Interpretation of Loess Deposits -- 16.8 Global Loess Deposits -- 16.8.1 Europe -- 16.8.2 Africa and the Middle East -- 16.8.3 Asia -- 16.8.4 Australia and New Zealand -- 16.8.5 South America -- 16.8.6 North America -- 16.9 Conclusion -- References -- 17 Subaquatic Dust Deposits -- 17.1 Introduction -- 17.2 From Desert Source to Subaquatic Sink: Dust Transport Processes -- 17.3 Wind-blown Dust in Subaqueous Sedimentary Archives: A Recorder of Environmental Changes -- 17.3.1 Lacustrine Dust Archives. , 17.3.2 Marine Dust Archives.
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  • 2
    Keywords: Dissertation ; Hochschulschrift
    Type of Medium: Book
    Pages: 128 S , Ill., graph. Darst., Kt
    ISBN: 9057440695
    Series Statement: Geologica Ultraiectina 212
    Language: English
    Note: Zsfassung in niederländ. Sprache , Zugl.: Utrecht, Univ., Diss., 2001
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  • 3
    ISSN: 1365-3091
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: The terrigenous fraction of seabed sediments recovered along the north-west African continental margin illustrates spatial variability in grain size attributed to different transport mechanisms. Three subpopulations are determined from the grain-size analyses (n = 78) of the carbonate-free silt fraction applying an end-member modelling algorithm (G. J. Weltje, 1997). The two coarsest end-members are interpreted as representing aeolian dust, and the fine-grained end-member is related to fluvial supply. The end-member model thus allows aeolian fallout to be distinguished from fluvial-sourced mud in this area. The relative contributions of the end-members show distinct regional variations that can be related to different transport processes and pathways. Understanding present-day sediment dispersal and mixing is important for a better understanding of older sedimentary records and palaeoclimate reconstructions in the region.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2020-02-06
    Description: Coccolithophores are calcifying phytoplankton and major contributors to both the organic and inorganic oceanic carbon pumps. Their export fluxes, species composition, and seasonal patterns were determined in two sediment trap moorings (M4 at 12° N, 49° W and M2 at 14° N, 37° W) collecting settling particles synchronously from October 2012 to November 2013 at 1200 m of water depth in the open equatorial North Atlantic. The two trap locations showed a similar seasonal pattern in total coccolith export fluxes and a predominantly tropical coccolithophore settling assemblage. Species fluxes were dominated throughout the year by lower photic zone (LPZ) taxa (Florisphaera profunda, Gladiolithus flabellatus) but also included upper photic zone (UPZ) taxa (Umbellosphaera spp., Rhabdosphaera spp., Umbilicosphaera spp., Helicosphaera spp.). The LPZ flora was most abundant during fall 2012, whereas the UPZ flora was more important during summer. In spite of these similarities, the western part of the study area produced persistently higher fluxes, averaging 241×107 ± 76×107 coccoliths m−2 d−1 at station M4 compared to only 66×107 ± 31×107 coccoliths m−2 d−1 at station M2. Higher fluxes at M4 were mainly produced by the LPZ species, favoured by the westward deepening of the thermocline and nutricline. Still, most UPZ species also contributed to higher fluxes, reflecting enhanced productivity in the western equatorial North Atlantic. Such was the case of two marked flux peaks of the more opportunistic species Gephyrocapsa muellerae and Emiliania huxleyi in January and April 2013 at M4, indicating a fast response to the nutrient enrichment of the UPZ, probably by wind-forced mixing. Later, increased fluxes of G. oceanica and E. huxleyi in October–November 2013 coincided with the occurrence of Amazon-River-affected surface waters. Since the spring and fall events of 2013 were also accompanied by two dust flux peaks, we propose a scenario in which atmospheric dust also provided fertilizing nutrients to this area. Enhanced surface buoyancy associated with the river plume indicates that the Amazon acted not only as a nutrient source, but also as a surface density retainer for nutrients supplied from the atmosphere. Nevertheless, lower total coccolith fluxes during these events compared to the maxima recorded in November 2012 and July 2013 indicate that transient productivity by opportunistic species was less important than "background" tropical productivity in the equatorial North Atlantic. This study illustrates how two apparently similar sites in the tropical open ocean actually differ greatly in ecological and oceanographic terms. The results presented here provide valuable insights into the processes governing the ecological dynamics and the downward export of coccolithophores in the tropical North Atlantic.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2020-04-22
    Description: Cruise M140 combined sampling of plankton, mineral dust and other particles in the water column with recovery of data and samples from long-term observational platforms (sediment traps and dust-collecting buoys). The aim of the cruise was to provide new observations to improve our understanding of the ecology of planktonic foraminifera as important carriers of paleoceanographic proxies and to investigate how mineral dust deposition and the production of marine snow and biogenic particle ballast vary in space and time and how they affect the marine biological pump. To this end, the cruise followed a transect in the central western Atlantic between oligotrophic waters of the subtropical gyre and the productive coastal waters off Mauretania affected by coastal upwelling. To characterise population dynamics, ecology and physiology of planktonic foraminifera, we obtained a series of fourteen vertically resolved plankton net profiles along the cruise track, together with profiles of physical and chemical properties of the ambient water masses. Live foraminifera extracted from these profiles were used to quantify photosynthetic activity of selected species and determine their photoadaptation. High-resolution spatial and temporal sampling of the upper 300 m over 24 hours was carried out at two locations (recovering 41 and 46 vertical profiles), allowing the characterisation of patchiness and daily vertical migration of planktonic foraminifera. Moorings with sediment traps monitoring the seasonal and short-term variability of particle fluxes and buoys monitoring atmospheric dust deposition in the region were successfully recovered in the central Atlantic (M3), south of Cabo Verde (M1) and off Mauretania (CB and CBi) and redeployed in the latter two regions to continue the monitoring. Short-term variability of sizes and types of sinking particles in the water column were characterised in each of the monitoring regions with drifting sediment traps and in the Cape Blanc region off Mauretania also with continuous vertical particle camera profile. All aims of the cruise have been met – the plankton sampling and particle characterization studies were carried out successfully and all moorings and buoys could be recovered and/or redeployed as planned.
    Type: Report , NonPeerReviewed
    Format: text
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  • 6
    Publication Date: 2019-09-23
    Description: A set of 40 Uranium-series datings obtained on the reef-forming scleractinian cold-water corals Lophelia pertusa and Madrepora oculata revealed that during the past 400 kyr their occurrence in the Gulf of Cádiz (GoC) was almost exclusively restricted to glacial periods. This result strengthens the outcomes of former studies that coral growth in the temperate NE Atlantic encompassing the French, Iberian and Moroccan margins dominated during glacial periods, whereas in the higher latitudes (Irish and Norwegian margins) extended coral growth prevailed during interglacial periods. Thus it appears that the biogeographical limits for sustained cold-water coral growth along the NE Atlantic margin are strongly related to climate change. By focussing on the last glacial-interglacial cycle, this study shows that palaeo-productivity was increased during the last glacial. This was likely driven by the fertilisation effect of an increased input of aeolian dust and locally intensified upwelling. After the Younger Dryas cold event, the input of aeolian dust and productivity significantly decreased concurrent with an increase in water temperatures in the GoC. This primarily resulted in reduced food availability and caused a widespread demise of the formerly thriving coral ecosystems. Moreover, these climate induced changes most likely caused a latitudinal shift of areas with optimum coral growth conditions towards the northern NE Atlantic where more suitable environmental conditions established with the onset of the Holocene.
    Type: Article , PeerReviewed
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  • 7
    Publication Date: 2023-02-08
    Description: Mineral dust plays an important role in the atmospheric radiation budget as well as in the ocean carbon cycle through fertilization and by ballasting of settling organic matter. However, observational records of open‐ocean dust deposition are sparse. Here, we present the spatial and temporal evolution of Saharan dust deposition over 2 years from marine sediment traps across the North Atlantic, directly below the core of the Saharan dust plume, with highest dust fluxes observed in summer. We combined the observed deposition fluxes with model simulations and satellite observations and argue that dust deposition in the Atlantic is predominantly controlled by summer rains. The dominant depositional pathway changes from wet deposition in summer to dry deposition in winter. Wet deposition has previously been suggested to increase the release of dust‐derived nutrients and their bioavailability, which may be a key contributor to surface‐ocean productivity in remote and oligotrophic parts of the oceans.
    Type: Article , PeerReviewed
    Format: text
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  • 8
    Publication Date: 2019-09-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: PANGAEA Documentation , notRev
    Format: application/pdf
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  • 9
  • 10
    Publication Date: 2020-05-13
    Description: Mineral dust plays an important role in the atmospheric radiation budget as well as in the ocean carbon cycle through fertilization and by ballasting of settling organic matter. However, observational records of open‐ocean dust deposition are sparse. Here, we present the spatial and temporal evolution of Saharan dust deposition over 2 years from marine sediment traps across the North Atlantic, directly below the core of the Saharan dust plume, with highest dust fluxes observed in summer. We combined the observed deposition fluxes with model simulations and satellite observations and argue that dust deposition in the Atlantic is predominantly controlled by summer rains. The dominant depositional pathway changes from wet deposition in summer to dry deposition in winter. Wet deposition has previously been suggested to increase the release of dust‐derived nutrients and their bioavailability, which may be a key contributor to surface‐ocean productivity in remote and oligotrophic parts of the oceans.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev , info:eu-repo/semantics/article
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