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Books on the topic 'Relative sea-level'

Author: Grafiati

Published: 4 June 2021

Last updated: 9 March 2023

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1

Gorman, Laurel T. Annotated bibliography of relative sea level change. U.S. Army Engineer Waterways Experiment Station, 1991.

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2

W, Stewart R., COMAR (Project), and COMAR Working Group on Mean Sea-Level Rise and Its Influence on the Coastal Zone, eds. Relative sea-level change: A critical evaluation. Unesco, 1990.

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3

Giese, G. S. Passive retreat of Massachusetts coastal upland due to relative sea-level rise. Massachusetts Coastal Zone Management, Massachusetts Coastal Submergence Program, 1987.

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4

K, Weddle Thomas, Retelle Michael J. 1953-, Geological Society of America, and Geological Society of America. Northeastern Section. Meeting, eds. Deglacial history and relative sea-level changes, northern New England and adjacent Canada. Geological Society of America, 2000.

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5

Shea, Penland, and Louisiana Geological Survey, eds. Relative sea level rise and subsidence in Louisiana and the Gulf of Mexico. Louisiana Geological Survey, 1989.

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6

Beale, Harriet. Relative rise in sea-level during the past 5000 years at six salt marshes in Northern Puget Sound, Washington. Washington Dept. of Ecology, 1990.

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7

Beale, Harriet. Relative rise in sea-level during the past 5000 years at six salt marshes in Northern Puget Sound, Washington. Washington Dept. of Ecology, 1990.

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8

Administration, United States Federal Insurance. Projected impact of relative sea level rise on the National Flood Insurance Program. U.S. Federal Emergency Management Agency, Federal Insurance Administration, 1991.

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9

Miettinen, Arto. Relative sea level changes in the eastern part of the Gulf of Finland during the last 8000 years. Suomalainen Tiedeakatemia, 2002.

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10

Eggleston, Jack. Land subsidence and relative sea-level rise in the southern Chesapeake Bay region. United States Geological Survey, 2014.

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11

Ena, Martin, Raukas Anto, and International Symposium Evolution and Dynamics of Seacoasts in Conditions of Relative Sea Level Oscillation (1986 : Tallinn, Estonia), eds. International Symposium Evolution and Dynamics of Seacoasts in Conditions of Relative Sea Level Oscillation, Aug. 20-26, 1986: Excursion guide and abstracts. Academy of Sciences of the Estonian SSR, Institute of Geology, 1986.

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12

Campeau, S. Diatoms from the Beaufort Sea coast, southern Arctic Ocean (Canada): Modern analogues for reconstructing Late Quaternary environments and relative sea levels. J. Cramer, 1999.

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13

Bruce, Jaffe, and Geological Survey (U.S.), eds. Louisiana barrier island erosion study: Correction for effect of relative sea level change on historical bathymetric survey comparisons, Isles Dernieres area, Louisiana. U.S. Dept. of the Interior, U.S. Geological Survey, 1991.

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14

McClenahan, Philippe. Geographical variations in the holocene chronology of western Europe coastal dunes in relation to climate, sea-level and human impact. The Author], 1997.

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15

Relative sea-level change: A critical evaluation. Unesco, 1990.

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16

Aucelli, Pietro, Giuseppe Mastronuzzi, and Gaia Mattei, eds. Relative Sea-Level Changes and their Impact on Coastal Zones. MDPI, 2022. http://dx.doi.org/10.3390/books978-3-0365-4633-9.

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17

Deglacial History and Relative Sea-Level Changes, Northern New England and Adjacent Canada (Special Paper (Geological Society of America)). Geological Society of America, 2001.

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18

Ancient Sea-Margins: As Memorials of Changes in the Relative Level of Sea and Land. Creative Media Partners, LLC, 2022.

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19

Ancient Sea-Margins: As Memorials of Changes in the Relative Level of Sea and Land. Creative Media Partners, LLC, 2022.

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20

Robert, Chambers. Ancient Sea-Margins, As Memorials Of Changes In The Relative Level Of Sea And Land. Kessinger Publishing, LLC, 2007.

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21

Robert, Chambers. Ancient Sea-Margins, As Memorials Of Changes In The Relative Level Of Sea And Land. Kessinger Publishing, LLC, 2007.

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22

Weddle, Thomas K., and Michael J. Retelle. Deglacial history and relative sea-level changes, northern New England and adjacent Canada. Geological Society of America, 2001. http://dx.doi.org/10.1130/spe351.

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23

Special Paper 351: Deglacial history and relative sea-level changes, northern New England and adjacent Canada. Geological Society of America, 2001. http://dx.doi.org/10.1130/0-8137-2351-5.

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24

Beale, Harriet. Relative rise in sea-level during the late Holocene at six salt marshes in the Puget Basin, Washington. 1990.

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25

Weber, Stacy J. Late Pleistocene littoral deposits in the Deming sand at Bellingham Bay, Washington, and their implications for relative sea level changes. 2001.

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26

Dickinson, William R. Coastal Landforms on Islands of Pacific Oceania. Edited by Ethan E. Cochrane and Terry L. Hunt. Oxford University Press, 2014. http://dx.doi.org/10.1093/oxfordhb/9780199925070.013.023.

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The evolution of coastal landforms on tropical Pacific islands has been influenced jointly by changes in relative sea level and by shoreline sediment dynamics. During human occupation of Pacific Oceania, changes in sea level have reflected a monotonic hydro-isostatic drawdown in regional sea level following a mid-Holocene highstand in eustatic sea level, and varied patterns of tectonic uplift or subsidence affecting individual islands or island groups. Wave erosion has altered some bold coastlines, but the dominant trend of paleoshoreline evolution along lowland coasts has been the expansion o

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27

Räisänen, Jouni. Future Climate Change in the Baltic Sea Region and Environmental Impacts. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190228620.013.634.

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The warming of the global climate is expected to continue in the 21st century, although the magnitude of change depends on future anthropogenic greenhouse gas emissions and the sensitivity of climate to them. The regional characteristics and impacts of future climate change in the Baltic Sea countries have been explored since at least the 1990s. Later research has supported many findings from the early studies, but advances in understanding and improved modeling tools have made the picture gradually more comprehensive and more detailed. Nevertheless, many uncertainties still remain.In the Balt

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28

Oleson, John Peter, and Robert L. Hohlfelder. Ancient Harbors in the Mediterranean. Edited by Ben Ford, Donny L. Hamilton, and Alexis Catsambis. Oxford University Press, 2012. http://dx.doi.org/10.1093/oxfordhb/9780199336005.013.0035.

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This article describes the evolution of harbors in the ancient world that can be linked to changing social needs and technological developments. Hundreds of harbor sites of varying sizes and designs can be documented around the Mediterranean dating back thousands of years. Relief sculpture and a few shipwrecks provide ample evidence for the intensity of trade by sea in the eastern Mediterranean during the Bronze Age, but the rise in the relative sea level in the eastern Mediterranean since the Bronze Age has obscured or destroyed many of the early harbor sites. Natural anchorages were used thr

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29

Freund, Holger, and Deutsche Quartärvereinigung e. V, eds. E&G – Quaternary Science Journal Vol. 59 No 1-2. Geozon Science Media, 2011.

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30

Kirkwood, Roger, and Simon Goldsworthy. Fur Seals and Sea Lions. CSIRO Publishing, 2013. http://dx.doi.org/10.1071/9780643109834.

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Fur seals and sea lions are charismatic, large carnivores that engage us with both their skill and playful antics. Although all species in Australian waters were harvested to near extinction 200 years ago, fur seals are recovering and are now common in near-shore waters across southern Australia. Sea lions, however, are endangered. Their populations appear not to have recovered like fur seals and are declining at some locations. Fur seals and sea lions are important top level predators and play an important role in Australia’s temperate marine ecosystems. Key threats they currently face relate

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31

Gabriele, Goettsche-Wanli. Part I Assessing the UN Institutional Structure for Global Ocean Governance: The UN’s Role in Global Ocean Governance, 1 The Role of the United Nations, including its Secretariat in Global Ocean Governance. Oxford University Press, 2018. http://dx.doi.org/10.1093/law/9780198824152.003.0001.

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This chapter examines the role of the United Nations and its related institutions for global ocean governance, including those established by the entry into force of the United Nations Convention on the Law of the Sea (UNCLOS). It first considers the main issues that these institutions have addressed, ranging from sustainable fisheries, via ecosystem protection, to marine biodiversity conservation; and more recently, maritime security. It then argues that the impacts of climate change have arguably not been directly addressed by either the global ocean governance regime, as it is currently con

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32

James, Harrison. 6 Marine Environmental Threats from Shipping. Oxford University Press, 2017. http://dx.doi.org/10.1093/law/9780198707325.003.0006.

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The prevention of pollution from ships as a topic is largely addressed at the global level through the International Maritime Organization (IMO). Chapter 6 analyses the main treaties in this field, including the International Convention on the Prevention of Pollution from Ships (MARPOL Convention), the International Convention on the Safety of Life at Sea (SOLAS Convention), the International Convention on Ballast Water Management, and the International Convention on Anti-Fouling Substances. The analysis addresses both the types of rules employed in the IMO treaties and the processes through w

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33

Canfield, Donald Eugene. Phanerozoic Oxygen. Princeton University Press, 2017. http://dx.doi.org/10.23943/princeton/9780691145020.003.0011.

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This chapter discusses the modeling of the history of atmospheric oxygen. The most recently deposited sediments will also be the most prone to weathering through processes like sea-level change or uplift of the land. Thus, through rapid recycling, high rates of oxygen production through the burial of organic-rich sediments will quickly lead to high rates of oxygen consumption through the exposure of these organic-rich sediments to weathering. From a modeling perspective, rapid recycling helps to dampen oxygen changes. This is important because the fluxes of oxygen through the atmosphere during

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34

Bilański, Piotr. Trypodendron laeve Eggers w Polsce na tle wybranych aspektów morfologicznych i genetycznych drwalników (Trypodendron spp., Coleoptera, Curculionidae, Scolytinae). Publishing House of the University of Agriculture in Krakow, 2019. http://dx.doi.org/10.15576/978-83-66602-38-0.

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In Poland, there are 4 species of the liypodendron genus: T lineaium Oliv., T domestkum L., T signature Fakir. and 7: laeve Egg. Trypodendron laeve is the leastknown of this group. Many factors had influence on the state of research on this species, including taxonomic aspects. Taking into account the unsatisfactory state of knowledge regarding the prevalence of T iaeve in Poland, as well as scarce information on the morphology of this species, research was undertaken to I) document the presence, including new sites, of T laeve in Poland and define, if possible, the habitat and trophic conditi

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35

Zalasiewicz, Jan, and Mark Williams. The Goldilocks Planet. Oxford University Press, 2012. http://dx.doi.org/10.1093/oso/9780199593576.001.0001.

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Climate change is a major topic of concern today and will be so for the foreseeable future, as predicted changes in global temperatures, rainfall, and sea level continue to take place. But as Jan Zalasiewicz and Mark Williams reveal in The Goldilocks Planet, the climatic changes we are experiencing today hardly compare to the changes the Earth has seen over the last 4.5 billion years. Indeed, the vast history that the authors relate here is dramatic and often abrupt--with massive changes in global and regional climate, from bitterly cold to sweltering hot, from arid to humid. They introduce us

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