GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
Document type
Keywords
Language
  • 1
    Online Resource
    Online Resource
    New York :Cambridge University Press,
    Keywords: Estuarine ecology. ; Electronic books.
    Description / Table of Contents: A comprehensive, state-of-the-art synthesis of biogeochemical dynamics at major river-coastal interfaces for advanced students and researchers. It presents a unique perspective on how humans have altered these systems, as well as the implications of these changes on issues as diverse as the health of fisheries and the global carbon budget.
    Type of Medium: Online Resource
    Pages: 1 online resource (674 pages)
    Edition: 1st ed.
    ISBN: 9781107503571
    DDC: 577.14
    Language: English
    Note: Intro -- Contents -- List of Contributors -- Preface -- Section I Introduction -- 1 An introduction to the biogeochemistry of river-coastal systems -- 1. Introduction -- 2. Riverine inputs of particulate and dissolved organic matter to the coastal ocean -- 2.1. The conundrum of missing OC -- 3. Transport processes and controls on OM preservation -- 4. CO2 fluxes in coastal waters -- 5. Possible links between coastal water CO2 flux and riverine loadings -- 6. Directions for future research -- Section II Water and sediment dynamics from source to sink -- 2 Water and sediment dynamics through the wetlands and coastal water bodies of large river deltaic plains -- 1. Introduction -- 2. Mechanisms of water and sediment input to the delta plain -- 2.1. Avulsion and distributary channel evolution -- 2.2. Overbank and crevasse processes -- 2.3. Groundwater and rainwater input -- 3. Processes and simulation of water and sediment circulation in deltaic plains and estuaries -- 3.1. Controlling physical processes -- 3.2. Simulation of water and sediment processes -- 3.3. Numerical modeling tools -- 4. The role of wetlands -- 4.1. Introduction to the ecogeomorphology of deltaic plain wetlands -- 4.2. Controls on deltaic wetland development -- 4.3. Large river wetlands as particle sources, sinks, and loci of particle transformation -- 5. Conclusions -- 3 Freshwater and sediment dispersal in large river plumes -- 1. Introduction -- 2. The anatomy of a river plume -- 2.1. Salinity space -- 2.2. The estuary -- 2.3. The near-field plume -- 2.4. The mid-field plume, or the bulge -- 2.5. Far-field plume -- 2.6. Very far-field plume -- 3. River plume classification -- 4. Sediment dispersal -- 4.1. Sediment dynamics -- 4.1.1. Buoyancy effect -- 4.1.2. Flocculation and hindered settling -- 4.2. Riverine input and carrying capacity. , 4.3. The near-, mid-, and far-field dispersal -- 5. Concluding remarks -- 4 Shelf and slope sedimentation associated with large deltaic systems -- 1. Introduction -- 2. Overview of large deltaic systems -- 3. Amazon: a subaqueous delta clinoform system -- 4. Ganges-Brahmaputra: a combination of influences -- 5. Mississippi-Atchafalaya: a proximal accumulation-dominated system -- 6. Fluvial and marine controls on large deltaic systems -- 7. Geological framework and human influence on large deltaic systems -- 8. Conclusions -- Acknowledgments -- 5 Changjiang (Yangtze) and Huanghe (Yellow) Rivers: historical reconstruction of land-use change and sediment load to the sea -- 1. Regional settings of the Changjiang and Huanghe River basins -- 1.1. Topographic settings -- 1.2. Hydrologic settings -- 1.3. Surface lithology of the river basins -- 2. Human impacts on the river basins and land-use change -- 3. Anthropogenic alteration of the rivers since the 1950s -- 3.1. Variation of the Changjiang sediment flux since the 1950s -- 3.2. Variation of the Huanghe sediment flux since the 1950s -- 4. Roles of climate change and human activities on river systems -- 5. The future of the mega-deltas of Changjiang and Huanghe -- 6. Conclusion -- 6 Flux and fate of the Yellow (Huanghe) River-derived materials to the sea: impacts of climate change and human activities -- 1. Introduction -- 2. Historical changes of the Yellow River water and sediment discharge -- 2.1. Sediment fluxes on the millennial scale -- 2.2. Sediment fluxes on the decadal scale -- 2.3. Causes of the recent decrease of the water and sediment discharge -- 2.4. Impacts of the recent-year water discharges and sediment loads decreasing -- 3. Fate of yellow river sediments in the Bohai and Yellow Seas -- 3.1. Rapid accumulations near the river mouth: proximal deltaic depocenter. , 3.2. Longshore transport to the Yellow Sea: distal mud depocenter -- 4. Conclusions -- 7 Carbon dioxide dynamics and fluxes in coastal waters influenced by river plumes -- 1. Introduction -- 2. CO2 degassing flux in inner estuaries -- 3. Distribution pattern of pCO2 in river plumes and control mechanisms -- 3.1. River carbonate contents and the associated buffering capacity changes during river-ocean mixing -- 3.2. CO2 in the Changjiang River plume -- 3.3. CO2 in the Mississippi River plume -- 3.4. CO2 in the Amazon River plume -- 4. A tentative estimate of global river-plume CO2 flux -- Acknowledgment -- 8 Impacts of watershed processes on exported riverine organic carbon -- 1. Introduction -- 2. POC Sources -- 2.1. Vegetation -- 2.2. Soils -- 2.3. The deeper regolith and geomorphic processes -- 2.4. In-channel and lowland sources and processes -- 3. Climate impacts on riverine OC -- 4. Predicting the exported riverine organic signature -- 5. Summary -- Acknowledgments -- 9 Black carbon in coastal and large river systems -- 1. Introduction -- 2. Sources of black carbon -- 2.1. Atmospheric BC -- 2.2. Soil BC -- 2.3. Dissolved BC -- 3. Isolation, quantification, and source discrimination methods for black carbon -- 3.1. Visual methods for BC quantification -- 3.2. Chemical and thermal BC quantification methods -- 3.3. Isolation of BC in the dissolved phase -- 3.4. Source discrimination of BC -- 4. Black carbon in large river systems -- 4.1. Fluvial BC -- 4.2. Global pyrogenic PAH discharge and comparison with BC -- 5. Fate of black carbon -- 5.1. Storage BC in the ocean -- 5.2. Degradation of BC -- 6. Conclusions -- Section III Eastern hemisphere systems -- 10 Carbon biogeochemistry in the continuum of the Changjiang (Yangtze) River watersheds across the East China Sea -- 1. Introduction. , 2. Characters of the land-source influx and open boundary processes -- 2.1. Dissolved inorganic carbon and CH4 -- 2.2. Dissolved organic carbon and particulate organic carbon -- 2.3. Pigments -- 3. Major pathways of carbon cycle and influence factors -- 3.1. DIC and CH4 -- 3.2. DOC and POC -- 3.3. Carbon fate inferred from pigments -- 4. Biogeochemical budgets and feedbacks to open ocean and atmosphere -- 5. Evidence of historical records -- 6. Biogeochemical provinces of the Changjiang estuary - ECS in the perspective of carbon biogeochemistry -- 7. Concluding remarks and future work -- Acknowledgments -- 11 Dynamics of phytoplankton blooms and nutrient limitation in the Pearl River (Zhujiang) estuarine coastal waters -- 1. Introduction -- 2. General geographic and oceanographic settings of the Pearl River estuary -- 3. Processes in estuarine and coastal waters -- 4. Spatial and seasonal variability of phytoplankton biomass -- 4.1. River outflow controlled variability -- 4.2. Tidal cycle regulated variability -- 4.3. Wind event driven variability -- 5. Dynamics of nutrients and nutrient limitation variability -- 6. Potential effects of climate change on eutrophication -- 7. Conclusions -- Acknowledgments -- 12 The Mekong River and its influence on the nutrient chemistry and matter cycling in the Vietnamese coastal zone -- 1. Introduction -- 2. Climatology of the Southeast Asian monsoon region -- 3. Hydrography of the Vietnamese coastal waters -- 4. The Mekong River and river plume -- 5. Biochemistry and productivity in the Mekong plume and coastal waters -- 5.1. Phytoplankton species composition -- 5.2. Primary production and nitrogen fixation -- 5.3. Food web and zooplankton nutrition -- 6. How does this compare with other tropical estuaries? -- 7. Future of the Mekong estuary and its catchment -- 8. Conclusion -- Acknowledgment. , 13 Physical dynamics and biogeochemistry of the Pearl River plume -- 1. Introduction -- 2. Basics of the Pearl River, estuary, and the shelf -- 2.1. The Pearl River -- 2.1.1. Basics -- 2.1.2. Precipitation and river discharge -- 2.2. Pearl River estuary -- 2.2.1. Basics -- 2.2.2. Circulation in the estuary -- 2.2.2.1. Gravitational circulation -- 2.2.2.2. Subtidal circulation -- 2.2.2.3. Intra-tidal circulation -- 2.2.3. Hydrology and biogeochemistry of the PRE -- 2.2.4. Conceptual summary and about the mixing behavior: Conservative and nonconservative -- 2.3. Northern South China Sea Shelf -- 2.3.1. Basics -- 2.3.2. Shelf circulation in the northern South China Sea -- 2.3.2.1. Upwelling circulation in summer (wet season) -- 2.3.2.2. Downwelling circulation in winter (dry season) -- 3. Physical dynamics and biogeochemistry of the plume -- 3.1. Plume over the Shelf -- 3.2. Plume effect on the shelf circulation -- 3.3. Biogeochemistry of the river plumes -- 3.3.1. Case of May 2001 -- 3.3.2. Case of August 2008 -- 3.3.3. Comparison between 2001 and 2008 -- 4. Coupling the physical dynamics and biogeochemistry -- 4.1. Mixing of different water masses -- 4.2. Coupled physical-biogeochemical model -- 5. Summary and perspectives -- Acknowledgment -- 14 The evolution of carbon signatures carried by the Ganges-Brahmaputra river system: a source-to-sink perspective -- 1. Introduction to the Ganges-Brahmaputra river system -- 2. Reworking and deposition of fluvial sediment and organic carbon in the Bay of Bengal -- 3. Characterization of organic carbon signatures of the Ganges and Brahmaputra rivers and the Bengal Fan -- 4. Carbon sources, transformations, and storage in the Himalayan range -- 5. Carbon sources, transformations, and storage in the Ganges floodplain -- 6. Carbon sources, transformations, and storage in the Brahmaputra floodplain. , 7. Carbon export from the G-B basin to the Bengal Fan.
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2016-09-19
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2022-05-25
    Description: © The Author(s), 2013. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Journal of Geophysical Research: Oceans 118 (2013): 5439–5460, doi:10.1002/jgrc.20369.
    Description: Underway and in situ observations of surface ocean pCO2, combined with satellite data, were used to develop pCO2 regional algorithms to analyze the seasonal and interannual variability of surface ocean pCO2 and sea-air CO2 flux for five physically and biologically distinct regions of the eastern North American continental shelf: the South Atlantic Bight (SAB), the Mid-Atlantic Bight (MAB), the Gulf of Maine (GoM), Nantucket Shoals and Georges Bank (NS+GB), and the Scotian Shelf (SS). Temperature and dissolved inorganic carbon variability are the most influential factors driving the seasonality of pCO2. Estimates of the sea-air CO2 flux were derived from the available pCO2 data, as well as from the pCO2 reconstructed by the algorithm. Two different gas exchange parameterizations were used. The SS, GB+NS, MAB, and SAB regions are net sinks of atmospheric CO2 while the GoM is a weak source. The estimates vary depending on the use of surface ocean pCO2 from the data or algorithm, as well as with the use of the two different gas exchange parameterizations. Most of the regional estimates are in general agreement with previous studies when the range of uncertainty and interannual variability are taken into account. According to the algorithm, the average annual uptake of atmospheric CO2 by eastern North American continental shelf waters is found to be between −3.4 and −5.4 Tg C yr−1 (areal average of −0.7 to −1.0 mol CO2 m−2 yr−1) over the period 2003–2010.
    Description: We wish to acknowledge the NASA Ocean Biology and Biogeochemistry program for providing funds for this project.
    Keywords: Coastal carbon ; Sea-air CO2 fluxes ; North American east coast
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2022-05-25
    Description: Author Posting. © The Oceanography Society, 2015. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 28, no. 2 (2015): 48-61, doi:10.5670/oceanog.2015.31.
    Description: Oceanic and coastal waters are acidifying due to processes dominated in the open ocean by increasing atmospheric CO2 and dominated in estuaries and some coastal waters by nutrient-fueled respiration. The patterns and severity of acidification, as well as its effects, are modified by the host of stressors related to human activities that also influence these habitats. Temperature, deoxygenation, and changes in food webs are particularly important co-stressors because they are pervasive, and both their causes and effects are often mechanistically linked to acidification. Development of a theoretical underpinning to multiple stressor research that considers physiological, ecological, and evolutionary perspectives is needed because testing all combinations of stressors and stressor intensities experimentally is impossible. Nevertheless, use of a wide variety of research approaches is a logical and promising strategy for improving understanding of acidification and its effects. Future research that focuses on spatial and temporal patterns of stressor interactions and on identifying mechanisms by which multiple stressors affect individuals, populations, and ecosystems is critical. It is also necessary to incorporate consideration of multiple stressors into management, mitigation, and adaptation to acidification and to increase public and policy recognition of the importance of addressing acidification in the context of the suite of other stressors with which it potentially interacts.
    Description: Funding for research on acidification and multiple stressors was provided by NOAACSCOR NA10NOS4780138 to DLB, NASA NNX14AL8 to JS, NSF OCE-1219948 to JMB, NSF OCE-927445 and OCE-1041062 to LAL, NSF EF-1041070 to W-JC, a Linnaeus grant from the Swedish Research Councils VR and Formas to SD, NSF EF-0424599 to SCD, NSF OCE-1041038 to UP, NSF EF-1316113 to BAS, NSF ANT-1142122 to AET, NSF OCE-1316040 to AMT, and the NOAA Ocean Acidification Program Office to BP, LMM, and WCL.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2022-05-25
    Description: © The Author(s), 2016. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Biogeosciences 13 (2016): 5065-5083, doi:10.5194/bg-13-5065-2016.
    Description: One of the major challenges to assessing the impact of ocean acidification on marine life is detecting and interpreting long-term change in the context of natural variability. This study addresses this need through a global synthesis of monthly pH and aragonite saturation state (Ωarag) climatologies for 12 open ocean, coastal, and coral reef locations using 3-hourly moored observations of surface seawater partial pressure of CO2 and pH collected together since as early as 2010. Mooring observations suggest open ocean subtropical and subarctic sites experience present-day surface pH and Ωarag conditions outside the bounds of preindustrial variability throughout most, if not all, of the year. In general, coastal mooring sites experience more natural variability and thus, more overlap with preindustrial conditions; however, present-day Ωarag conditions surpass biologically relevant thresholds associated with ocean acidification impacts on Mytilus californianus (Ωarag 〈 1.8) and Crassostrea gigas (Ωarag 〈 2.0) larvae in the California Current Ecosystem (CCE) and Mya arenaria larvae in the Gulf of Maine (Ωarag 〈 1.6). At the most variable mooring locations in coastal systems of the CCE, subseasonal conditions approached Ωarag =  1. Global and regional models and data syntheses of ship-based observations tended to underestimate seasonal variability compared to mooring observations. Efforts such as this to characterize all patterns of pH and Ωarag variability and change at key locations are fundamental to assessing present-day biological impacts of ocean acidification, further improving experimental design to interrogate organism response under real-world conditions, and improving predictive models and vulnerability assessments seeking to quantify the broader impacts of ocean acidification.
    Description: The CO2 and ocean acidification observations were funded by NOAA’s Climate Observation Division (COD) in the Climate Program Office and NOAA’s Ocean Acidification Program. The maintenance of the Stratus and WHOTS Ocean Reference Stations were also supported by NOAA COD (NA09OAR4320129). Additional support for buoy equipment, maintenance, and/or ancillary measurements was provided by NOAA through the US Integrated Ocean Observing System office: for the La Parguera buoy under a Cooperative Agreement (NA11NOS0120035) with the Caribbean Coastal Ocean Observing System, for the Chá b˘a buoy under a Cooperative Agreement (NA11NOS0120036) with the Northwest Association of Networked Ocean Observing System, for the Gray’s Reef buoy under a Cooperative Agreement (NA11NOS0120033) with the Southeast Coastal Ocean Observing Regional Association, and for the Gulf of Main buoy under a Cooperative Agreement (NA11NOS0120034) with the Northeastern Regional Association of Coastal and Ocean Observing Systems.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2018. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Global Biogeochemical Cycles 32 (2018): 389-416, doi:10.1002/2017GB005790.
    Description: Carbon cycling in the coastal zone affects global carbon budgets and is critical for understanding the urgent issues of hypoxia, acidification, and tidal wetland loss. However, there are no regional carbon budgets spanning the three main ecosystems in coastal waters: tidal wetlands, estuaries, and shelf waters. Here we construct such a budget for eastern North America using historical data, empirical models, remote sensing algorithms, and process‐based models. Considering the net fluxes of total carbon at the domain boundaries, 59 ± 12% (± 2 standard errors) of the carbon entering is from rivers and 41 ± 12% is from the atmosphere, while 80 ± 9% of the carbon leaving is exported to the open ocean and 20 ± 9% is buried. Net lateral carbon transfers between the three main ecosystem types are comparable to fluxes at the domain boundaries. Each ecosystem type contributes substantially to exchange with the atmosphere, with CO2 uptake split evenly between tidal wetlands and shelf waters, and estuarine CO2 outgassing offsetting half of the uptake. Similarly, burial is about equal in tidal wetlands and shelf waters, while estuaries play a smaller but still substantial role. The importance of tidal wetlands and estuaries in the overall budget is remarkable given that they, respectively, make up only 2.4 and 8.9% of the study domain area. This study shows that coastal carbon budgets should explicitly include tidal wetlands, estuaries, shelf waters, and the linkages between them; ignoring any of them may produce a biased picture of coastal carbon cycling.
    Description: NASA Interdisciplinary Science program Grant Number: NNX14AF93G; NASA Carbon Cycle Science Program Grant Number: NNX14AM37G; NASA Ocean Biology and Biogeochemistry Program Grant Number: NNX11AD47G; National Science Foundation's Chemical Oceanography Program Grant Number: OCE‐1260574
    Description: 2018-10-04
    Keywords: Carbon cycle ; Coastal zone ; Tidal wetlands ; Estuaries ; Shelf waters
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2022-01-24
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev , info:eu-repo/semantics/article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2022-05-26
    Description: Author Posting. © Association for the Sciences of Limnology and Oceanography, 2013. This article is posted here by permission of Association for the Sciences of Limnology and Oceanography for personal use, not for redistribution. The definitive version was published in Limnology and Oceanography 58 (2013): 325-342, doi:10.4319/lo.2013.58.1.0325.
    Description: Distributions of total alkalinity (TA), dissolved inorganic carbon (DIC), and other parameters relevant to the marine inorganic carbon system were investigated in shelf and adjacent ocean waters during a U.S. Gulf of Mexico and East Coast Carbon cruise in July–August 2007. TA exhibited near-conservative behavior with respect to salinity. Shelf concentrations were generally high in southern waters (Gulf of Mexico and East Florida) and decreased northward from Georgia to the Gulf of Maine. DIC was less variable geographically and exhibited strongly nonconservative behavior. As a result, the ratio of TA to DIC generally decreased northward. The spatial patterns of other CO2 system parameters closely followed those of the TA : DIC ratio. All sampled shelf waters were supersaturated with respect to aragonite (saturation state ΩA 〉 1). The most intensely buffered and supersaturated waters (ΩA 〉 5.0) were in northern Gulf of Mexico river-plume waters; the least intensely buffered and least supersaturated waters (ΩA 〈 1.3) were in the deep Gulf of Maine. Due to their relatively low pH, ΩA, and buffer intensity, waters of the northeastern U.S. shelves may be more susceptible to acidification pressures than are their southern counterparts. In the Mid-Atlantic Bight, alongshore mixing tended to increase DIC concentrations southward, but this effect was largely offset by the opposing effects of biogeochemical processing. In the Gulf of Mexico, downstream increases in Loop Current DIC suggested significant contributions from shelf and gulf waters, estimated at 9.1 × 109 mol C d−1. Off the southeastern U.S., along-flow chemical changes in the Florida Current were dominated by mixing associated with North Atlantic subtropical recirculation.
    Description: The study was supported by the NOAA Global Carbon Cycle Program, proposal GC05-208.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2022-10-31
    Description: Dataset: HPLC analysis
    Description: High pressure liquid chromatography analyses of photosynthetic pigments taken on the R/V Acadian and R/V Pelican from September to October 2017 in the Central northern Gulf of Mexico. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/789061
    Description: NSF Division of Ocean Sciences (NSF OCE) OCE-1760660, NSF Division of Ocean Sciences (NSF OCE) OCE-1760509
    Keywords: Phytoplankton pigments ; HPLC ; Gulf of Mexico ; Mississippi River ; Phytoplankton community
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 10
    facet.materialart.
    Unknown
    Biological and Chemical Oceanography Data Management Office (BCO-DMO). Contact: bco-dmo-data@whoi.edu
    Publication Date: 2022-10-31
    Description: Dataset: Discrete Samples
    Description: Dissolved inorganic carbon, total alkalinity and pH from R/V Pelican cruises conducted in the northern Gulf of Mexico (27.5 N, 30 N, 88 W, 94 W ) from April 5 to 16 and July 7 to 21 in 2017 For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/772513
    Description: NSF Division of Ocean Sciences (NSF OCE) OCE-1559279
    Keywords: Dissolved inorganic carbon ; Alkalinity ; Spectrophotometric pH ; Spring bloom ; Northern Gulf of Mexico
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...