Relevant bibliographies by topics / Geophysical ows

Academic literature on the topic 'Geophysical ows'

Author: Grafiati
Published: 11 March 2023

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Journal articles on the topic "Geophysical ows"

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Kilic, Lise, Catherine Prigent, Carlos Jimenez, and Craig Donlon. "Technical note: A sensitivity analysis from 1 to 40 GHz for observing the Arctic Ocean with the Copernicus Imaging Microwave Radiometer." Ocean Science 17, no. 2 (March 11, 2021): 455–61. http://dx.doi.org/10.5194/os-17-455-2021.

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Abstract. The Copernicus Imaging Microwave Radiometer (CIMR) is one of the high-priority missions for the expansion of the Copernicus program within the European Space Agency (ESA). It is designed to respond to the European Union Arctic policy. Its channels, incidence angle, precision, and spatial resolutions have been selected to observe the Arctic Ocean with the recommendations expressed by the user communities. In this note, we present the sensitivity analysis that has led to the choice of the CIMR channels. The famous figure from Wilheit (1979), describing the frequency sensitivity of passive microwave satellite observations to ocean parameters, has been extensively used for channel selection of microwave radiometer frequencies on board oceanic satellite missions. Here, we propose to update this sensitivity analysis, using state-of-the-art radiative transfer simulations for different geophysical conditions (Arctic, mid-latitude, tropics). We used the Radiative Transfer Model (RTM) from Meissner and Wentz (2012) for the ocean surface, the Round Robin Data Package of the ESA Climate Change Initiative (Pedersen et al., 2019) for the sea ice, and the RTM from Rosenkranz (2017) for the atmosphere. The sensitivities of the brightness temperatures (TBs) observed by CIMR as a function of sea surface temperature (SST), sea surface salinity (SSS), sea ice concentration (SIC), ocean wind speed (OWS), total column water vapor (TCWV), and total column liquid water (TCLW) are presented as a function of frequency between 1 and 40 GHz. The analysis underlines the difficulty to reach the user requirements with single-channel retrieval, especially under cold ocean conditions. With simultaneous measurements between 1.4 and 36 GHz onboard CIMR, applying multi-channel algorithms will be facilitated, to provide the user community with the required ocean and ice information under arctic environments.
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Giga, Yoshikazu, Matthias Hieber, and Edriss Titi. "Geophysical Fluid Dynamics." Oberwolfach Reports 10, no. 1 (2013): 521–77. http://dx.doi.org/10.4171/owr/2013/10.

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Giga, Yoshikazu, Matthias Hieber, and Edriss Titi. "Geophysical Fluid Dynamics." Oberwolfach Reports 14, no. 2 (April 27, 2018): 1421–62. http://dx.doi.org/10.4171/owr/2017/23.

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Klein, Rupert, Shafer Smith, and Jacques Vanneste. "Multiscale Interactions in Geophysical Fluids." Oberwolfach Reports 13, no. 3 (2016): 2225–68. http://dx.doi.org/10.4171/owr/2016/39.

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Giga, Yoshikazu, Matthias Hieber, Peter Korn, and Edriss S. Titi. "Mathematical Advances in Geophysical Fluid Dynamics." Oberwolfach Reports 17, no. 2 (July 1, 2021): 857–76. http://dx.doi.org/10.4171/owr/2020/15.

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Waldner, Jeffrey, Jeffrey Reidenauer, Lora Turner, Paul Knorr, and Leighann Brandt. "BUILDING A NATIONAL SAND RESOURCE INVENTORY FOR THE US CONTINENTAL SHELF." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 88. http://dx.doi.org/10.9753/icce.v36.sediment.88.

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The future of coastal resilience or restoration plans which implement natural or nature-based features largely depends upon the identification of proximate and compatible offshore sand and gravel material. BOEM’s Marine Minerals Program (MMP) is multi-faceted, focusing on coordinated leasing of sediment for extraction, inventorying sediment resources through geological and geophysical surveys of the Outer Continental Shelf (OCS), and environmental studies and reviews to inform decisions. However, on a national scale, little is known about the character, quantity, and location of sand resources on the OCS and the habitat it provides for biological communities. BOEM places a high priority on creating a comprehensive national sand resource inventory to meet BOEM’s mandate as stewards of all federal mineral resources on the OCS. This stewardship responsibility will be realized by proactively planning for the increasing demands for OCS resources and emergency needs as they arise.
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Wang, Jing, Jianhe Guan, and Donglin Liu. "Research and Application of FAHP in Bidding Quotation for Petroleum Geophysical Prospecting Project." Open Journal of Statistics 07, no. 04 (2017): 589–98. http://dx.doi.org/10.4236/ojs.2017.74040.

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Carr, S., J. K. Pringle, P. Doyle, K. D. Wisniewski, and I. G. Stimpson. "Scallywag bunkers: geophysical investigations of WW2 Auxiliary Unit Operational Bases (OBs) in the UK." Journal of Conflict Archaeology 15, no. 1 (January 2, 2020): 4–31. http://dx.doi.org/10.1080/15740773.2020.1822102.

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Tian, Jinyu, Jian Lin, Fan Zhang, Min Xu, Yayun Zhang, Laiyin Guo, and Xin Zeng. "Time Correction of Ocean-Bottom Seismometers Using Improved Ambient Noise Cross Correlation of Multicomponents and Dual-Frequency Bands." Seismological Research Letters 92, no. 3 (January 13, 2021): 2004–14. http://dx.doi.org/10.1785/0220200358.

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Abstract An effective approach was developed for identifying and correcting ocean-bottom seismometer (OBS) time errors through improving ambient noise cross-correlation function (NCCF) analysis and combination with other methods. Significant improvements were illustrated through analyzing data from a passive-source seismic experiment in the southwestern sub-basin of the South China Sea. A novel method was first developed that can effectively identify errors in the sampling frequency of the OBS instruments. The traditional NCCF method was then expanded by increasing the analyzed data spectrum from a single-frequency band to dual-frequency band pairs, thus doubling the number of available data points and substantially improving the time correction quality. For data with relatively low signal-to-noise ratios, the average time errors were reduced from the original average values of 60–80 ms by the conventional methods to <40 ms using the improved approaches. The new multistep procedure developed in this study has general applicability to analysis of other OBS experiments. The demonstrated significant improvements in the data quality are critical for advancing seismic tomography and other modern marine geophysical studies that require high accuracy in the OBS data.
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Tonka, Şebnem Karul, and Ismail Ekmekci. "A Model Proposal for Occupational Health and Safety Performance Measurement in Geothermal Drilling Areas." Sustainability 14, no. 23 (November 24, 2022): 15669. http://dx.doi.org/10.3390/su142315669.

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The energy sources required for general development and maintenance cause environmental pollution due to the carbon emissions released into the atmosphere. For these reasons, countries have turned to renewable energy sources. Energy production methods also cause serious problems in terms of the health and safety of employees. This study aimed to create an occupational health and safety performance model in geothermal energy fields, which generate renewable energy sources, using multi-criteria decision-making methods. A two-stage model was created for OHS performance index measurement. In the first stage, a literature screening was performed, risk analysis criteria were examined, and performance measurement criteria were determined with geophysical engineers and OHS experts. Seven main criteria and forty-seven subcriteria were set. An analytical hierarchy process method (AHP) and a fuzzy analytical hierarchy process (F-AHP) using the main criteria and subcriteria were determined. In the second stage, exposure rates were obtained using the Promethee method in three geothermal wells. The risks in these three wells are listed according to their importance. A performance model was created. The Results section includes conclusions and suggestions. This study, by creating an OHS performance model, can be used by managers and OHS professionals working in geothermal energy production fields to solve problems.
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Books on the topic "Geophysical ows"

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M, Isaacs Caroline, and Geological Survey (U.S.), eds. Abundances of major elements and sedimentary components in cuttings from the Foxen, Sisquoc, Monterey, and Point Sal Formations, OCS P-0315-1 well, Point Arguello oil field, offshore Santa Maria basin, southern California. [Menlo Park, CA]: U.S. Dept. of the Interior, U.S. Geological Survey, 1993.

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United States. Minerals Management Service., ed. GEOLOGICAL & GEOPHYSICAL DATA ACQUISITION, OUTER CONTINENTAL SHELF THROUGH 1999... RESOURCE EVALUATION PROGRAM REPORT... OCS REPORT 2000-071. [S.l: s.n., 2001.

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United States. Minerals Management Service., ed. GEOLOGICAL & GEOPHYSICAL DATA ACQUISITION, OUTER CONTINENTAL SHELF THROUGH 1999... RESOURCE EVALUATION PROGRAM REPORT... OCS REPORT 2000-071. [S.l: s.n., 2001.

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United States. Bureau of Ocean Energy Management. Gulf of Mexico OCS Region. Atlantic OCS proposed geological and geophysical activities Mid-Atlantic and South Atlantic planning areas final programmatic environmental impact statement. New Orleans: U.S. Department of the Interior, Bureau of Ocean Energy Management, Gulf of Mexico OCS Region, 2014.

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United States. Minerals Management Service, ed. GEOLOGICAL & GEOPHYSICAL DATA ACQUISITION, OUTER CONTINENTAL SHELF THROUGH 2002... RESOURCE EVALUATION PROGRAM..., OCS REPORT MMS 2004-003... U.S. DEPARTMENT OF THE INTERIOR. [S.l: s.n., 2004.

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United States. Minerals Management Service, ed. Geological & Geophysical Data Acquisition, Outer Continental Shelf Through 2000... Resource Evaluation Program Report... OCS Report MMS 2001-092... U.S. Department Of The Interior. [S.l: s.n., 2002.

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United States. Minerals Management Service., ed. Geological & Geophysical Data Acquistion, Outer Continental Shelf Through 2000... Resource Evaluation Program Report... OCS Report MMS 2001-092... U.S. Department Of The Interior. [S.l: s.n., 2002.

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United States. Minerals Management Service., ed. Geological & Geophysical Data Acquistion, Outer Continental Shelf Through 2000... Resource Evaluation Program Report... OCS Report MMS 2001-092... U.S. Department Of The Interior. [S.l: s.n., 2002.

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United States. Minerals Management Service., ed. Geological & Geophysical Data Acquistion, Outer Continental Shelf Through 2000... Resource Evaluation Program Report... OCS Report MMS 2001-092... U.S. Department Of The Interior. [S.l: s.n., 2002.

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GEOLOGICAL & GEOPHYSICAL DATA ACQUISITION, OUTER CONTINENTAL SHELF THROUGH 1999... RESOURCE EVALUATION PROGRAM REPORT... OCS REPORT 2000-071. [S.l: s.n., 2001.

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Book chapters on the topic "Geophysical ows"

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Liu, Daniel. "Scaling from Weather to Climate." In Cultural Inquiry, 93–117. Berlin: ICI Berlin Press, 2020. http://dx.doi.org/10.37050/ci-17_05.

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One of the theoretical tensions that has arisen from Anthropocene studies is what Dipesh Chakrabarty has called the ‘two figures of the human’, and the question of which of these two figures of the human inheres in the concept of the Anthropocene more. On the one hand, the Human is conceived as the universal reasoning subject upon whom political rights and equality are based, and on the other hand, humankind is the collection of all individuals of our species, with all of the inequalities, differences, and variability inherent in any species category. This chapter takes up Deborah Coen’s argument that Chakrabarty’s claim of the ‘incommensurability’ of these two figures of the human ignores the way both were constructed within debates over how to relate local geophysical specificities to theoretical generalities. This chapter examines two cases in the history of science. The first is Martin Rudwick’s historical exploration of how geologists slowly gained the ability to use fossils and highly local stratigraphic surveys to reconstruct the history of the Earth in deep time, rather than resort to speculative cosmological theory. The second is Coen’s own history of imperial, Austrian climate science, a case where early nineteenth-century assumptions about the capriciousness of the weather gave way to theories of climate informed by thermodynamics and large-scale data collection.
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Oreskes, Naomi. "The Depersonalization of Geology." In The Rejection of Continental Drift. Oxford University Press, 1999. http://dx.doi.org/10.1093/oso/9780195117325.003.0018.

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Some historians have concluded that plate tectonics caused a change in the standards of the geological community, but the shift in standards of the American scientific community was not so much the result of the development of plate tectonics as it was a larger trend that helped to cause it. Geologists consciously chose to move their discipline away from observational field studies and an inductive epistemic stance toward instrumental and laboratory measurements and a more deductive stance. This shift helps to explain why geologists felt compelled to attend to the demands of geodesists even at the expense of their own data: it was the geodesists’ data, rather than their own, that seemed to be in the vanguard of their science. Geologists at the start of the twentieth century had high hopes for their discipline, and they were not disappointed. The Carnegie Institution’s Geophysical Laboratory became one of the world’s leading locales for laboratory investigations of geological processes, and work done there inspired scientists at other American institutions. At Harvard, for example, Reginald Daly joined forces with Percy Bridgman to raise funds for a high pressure laboratory to determine the physical properties of rocks under conditions prevailing deep within the earth. The application of physics and chemistry to the earth was also advanced at the Carnegie’s Department of Terrestrial Magnetism, where scientists pursued geomagnetism, isotopic dating, and explosion seismology.’ By mid-century, the origins of igneous and metamorphic rocks had been explained, the age of the earth accurately determined, the behavior of rocks under pressure elucidated, and the nature of isostatic compensation resolved, largely through the application of instrumental and laboratory methods. Similar advances occurred in geophysics and oceanography. The work that Bowie and Field instigated in cooperation with the U.S. Navy, and that scientists at places like Wood’s Hole and the Scripps Institution of Oceanography greatly furthered, had grown by the 1950s into a fully fledged science of marine geophysics and oceanography with abundant financial and logistical backing. This work —in gravity, magnetics, bathymetry, acoustics, seismology— relied on instrumentation, much of it borrowed from physics.
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Deamer, David W. "The Early Earth: An Ocean with Volcanoes." In Assembling Life. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780190646387.003.0006.

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Malcolm Walter was talking about the Pilbara region of Western Australia where some of the oldest known biosignatures of ancient life, in the form of extensive fossilized stromatolites, are preserved. The first potential stromatolite was discovered by graduate student John Dunlop, who was studying barite deposits at the North Pole Dome. Roger Buick went on to investigate the biogenicity of the stromatolites for his PhD (Buick, 1985) and Dunlop, Buick, and Walter published their results (Walter et al., 1980). In a prescient paper, Walter and Des Marais (1993) proposed that the ancient stromatolite fossils could guide the search for life on Mars. I have walked with Malcolm Walter through the Dresser formation where the fossils were found. It is humbling to realize that if time passed at a thousand years per second, it would take 41 days to go back in time to the first signs of life on our planet. In any description of events that occurred some 4 billion years ago, certain assumptions must be made. I will try to make assumptions explicit throughout this book, beginning here with the geochemical and geophysical conditions prevailing on the early Earth and Mars. I am including Mars not as an afterthought but because both planets had liquid water 4 billion years ago. Most of our understanding of planetary evolution comes from observations of our own planet, but it is now clear that the Earth and Mars were undergoing similar geophysical processes during the first billion years of the solar system’s existence, with an equal probability that life could begin on either planet. In a sense, the surface of Mars is a geological fossil that has preserved evidence of what was happening there at the same time that life began on the Earth. For instance, Martian volcanoes offer direct, observable evidence that volcanism was occurring nearly 4 billion years ago; making it plausible that similar volcanism was common on Earth even though the evidence has been completely erased by geological and tectonic processes.
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"Institute of Oceanography and Applied Geophysics (Instituto Nazionale di Oceanografia e di Geofisica Sperimentale, OGS)." In The Adriatic Sea Encyclopedia, 165–66. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-50032-0_250.

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SUTER, JOHN R., KENNETH C. ABDULAH, PATTY D. TRAVIS, PETER A. GLAGOLA, JAMES W. YOUNG, DAVID C. WATSO, WILLIAM E. FINLEY, Joseph R. Davis, and David A. Scolman. "An Integrated Seismic and Well-Log Sequence Stratigraphic Study Over 32 Grand Isle/West Delta OCS Blocks." In Stratigraphic Analysis Utilizing Advanced Geophysical, Wireline and Borehole Technology for Petroleum Exploration and Productioni: 17th Annual, 305–13. SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS, 1996. http://dx.doi.org/10.5724/gcs.96.17.0305.

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"Benthic Habitats and the Effects of Fishing." In Benthic Habitats and the Effects of Fishing, edited by J. A. REID, C. J. JENKINS, M. E. FIELD, M. ZIMMERMANN, S. J. WILLIAMS, J. M. CURRENCE, C. E. BOX, and J. V. GARDNER. American Fisheries Society, 2005. http://dx.doi.org/10.47886/9781888569605.ch33.

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The identification of benthic habitat is based, in part, on its underlying geologic character. While some geologic characteristics can be inferred through bathymetry and remotely sensed imagery, knowledge based on actual sampling of the seabed, either through cores or through photography, can be expensive to collect, and in the latter case, difficult to quantify and assess. Hundreds of thousands of sediment cores, photographs, and videos have been collected along the continental shelves of the United States, in very large and very small research efforts, for various purposes and using a variety of equipment. We unify these sets, both numerical lab-based data and word-based data from from core logs, photos, and videos, where we apply fuzzy set theory to parse values from graphed meanings. These quantified combined data are mined for information useful for geologists, biologists, and ecologists into an linked information system, usSEABED, mappable in GISs and queriable in RDBs. We present a ever-growing integrated look at the character of the surficial seabed of the United States (to about 100m depth, where available) that includes textural information, degree of hardness, presence of biota, basic chemistry, and critical shear strength, to name a few. While these data are useful in their own right, most data held within usSEABED are available as baselines for habitat identification and assessment, or in combination with oceanographic, biologic, or geophysical data to a more complete understanding of a variety of critical processes necessary for effective resource management.
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Fleming, James R. "Global Cooling, Global Warming: Historical Dimensions." In Historical Perspectives on Climate Change. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195078701.003.0015.

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I have chosen to conclude these essays just as the well-known IGY was getting started. Of course, much has changed since then. There is little to gain, however, by attempting to recount the recent policy history of global change, at least from my perspective as a historian of science and technology. I have tried in this book to provide fresh perspectives on the more distant past, not to replicate the recent literature on global change. Although I am actively engaged in projects sponsored by the American Meteorological Society and the American Geophysical Union that document the recent past, I have little inclination to attempt to interpret it. Consequently I include in this chapter only the briefest sketch of the global cooling scare after 1958 and the return of a global warming discourse in the 1980s. I believe the metaphor of apprehension (awareness, understanding, fear, intervention) applies quite well to a number of current environmental issues, and I will point to some of them by way of conclusion. I was asked once after a seminar whether, as a historian, I could predict the eventual demise of today’s global change discourse, since there had been so many changes in the past. I responded that history has no predictive value, but does indeed provide valuable perspectives to its readers. History is first and foremost the study of change. For students of global change, history can serve as an inspirational story of how far we have come. It can also serve as a humbling reminder that change is indeed inevitable in our lives, in the Earth system, and in our ideas and institutions. Although I am professionally engaged with the past, I am still a citizen of my own age—an age of vastly enhanced environmental awareness. Like many of my contemporaries, I believe that humanity is a part of, not apart from, nature; that human activity is placing tremendous stress on global biophysical systems; and that we have an ethical responsibility to each other and to future generations to live sustainably, in harmony with the Earth. Your guesses about the future are probably as good as and perhaps better than mine.
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Conference papers on the topic "Geophysical ows"

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Lou, Bing, Hong‐ming Zheng, and Hong‐xian Guo. "The application of Common‐Reflection‐Surface stacking method (CRS‐OIS)." In Beijing 2009 International Geophysical Conference and Exposition. Society of Exploration Geophysicists, 2009. http://dx.doi.org/10.1190/1.3603618.

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Janneh, M., F. A. Bruno, S. Guardato, G. P. Donnarumma, G. Iannaccone, G. Gruca, S. Werzinger, et al. "Fiber optic hydrophones for geophysical and volcanological monitoring." In Optical Fiber Sensors. Washington, D.C.: Optica Publishing Group, 2022. http://dx.doi.org/10.1364/ofs.2022.w4.6.

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Here, we report on the development and field test of a fiber optic seismic hydrophone. The sensing configuration exploits a fiber coil interferometer in Michelson configuration, wrapped around a sensitive composite cylinder. The materials and the size of the hydrophone were selected by numerical analysis in order to offer performance suitable to operate with resolution down to the sea state zero in underwater environments. The sensing system was integrated in the seismological monitoring system of the Campi Flegrei caldera. During the field trials, we detected several earthquakes occurred in the area and compared the results with a reference piezoelectric hydrophone. The seismic sequence was used to retrieve the sensor responsivity in the frequency range 1-80Hz. The sensing system exhibited a responsivity of about -300nm/Pa and an average noise floor level down to 100µPa/√Hz. The reported field trial demonstrated the capability of optical fiber hydrophones to operate for geophysical and volcanological monitoring.
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Missiaen, Tine, and Pascal Feller. "Geophysical investigations of a chemical munition dumpsite in the Baltic Sea." In 2008 IEEE/OES US/EU-Baltic International Symposium (BALTIC). IEEE, 2008. http://dx.doi.org/10.1109/baltic.2008.4625510.

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Pestana, Reynam. "Migrac¸ ˜ao Kirchhoff em Profundidade de Sec¸ ˜oes de Ondas Planas." In 9th International Congress of the Brazilian Geophysical Society. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.160.sbgf328.

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Evans, Amanda M., and Erin E. Voisin. "Geophysics, Industry, and Shipwrecks on the Gulf of Mexico OCS." In Offshore Technology Conference. Offshore Technology Conference, 2011. http://dx.doi.org/10.4043/21697-ms.

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Paffenholz, J., R. Shurtleff, D. Hays, and P. Docherty. "Evolution of a Multicomponent Autonomous OBS – The Role of Geophysics." In EAGE/SEG Research Workshop - Multicomponent Seismic - Past, Present and Future. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.17.a12.

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C. Sprinceana, V., A. Popescu, C. Petrescu, S. T A Prisecaru, M. Nedelcu, V. Zorilescu, and M. Albaiu. "Synoptic Aero Magnetic And Gravity Maps Implementation Of The Oas – Gutai – Tibles Mountains (Romania)." In 4th Congress of the Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.26.p3-05.

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Yu*, Pengfei, and Jianhua Geng. "Vector-decomposition-based acoustic-elastic coupled equation for OBS data V-ERTM." In International Geophysical Conference, Qingdao, China, 17-20 April 2017. Society of Exploration Geophysicists and Chinese Petroleum Society, 2017. http://dx.doi.org/10.1190/igc2017-222.

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Dordea, D., V. Sprinceana, and A. DobrescuProspectiuni S.A. "Tectonic Alignments Analysis In Oas-Gutai Mts. Area (Nw Romania) By Remote Sensing And Geophysical Methods." In 4th Congress of the Balkan Geophysical Society. European Association of Geoscientists & Engineers, 2005. http://dx.doi.org/10.3997/2214-4609-pdb.26.o13-03.

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Felix, Cesar A., Thiago S. Martins, Camila H. C. Soares, Vanessa Guesser, Larissa F. Demarco, Beau Suthard, Rodrigo C. Barletta, Jorge A. G. Souza, and Michel M. de Mahiques. "Some limitations of shallow water geophysical devices imposed by different oceanographic and geological conditions." In 2013 IEEE/OES Acoustics in Underwater Geosciences Symposium (RIO Acoustics). IEEE, 2013. http://dx.doi.org/10.1109/rioacoustics.2013.6684000.

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