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  • 1
    Monograph available for loan
    Monograph available for loan
    Cham : Springer International Publishing
    Call number: 5/M 14.0244
    Description / Table of Contents: This unitary resource sets out the derivation of conservation, thermodynamic, and evolution equations used in modeling multiphase porous media systems. It includes detailed, multiscale applications and a forward-looking discussion of open research issues. Thermodynamically constrained averaging theory provides a consistent method for upscaling conservation and thermodynamic equations for application in the study of porous medium systems. The method provides dynamic equations for phases, interfaces, and common curves that are closely based on insights from the entropy inequality. All larger scale variables in the equations are explicitly defined in terms of their microscale precursors, facilitating the determination of important parameters and macroscale state equations based on microscale experimental and computational analysis. The method requires that all assumptions that lead to a particular equation form be explicitly indicated, a restriction which is useful in ascertaining the range of applicability of a model as well as potential sources of error and opportunities to improve the analysis.
    Description / Table of Contents: Chapter 1 Elements of Thermodynamically Constrained Averaging Theory.- Chapter 2 Microscale Conservation Principles.- Chapter 3 Microscale Thermodynamics.- Chapter 4 Microscale Equilibrium Conditions.- Chapter 5 Microscale Closure for a Fluid Phase.- Chapter 6 Macroscale Conservation Principles.- Chapter 7 Macroscale Thermodynamics.- Chapter 8 Evolution Equations.- Chapter 9 Single-Fluid-Phase Flow.- Chapter 10 Single-Fluid-Phase Species Transport.- Chapter 11 Two-Phase Flow.- Chapter 12 Modeling Approach and Extensions.- Appendix A Considerations on Calculus of Variations.- Appendix B Derivations of Averaging Theorems.- Appendix C Constrained Entropy Inequality Derivations.- Index.
    Type of Medium: Monograph available for loan
    Pages: XXXIV, 582 S. : z.T. farb. Ill.
    ISBN: 9783319040097
    Series Statement: Advances in Geophysical and Environmental Mechanics and Mathematics
    Classification:
    Geophysics
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: MOP 44509 / Mitte
    Type of Medium: Monograph available for loan
    Pages: XXIII, 723 Seiten , Diagramme
    Language: English
    Location: MOP - must be ordered
    Branch Library: GFZ Library
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  • 3
    Publication Date: 2019-08-19
    Description: Planktic foraminifera census data have been used to reconstruct past temperatures through transfer functions, as well as changes in ocean ecosystems, chemistry and circulation. Here we present new multinet, plankton net and core-top census data from 20 sites in the Subpolar North Pacific. We combine these with previous data to provide an up to date compilation of North Pacific planktic foraminifera assemblage data. Our compilation is used to define 6 faunal zones: the subpolar zone; transitional zone; upwelling zone; subtropical zone; east equatorial zone; west equatorial zone; based on the distribution of 10 major species of planktic foraminifera. Two species of planktic foraminifera Neogloboquadrina pachyderma and Globigerina bulloides provide the basis for many subpolar paleo-reconstructions. Through the analysis of new multinet and CTD data we find that G. bulloides and N. pachyderma are predominantly found within 0–50 m of the water column and coincide with high food availability. N. pachyderma also shows a strong temperature control and can thrive in food poor waters where temperatures are low. Both species bloom seasonally, particularly during the spring bloom of March to June, with G. bulloides exhibiting greater seasonal variation. We suggest that percentage abundance of N. pachyderma in paleo-assemblages can be used to assess relative changes in past temperature, with G. bulloides abundance more likely to reflect changes in food availability. By comparing our core-top and multinet data, we also find a dissolution bias of G. bulloides over N. pachyderma in the North Pacific, which may enrich assemblages in the latter species.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 4
    Publication Date: 2022-11-06
    Description: Author Posting. © American Geophysical Union, 2022. 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 36(5), (2022): e2022GB007388, https://doi.org/10.1029/2022gb007388.
    Description: The cycling of biologically produced calcium carbonate (CaCO3) in the ocean is a fundamental component of the global carbon cycle. Here, we present experimental determinations of in situ coccolith and foraminiferal calcite dissolution rates. We combine these rates with solid phase fluxes, dissolved tracers, and historical data to constrain the alkalinity cycle in the shallow North Pacific Ocean. The in situ dissolution rates of coccolithophores demonstrate a nonlinear dependence on saturation state. Dissolution rates of all three major calcifying groups (coccoliths, foraminifera, and aragonitic pteropods) are too slow to explain the patterns of both CaCO3 sinking flux and alkalinity regeneration in the North Pacific. Using a combination of dissolved and solid-phase tracers, we document a significant dissolution signal in seawater supersaturated for calcite. Driving CaCO3 dissolution with a combination of ambient saturation state and oxygen consumption simultaneously explains solid-phase CaCO3 flux profiles and patterns of alkalinity regeneration across the entire N. Pacific basin. We do not need to invoke the presence of carbonate phases with higher solubilities. Instead, biomineralization and metabolic processes intimately associate the acid (CO2) and the base (CaCO3) in the same particles, driving the coupled shallow remineralization of organic carbon and CaCO3. The linkage of these processes likely occurs through a combination of dissolution due to zooplankton grazing and microbial aerobic respiration within degrading particle aggregates. The coupling of these cycles acts as a major filter on the export of both organic and inorganic carbon to the deep ocean.
    Description: This work was funded by NSF OCE-1220301 to W.B., NSF OCE-1220600 to J.F.A., and startup funding for A.V.S.
    Description: 2022-11-06
    Keywords: Calcium carbonate ; Dissolution ; Carbon cycle
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 5
    Publication Date: 2022-05-26
    Description: This is the second part in three of an observational study of tropical oceanic clouds and their relation to the large-scale flow patterns. The first part appeared in preliminary form in 1959 in a volume entitled "Cloud Structure am.d Distributions over the Tropical Pacific. Part I", an unpublished Technical Report (Reference No.58-62) of the Woods Hole Oceanographic Institution. The four authors were the same as those of this report. In addition, a very brief summary of the work (by J. Malkus and C. Ronne) was published in Monograph No.5 of the American Geophysical Union in 1960. A review of the cloud code evolved during this program has been published by M. Alaka in the Bulletin of World Meteorological Organization for April, 1960. The basic material for this study consists of three photographic flights made during July and August 1957 on Military Air Transport (MATS) cargo aircraft flying on regular schedules between San Francisco and the Phillipines. The photographer was Claude Ronne of Woods Hole, accompanied by Joanne Malkus om. the third flight. The appropriate synoptic data were kindly collected by Prof. Colin Ramage of the University of Hawaii and were analyzed by Professor Riehl (then at the University of Chicago) and his colleague Mr. W.S.Gray. The first report described the purposes and methods of the inquiry and presented the results of the first trans-Pacific flight. This report is concerned primarily with the results of the Second flight. A third report on the last flight is planned later, as well as eventual publication of all three parts together. The part of the program reported here has been supported jointly by the Office of Naval Research and the National Science Foundation.
    Description: Office of Naval Research under Contract No. 1721(00) and to the National Science Foundation under Grantt No.7368 with the Woods Hole Oceanographic Institution.
    Keywords: Clouds ; Marine meteorology--Tropics ; Pacific Ocean
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
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  • 6
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    PANGAEA
    In:  Supplement to: Drury, Anna Joy; Lee, Geoffrey P; Gray, William Robert; Lyle, Mitchell W; Westerhold, Thomas; Shevenell, Amelia E; John, Cédric M (2018): Deciphering the state of the late Miocene to early Pliocene equatorial Pacific. Paleoceanography and Paleoclimatology, 33, 246-263, https://doi.org/10.1002/2017PA003245
    Publication Date: 2023-03-06
    Description: The late Miocene-early Pliocene was a time of global cooling and the development of modern meridional thermal gradients. Equatorial Pacific sea surface conditions potentially played an important role in this global climate transition, but their evolution is poorly understood. Here, we present the first continuous late Miocene-early Pliocene (8.0-4.4 Ma) planktic foraminiferal stable isotope records from eastern equatorial Pacific Integrated Ocean Drilling Program Site U1338, with a new astrochronology spanning 8.0-3.5 Ma. Mg/Ca analyses on surface dwelling foraminifera Trilobatus sacculifer from carefully selected samples suggest mean sea-surface-temperatures (SSTs) are ~27.8±1.1°C (1 Sigma) between 6.4-5.5 Ma. The planktic foraminiferal d18O record implies a 2°C cooling between 7.2-6.1 Ma and an up to 3°C warming between 6.1-4.4 Ma, consistent with observed tropical alkenone paleo-SSTs. Diverging fine-fraction-to-foraminiferal d13C gradients likely suggest increased upwelling from 7.1-6.0 and 5.8-4.6 Ma, concurrent with the globally recognized late Miocene Biogenic Bloom. This study shows that both warm and asymmetric mean states occurred in the equatorial Pacific during the late Miocene-early Pliocene. Between 8.0-6.5 and 5.2-4.4 Ma, low east-west d18O and SST gradients and generally warm conditions prevailed. However, an asymmetric mean climate state developed between 6.5-5.7 Ma, with larger east-west d18O and SST gradients and eastern equatorial Pacific cooling. The asymmetric mean state suggests stronger trade winds developed, driven by increased meridional thermal gradients associated with global cooling and declining atmospheric pCO2 concentrations. These oscillations in equatorial Pacific mean state are reinforced by Antarctic cryosphere expansion and related changes in oceanic gateways (e.g., Central American Seaway/Indonesian Throughflow restriction).
    Keywords: Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 7
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    Unknown
    PANGAEA
    In:  Supplement to: Taylor, Ben J; Rae, James W B; Gray, William Robert; Darling, Kate F; Burke, Andrea; Gersonde, Rainer; Abelmann, Andrea; Maier, Edith; Esper, Oliver; Ziveri, Patrizia (2018): Distribution and ecology of planktic Foraminifera in the North Pacific: Implications for paleo-reconstructions. Quaternary Science Reviews, 191, 256-274, https://doi.org/10.1016/j.quascirev.2018.05.006
    Publication Date: 2023-03-06
    Description: Planktic foraminifera census data have been used to reconstruct past temperatures through transfer functions, as well as changes in ocean ecosystems, chemistry and circulation. Here we present new multinet, plankton net and core-top census data from 20 sites in the Subpolar North Pacific. We combine these with previous data to provide an up to date compilation of North Pacific planktic foraminifera assemblage data. Our compilation is used to define 6 faunal zones: the subpolar zone; transitional zone; upwelling zone; subtropical zone; east equatorial zone; west equatorial zone; based on the distribution of 10 major species of planktic foraminifera. Two species of planktic foraminifera Neogloboquadrina pachyderma and Globigerina bulloides provide the basis for many subpolar paleo-reconstructions. Through the analysis of new multinet and CTD data we find that G. bulloides and N. pachyderma are predominantly found within 0-50 m of the water column and coincide with high food availability. N. pachyderma also shows a strong temperature control and can thrive in food poor waters where temperatures are low. Both species bloom seasonally, particularly during the spring bloom of March to June, with G. bulloides exhibiting greater seasonal variation. We suggest that percentage abundance of N. pachyderma in paleo-assemblages can be used to assess relative changes in past temperature, with G. bulloides abundance more likely to reflect changes in food availability. By comparing our core-top and multinet data, we also find a dissolution bias of G. bulloides over N. pachyderma in the North Pacific, which may enrich assemblages in the latter species.
    Keywords: AWI
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 8
    Publication Date: 2023-03-06
    Description: The 26,000-year long time-series analyzed in a marine sediment core from the northern Bay of Bengal includes Mg/Ca-based SST estimates, Ba/Ca-based mixed layer salinity estimates, and estimates of ice-volume corrected d18O of the mixed layer. The data are provide new insights into the control of Indian Summer Monsoon over the last 26,000 years, including a strong influence of zonal and meridional SST gradient changes within the tropical Indian Ocean on Indian Summer Monsoon variability.
    Keywords: Ba/Ca-based salinitt estimates; Bay of Bengal; Holocene climate variability; Indian Monsoon; Indian Ocean Dipole; last deglaciation; Last Glacial Maximum; Mg/Ca-based paleotemperatures; runoff; Salinity; Temperature
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 9
    Publication Date: 2023-03-06
    Keywords: AWI; Bering Sea; Chlorophyll a; CTD/Rosette; CTD-RO; Date/Time of event; DEPTH, water; Elevation of event; Event label; INOPEX; Latitude of event; Longitude of event; North Pacific Ocean; Oxygen; Salinity; SO202/1; SO202/1_02-1; SO202/1_10-1; SO202/1_13-1; SO202/1_14-1; SO202/1_15-1; SO202/1_27-2; SO202/1_31-1; SO202/1_33-1; SO202/1_34-1; Sonne; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 35893 data points
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  • 10
    Publication Date: 2023-03-06
    Keywords: AWI; Bering Sea; Date/Time of event; Depth, bottom/max; Depth, top/min; DEPTH, water; Elevation of event; Event label; Foraminifera, planktic; Globigerina bulloides; Globigerinella siphonifera; Globigerinita glutinata; Globigerinoides ruber; Globoconella inflata; Globorotalia scitula; Globorotaloides hexagonus; INOPEX; Latitude of event; Longitude of event; MSN; Multiple opening/closing net; Neogloboquadrina dutertrei; Neogloboquadrina incompta; Neogloboquadrina pachyderma sinistral; North Pacific Ocean; SO202/1; SO202/1_02-5; SO202/1_10-4; SO202/1_13-3; SO202/1_14-4; SO202/1_15-3; SO202/1_27-4; SO202/1_31-2; SO202/1_33-2; SO202/1_34-2; Sonne; Turborotalita quinqueloba
    Type: Dataset
    Format: text/tab-separated-values, 574 data points
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