Relevant bibliographies by topics / Sea Change

Academic literature on the topic 'Sea Change'

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Published: 4 June 2021
Last updated: 19 February 2023

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Journal articles on the topic "Sea Change"

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Sgro, Gaetan. "Sea Change." Annals of Internal Medicine 162, no. 2 (January 20, 2015): 99. http://dx.doi.org/10.7326/m14-1074.

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Grimm, David. "Sea Change." Science 377, no. 6601 (July 2022): 18–21. http://dx.doi.org/10.1126/science.add6833.

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Perkins, Sid. "Sea Change." Science News 166, no. 3 (July 17, 2004): 35. http://dx.doi.org/10.2307/4015538.

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Power, Marjorie. "Sea Change." Psychological Perspectives 52, no. 4 (November 18, 2009): 504–5. http://dx.doi.org/10.1080/00332920903306833.

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de Boer, Agatha M. "Sea change." Nature Geoscience 3, no. 10 (September 12, 2010): 668–69. http://dx.doi.org/10.1038/ngeo963.

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Barusch, Amanda. "Sea Change." Journal of Aging, Humanities, and the Arts 2, no. 3-4 (December 17, 2008): 291–92. http://dx.doi.org/10.1080/19325610802558035.

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Collins, Al. "Sea Change." Jung Journal 8, no. 4 (October 2, 2014): 87–92. http://dx.doi.org/10.1080/19342039.2014.930013.

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Ré, R. N., E. D. Frohlich, and L. G. Navar. "Sea change." Hypertension 23, no. 3 (March 1994): 273–74. http://dx.doi.org/10.1161/01.hyp.23.3.273.

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Anonymous. "Sea change." Eos, Transactions American Geophysical Union 77, no. 9 (February 27, 1996): 82. http://dx.doi.org/10.1029/96eo00053.

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Schiffman, Richard. "Sea change." New Scientist 233, no. 3116 (March 2017): 22–23. http://dx.doi.org/10.1016/s0262-4079(17)30468-2.

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Dissertations / Theses on the topic "Sea Change"

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Vice, President Research Office of the. "Sea Change." Office of the Vice President Research, The University of British Columbia, 2009. http://hdl.handle.net/2429/9510.

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Jakub, Lucy(Lucy Marita). "Sea of change." Thesis, Massachusetts Institute of Technology, 2020. https://hdl.handle.net/1721.1/130207.

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Thesis: S.M., Massachusetts Institute of Technology, Department of Humanities, September, September, 2020
Cataloged from student-submitted PDF version of thesis.
Includes bibliographical references (pages 13-16).
The Gulf of Maine is warming at a faster rate than 99.9 percent of the world ocean, a trend with uncertain implications for the last great maritime fishery: American lobster. Every year, fishermen, scientists, and managers wait to see if the fishery reverses its fantastic growth, which has been a salutary effect of climate change over the past three decades. The gulf has as many horizons as it has islands, and nobody knows the whole thing. Like the story of the blind men and the elephant, every person you ask, even the most expert, will describe a different gulf to you, and a different crisis. What's clear is that the ecosystems of the region have been shaped by many different pressures: domesticated by management, depleted by overfishing, shuffled by natural climatic cycles. The future of the gulf will depend not just on the trajectory of ocean warming, but on whether people can rethink the way we use the environment, and adapt to a changing world.
by Lucy Jakub.
S.M.
S.M. Massachusetts Institute of Technology, Department of Humanities
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Sandin, Jetta Christine. "Sea Change or Charade." Thesis, Boston College, 2004. http://hdl.handle.net/2345/475.

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Thesis advisor: Timothy W. Crawford
Following the devastation UN peacekeeping experienced in the 1990s, the United Nations Panel on Peace Operations wrote a report, known as the Brahimi Report, that contained twenty key recommendations as how to make peacekeeping more effective and efficient. These recommendations addressed certain fundamental flaws in peacekeeping practices and procedures. This paper discusses the purpose behind several key recommendations and examines the political and internal debate surrounding their implementation. It addresses the effect of the Brahimi Report on UN reform and concludes that the Brahimi Report has spurred a long needed examination of peacekeeping and has influenced progress in most areas, even though most of the actual suggestions of the Panel were not followed
Thesis (BA) — Boston College, 2004
Submitted to: Boston College. College of Arts and Sciences
Discipline: Political Science
Discipline: College Honors Program
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Hentati-Sundberg, Jonas. "SEA CHANGE : Social-ecological co-evolution in Baltic Sea fisheries." Doctoral thesis, Stockholms universitet, Stockholm Resilience Centre, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-122372.

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Sustainable management of natural resources requires an in-depth understanding of the interplay between social and ecological change. Linked social-ecological systems (SES) have been described as complex adaptive systems (CAS), which mean that they are irreducible, exhibit nonlinear dynamics, have interactions across scales and are uncertain and unpredictable. These propositions have however rarely been tested empirically, in part due to a lack of methodological approaches and suitable datasets. In this thesis, I address this methodological and empirical gap in a study of long-term change of Baltic Sea fisheries. In Paper I, we develop the concept of fishing style through integrating multivariate statistical analysis and in-depth interviews. We thereby identify an intermediate level of detail for analyzing social-ecological dynamics, embracing the case specific and context dependent approaches of the social sciences with the generalizable and quantifiable approaches from the natural sciences. In Paper II we ask: How has the Baltic Sea fishery been regulated over time, and can we identify a way to quantify regulations in order to be able to analyze their effects? We analyze all regulatory changes in Sweden since 1995 with a new methodology and conclude that there is a clear trend towards increased micro-management. In Paper III, we use the fishing styles developed in Paper I and examine how they have changed over time. We relate these changes to the dynamics of regulation (Paper II), as well as to the dynamics of fish stocks and prices. We conclude that regulation has been the main driving force for observed changes, but also that regulation has prompted significant specialization and decline in flexibility for fishers over time. These changes are unintended consequences and may represent a looming risk for the long-term sustainability of this social-ecological system. Paper IV zooms in on a particular fishery, the pelagic trawl fishery for sprat Sprattus sprattus and Atlantic herring Clupea harengus, mainly targeted for the production of fishmeal and fish oil. Suspicions of non-compliance in this fishery motivated us to apply a statistical approach where we used socioeconomic data to re-estimate the historical catches in this fishery (a novel approach to catch-reconstruction estimates). We found that catches had been significantly underreported over several years, with consequences for the quality of stock assessments and management. The study underlines the importance of understanding linked social, economic and ecological dynamics for sustainable outcomes. Finally, Paper V takes a longer historical look at the Baltic Sea fishery, using regionally disaggregated data from 1914-2009 (96 years), which were analyzed with a novel type of nonlinear statistical time-series methods (Empirical Dynamical Modeling). Our analysis explicitly recognized the potential nonlinear dynamics of SES and showed high predictability across regions of catches and prices of cod Gadus morhua and herring. The signal was generally nonlinear and predictability decreased strongly with time, suggesting that the dynamics of this SES are ever-changing. To our knowledge, this is the first long-term analysis of a SES using empirical data and methods developed from the CAS field of research. The main contributions of this thesis are the integrated analysis of social and ecological data, the development of novel methods for understanding SES dynamics, insights on the ever-changing nature of CAS and the quantitative analysis of management outcomes. Future work should focus on assessing the generality of these findings across a broad range of SES and evaluate alternative governance approaches given the complexity and uncertainty of SES suggested by this thesis.

At the time of the doctoral defense, the following paper was unpublished and had a status as follows: Paper 5: Manuscript.

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Daly, Julia. "Late holocene sea-level change around Newfoundland." Fogler Library, University of Maine, 2002. http://www.library.umaine.edu/theses/pdf/DalyJ2002.pdf.

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Desflots, Melicie. "Environmental and Internal Controls of Tropical Cyclones Intensity Change." Scholarly Repository, 2008. http://scholarlyrepository.miami.edu/oa_dissertations/120.

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Tropical cyclone (TC) intensity change is governed by internal dynamics (e.g. eyewall contraction, eyewall replacement cycles, interactions of the inner-core with the rainbands) and environmental conditions (e.g. vertical wind shear, moisture distribution, and surface properties). This study aims to gain a better understanding of the physical mechanisms responsible for TC intensity changes with a particular focus to those related to the vertical wind shear and surface properties by using high resolution, full physics numerical simulations. First, the effects of the vertical wind shear on a rapidly intensifying storm and its subsequent weakening are examined. Second, a fully coupled atmosphere-wave-ocean model with a sea spray parameterization is used to study the impact of sea spray on the hurricane boundary layer. The coupled model consists of three components: the high resolution, non-hydrostatic, fifth generation Pennsylvania State University-NCAR mesoscale model (MM5), the NOAA/NCEPWAVEWATCH III (WW3) ocean surface wave model, and theWHOI threedimensional upper ocean circulation model (3DPWP). Sea spray parameterizations were developed at NOAA/ESRL and modified by the author to be introduced in uncoupled and coupled simulations. The model simulations are conducted in both uncoupled and coupled modes to isolate various physical processes influencing TC intensity. The very high-resolutionMM5 simulation of Hurricane Lili (at 0.5 km grid resolution) showed a rapid intensification associated with a contracting eyewall. Changes in both the magnitude and the direction of the vertical wind shear associated with an approaching upper-tropospheric trough were responsible for the weakening of the storm before landfall. Hurricane Lili weakened in a 5-10 m/s vertical wind shear environment. The simulated storm experienced wind shear direction normal to the storm motion, which produced a strong wavenumber one rainfall asymmetry in the downshear-left quadrant of the storm. The rainfall asymmetry was confirmed by various observations from the TRMM satellite and the WSR-88D ground radar in the coastal region. The increasing vertical wind shear induced a vertical tilt of the vortex with a time lag of about 5-6 hours after the wavenumber one rainfall asymmetry was first observed in the model simulation. Other key factors controlling intensity and intensity change in tropical cyclones are the air-sea fluxes. Accurate measurement and parameterization of air-sea fluxes under hurricane conditions are challenging. Although recent studies have shown that the momentum exchange coefficient levels off at high wind speed, little is known about the high wind behavior of the exchange coefficient for enthalpy flux. One of the largest uncertainties is the potential impact of sea spray. The current sea spray parameterizations are closely tied to wind speed and tend to overestimate the mediated heat fluxes by sea spray in the hurricane boundary layer. The sea spray generation depends not only on the wind speed but also on the variable wave state. A new spray parameterization based on the surface wave energy dissipation is introduced in the coupled model. In the coupled simulations, the wave energy dissipation is used to quantify the amount of wave breaking related to the generation of sea spray. The spray parameterization coupled to the waves may be an improvement compared to sea spray parameterizations that depends on wind speed only.
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Hamlin, Samantha L. Miner Benjamin G. "Predation and thermal stress affect color change in the symbiotic sea anemone Aiptasia /." Online version, 2009. http://content.wwu.edu/cdm4/item_viewer.php?CISOROOT=/theses&CISOPTR=359&CISOBOX=1&REC=17.

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Fenoglio-Marc, Luciana. "Satellite geodesy for sea level and climate change." TU Darmstadt, 2015. https://tuprints.ulb.tu-darmstadt.de/4412/1/Fenoglio_Habil2015_v3.pdf.

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This habilitation thesis presents the findings of the sea level change studies conducted at the Institute of Geodesy of the Technischen Universität Darmstadt betweeen 2001 and 2013. Sea level is an important indicator of climate change. It has been traditionally measured by coastal tide gauges and by satellite altimetry since 1993. Tide gauge measurements indicate a coastal average sea level rise of 1-2 millimeters per year over the 20th century. Over the last two decades the average sea level rise increased to 3.3±0.7 millimeters per year, consistently measured by tide gauges and satellite altimetry. The 2013 Intergovernmental Panel on ClimateChange (IPCC AR5) predicts a global mean rise of 50 ± 20 cm by 2100 for a medium warming scenario for the interval 2081-2100. Sea level rise is not uniform and some regions will be more affected than others. It can possibly exacerbate the effects of other factors, such as flooding and ground subsidence. Because of its potential impact on coastal regions, rising sea level is one of the major threatsof climate warming. Changes in each component of the climate system, ocean, land and ice sheets, affects sea level. The two primary contributors of sea level rise, thermal expansion due to ocean warming and melting of continental glaciers and ice sheets, have been identifiedbut large uncertainties remain. Locally non-climatic components, as subsidence, can causerelative sea level rise much larger than the global average mean sea level rise. The global and highly accurate analysis of sea level variations is made possible by spacebasedtechniques. Their main innovation is the use of the same accurate and global reference frame ensuring long-term, precise monitoring and integration in a Global Geodetic ObservingSystem, which is crucial for many practical applications. This thesis focuses on the use of geodetic techniques. Its aim is a comprehensive analysis of the regional sea level variability and of its causes with particular attention to the coastalzone. The three main scientific objectives are: improvement of multi-mission satellite altimetry records, quantification of global and regional sea level change and attribution of sea level rise. Firstly the altimeter data from different missions are unified, improved in the coastal zoneand validated with in-situ and model data. Secondly global and regional estimations of sea level variability from altimetry and tide gauge data are made. The third part of the work is dedicated to the analysis of the reason for sea level change. Here satellite altimetry andgravity missions data are combined with model data to detect the causes of this variation. The analysis includes the separation of mass and volume sea level change and the closing of the water budget. This work shows the challenges of merging satellite data of different types for the understanding of physical processes in sea basins. It also deals with the challenges of new satellite altimetry missions in the coastal zone, where altimetry provides a consistent link to tide gauge stations co-located with Global Navigation Satellite System observations. It finally discusses the importance of highly accurate sea level variability and trends for modeling coastal processes and for long-term predictions.
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Miller, Jason R. "An analysis of the Sea Enterptise program." Thesis, Monterey, Calif. : Springfield, Va. : Naval Postgraduate School ; Available from National Technical Information Service, 2005. http://library.nps.navy.mil/uhtbin/hyperion/05JunMiller.pdf.

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Laxon, Seymour William Clarke. "Satellite radar altimetry of sea ice." Thesis, University College London (University of London), 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.325510.

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The thesis concerns the analysis and interpretation of data from satellite borne radar altimeters over ice covered ocean surfaces. The applications of radar altimetry are described in detail and consider monitoring global climate change, the role that sea ice plays in the climate system, operational applications and the extension of high precision surface elevation measurements into areas of sea ice. The general nature of sea ice cover is discussed and a list of requirements for sea ice monitoring is provided and the capability of different satellite sensors to satisfy needs is examined. The operation of satellite borne altimeter over non-ocean surfaces is discussed in detail. Theories of radar backscatter over sea ice are described and are used to predict the radar altimeter response to different types of sea ice cover. Methods employed for analysis of altimeter data over sea ice are also described. Data from the Seasat altimeter is examined on a regional and global scale and compared with sea ice climatology. Data from the Geosat altimeter is compared with co-incident imagery from the Advanced Very High Resolution Radiometer and also from airborne Synthetic Aperture Radar. Correlations are observed between the altimeter data and imagery for the ice edge position, zones within the ice cover, new ice and leads, vast floes and the fast ice boundary. An analysis of data collected by the Geosat altimeter over a period of more than two years is used to derive seasonal and inter-annual variations in the total Antarctic sea ice extent. In addition the retrieval of high accuracy elevation measurements over sea ice areas is carried out. These data are used to produce improved maps of sea surface topography over icecovered ocean and provide evidence of the ability of the altimeter to determine sea ice freeboard directly. In addition the changing freeboard of two giant Antarctic tabular icebergs, as measured by the Geosat altimeter, is presented. As a summary the achievements are reviewed and suggestions are made towards directions for further work on present data sets and for future data from the ERS-1 satellite.
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Books on the topic "Sea Change"

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Sea change. New York, N.Y: Island Books, 2000.

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Sea change. New York: Delacorte Press, 1999.

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Copyright Paperback Collection (Library of Congress), ed. Sea change. New York: Bantam Books, 2007.

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Sea change. New York: Point, 2009.

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White, Karen. Sea change. Thorndike, Maine: Center Point Publishing, 2012.

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Sea Change. London: Hale, 1985.

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B, Parker Robert. Sea Change. New York: Penguin Group USA, Inc., 2008.

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Sea change. Akron, OH: Ellora's Cave, 2015.

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Sea change. London: Bodley Head, 1996.

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White, Karen. Sea change. New York: New American Library, 2012.

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Book chapters on the topic "Sea Change"

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Higgins, Jennifer. "Sea change." In Franco-British Cultural Exchanges, 1880–1940, 17–33. London: Palgrave Macmillan UK, 2012. http://dx.doi.org/10.1057/9781137030788_2.

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Bruns, Sebastian. "Sea Change." In US Naval Strategy and National Security, 221–48. Abingdon, Oxon ; New York, NY : Routledge, [2018] | Series: Cass series: naval policy and history 1366-9478: Routledge, 2017. http://dx.doi.org/10.4324/9781315624679-7.

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Goosse, Hugues. "Sea Ice." In Global Environmental Change, 97–102. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-5784-4_34.

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Hawkes, Peter J. "Sea Level Change." In Encyclopedia of Natural Hazards, 895–900. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-1-4020-4399-4_309.

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Healy, Terry R., Katherine Stone, Orville Magoon, Billy Edge, Lesley Ewing, Andrew D. Short, Dougals L. Inman, et al. "Sea-Level Change." In Encyclopedia of Coastal Science, 830. Dordrecht: Springer Netherlands, 2005. http://dx.doi.org/10.1007/1-4020-3880-1_269.

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Smith, Thomas M. "Sea-Surface Temperature." In Global Environmental Change, 71–76. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-5784-4_38.

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Milne, Glenn A. "Sea Level." In Coastal Environments and Global Change, 28–51. Chichester, UK: John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781119117261.ch2.

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Gerdes, Rüdiger, and Peter Lemke. "Sea-Ice–Ocean Modelling." In Arctic Climate Change, 381–403. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-2027-5_10.

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Banerjee, Subhankar. "Sea ice." In Systemic Crises of Global Climate Change, 299. Abingdon, Oxon ; New York, NY : Routledge, 2016.Identifiers: LCCN 2015040964 | ISBN 9781138830066 (hb) | ISBN 9781315737454 (ebook): Routledge, 2016. http://dx.doi.org/10.4324/9781315737454-52.

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Huthnance, John, Ralf Weisse, Thomas Wahl, Helmuth Thomas, Julie Pietrzak, Alejandro Jose Souza, Sytze van Heteren, et al. "Recent Change—North Sea." In North Sea Region Climate Change Assessment, 85–136. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-39745-0_3.

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Conference papers on the topic "Sea Change"

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Maul, George A. "Temperature and sea level change." In Global warming: physics and facts. AIP, 1992. http://dx.doi.org/10.1063/1.41923.

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Schroeder, A. J. "Outsourcing: Navigating A Sea Of Change." In Offshore Technology Conference. Offshore Technology Conference, 2005. http://dx.doi.org/10.4043/17739-ms.

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Aral, Mustafa M., Jiabao Guan, and Biao Chang. "Climate Change and Sea Level Rise." In World Environmental and Water Resources Congress 2011. Reston, VA: American Society of Civil Engineers, 2011. http://dx.doi.org/10.1061/41173(414)144.

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Soule, Danald. "Stability in a sea of change." In Conference proceedings. New York, New York, USA: ACM Press, 1990. http://dx.doi.org/10.1145/97808.97871.

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Nunn, P. D. "Sea-Level Change in the Pacific." In Ocean and Atmosphere Pacific: OAP 95. WORLD SCIENTIFIC, 2001. http://dx.doi.org/10.1142/9789812811936_0001.

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SALLENGER, ASBURY H. "HURRICANES, SEA LEVEL RISE, AND COASTAL CHANGE." In The Proceedings of the Coastal Sediments 2011. World Scientific Publishing Company, 2011. http://dx.doi.org/10.1142/9789814355537_0002.

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Felikson, Denis, Ian Fenty, Ben Hamlington, Alexey Shiklomanov, Carmen Blackwood, Mark Carroll, Michael Croteau, et al. "NASA’s Earth Information System: Sea-Level Change." In OCEANS 2022, Hampton Roads. IEEE, 2022. http://dx.doi.org/10.1109/oceans47191.2022.9977250.

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Горячкин, Ю., and Yu Goryachkin. "VARIABILITY OF SEA LEVEL AND DYNAMICS THE ACCUMULATIVE COASTS OF WESTERN CRIMEA." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce394b37220.57460895.

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Influence of the sea level changes on the dynamics of accumulative coasts (in the region of the western Crimea) is considered. The data of observations shows that the greatest change of the beaches under the influence of the level changes by 1 cm can be 1, 3 m. However, the period for which it is determined (1989–2001) was characterized, firstly, by amplification of storm activity, and secondly, by substantial growth of deficiency in deposits. It has been caused by the new deep-water mooring in Eupatoria trading port, which has changed the local migration of deposits. The regular deepening of the waterway has resulted in change of their balance, adaptation of the coast to the changed conditions and, consequently, to acceleration of the coastal line abrasion. The weakest change of beaches under the influence of changes of the level by 1 cm, which is determined for the period 2006–2010, is 0,2–0,3 m. This period was characterized by relatively little changeability of storm activity and relative stabilization of anthropogenic influence, thus such figure seems to be more trustworthy.
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Feldmann, Felix, Emad W. Al-Shalabi, and Waleed AlAmeri. "Carbonate Mineral Effect on Surface Charge Change During Low-Salinity Imbibition." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/206013-ms.

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Abstract Low-salinity waterflooding is a relatively simple and cheap improved oil recovery technique in which the reservoir salinity is optimized to increase oil recovery. Multivalent ion enriched as well as diluted brines have shown promising potential to increase oil production over conventional waterflooding. While the literature generally acknowledges that low-salinity improves oil recovery, the physical mechanisms behind low-salinity effects are still controversial. Surface charge change refers to a low-salinity mechanism in which modified brine is believed to cause a re-equilibrium of the carbonate surface potential. As a result of surface charge change, the rock wettability alters towards a more water-wetting state. This experimental study combines zeta potential, spontaneous imbibition, and contact angle measurements to highlight the effect of carbonate minerals on surface charge change. Initially, zeta potential measurements were conducted to compare the impact of five carbonate minerals (Indiana Limestone, Edward Limestone, Reservoir Limestone, Austin Chalk, and Silurian Dolomite) and brine compositions (Formation-water, Sea-water, and Diluted-sea-water) on carbonate surface charge. Moreover, the impact of potential determining ions (calcium, magnesium, and sulfate) on the mineral surface charge was investigated. The effect of carbonate minerals on spontaneous oil recovery was investigated by comparing the spontaneous imbibition of Formation-water, Sea-water, and Diluted-sea-water into the five carbonate minerals. Moreover, the wettability alteration during the spontaneous imbibition tests was quantified by conducting contact angle measurements. The brine-mineral zeta potential measurements were positive for Formation-water, slightly negative for Sea-water, and strongly negative for Diluted-sea-water. While calcium and magnesium ions promoted stronger positive electrical potentials, sulfate ions caused a zeta potential reduction. The magnitude of surface charge change was significantly different for the five tested carbonate minerals. Under the presence of Diluted-sea-water, the zeta potential measurements of Indiana Limestone and Austin Chalk resulted in strong negative electrical potentials. Reservoir Limestone and Edward Limestone showed less negative zeta potentials, while Silurian Dolomite and Diluted-sea-water resulted in slightly negative zeta potential results. Compared to Formation-water, Sea-water, and particularly Diluted-sea-water caused significant spontaneous oil recovery. The high spontaneous oil recovery of Diluted-sea-water and Indiana Limestone and Austin Chalk correlated with strong negative brine-mineral zeta potentials. Moderate spontaneous oil recovery was observed for the slightly negative zeta potential Sea-water and limestone/chalks systems. The contact angle measurements showed oil-wet contact angles under the presence of Formation-water, while the introduction of Sea-water and Diluted-sea-water promoted stronger water-wet contact angles. This work is one of the very few studies that investigates the effect of carbonate rock mineralogy on surface charge change and spontaneous oil recovery.
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Solow, Andrew R. "The response of sea level to global warming." In The world at risk: Natural hazards and climate change. AIP, 1992. http://dx.doi.org/10.1063/1.43887.

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Reports on the topic "Sea Change"

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Le, Tom. A Japanese Security Sea Change? Let’s See Change First. Critical Asian Studies, January 2023. http://dx.doi.org/10.52698/wajo6699.

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Clague, J. J. Sea level change: factors affecting sea level. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/213910.

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Clague, J. J. Sea level change: introduction. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/213911.

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Clague, J. J., P. T. Bobrowsky, J. P. Builbault, and R. W. Mathewes. Sea level change: late Holocene sea level change, south-central British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/213913.

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Clague, J. J. Sea level change: late Quaternary sea level change in British Columbia: summary of past work. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/213912.

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Gorman, Laurel T. Annotated Bibliography of Relative Sea Level Change. Fort Belvoir, VA: Defense Technical Information Center, September 1991. http://dx.doi.org/10.21236/ada241604.

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Clague, J. J., S. Lichti-federovich, J. P. Guilbault, and R. W. Mathewes. Holocene Sea Level Change, South - Coastal British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132490.

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8

James, T., K. Simon, and A. Darlington. Antarctic ice sheet balance and sea-level change. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2012. http://dx.doi.org/10.4095/290201.

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Solomon, S. M., D. L. Forbes, and B. Kierstead. Coastal impacts of climate change: Beaufort Sea erosion study. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194148.

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Treadway, William D. Implications of the Change Mandated by '...From the Sea.'. Fort Belvoir, VA: Defense Technical Information Center, April 1996. http://dx.doi.org/10.21236/ada326892.

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