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Journal articles on the topic 'Climate change; sea level'

Author: Grafiati

Published: 3 June 2025

Last updated: 31 July 2025

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1

Lanovoy, Vladyslav, and Sally O’Donnell. "Climate Change and Sea-Level Rise." International Community Law Review 23, no. 2-3 (2021): 133–57. http://dx.doi.org/10.1163/18719732-12341466.

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Abstract This article examines the challenges that climate change and sea-level rise pose to certain key aspects of the law of the sea. Sea-level rise is likely to impact maritime baselines, the qualification of maritime features and the entitlements they generate, and ultimately the stability of maritime boundaries, which are critical for the peaceful co-existence of sovereign States. This article examines whether some of the relevant provisions of the United Nations Convention on the Law of the Sea can accommodate a liberal interpretation so as to provide some, even if incomplete, answers to

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2

Long, A. "Late Holocene sea-level change and climate." Progress in Physical Geography 24, no. 3 (2000): 415–24. http://dx.doi.org/10.1191/030913300701542714.

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3

Drewry, David. "Ice sheets, climate change and sea level." Physics World 9, no. 1 (1996): 29–33. http://dx.doi.org/10.1088/2058-7058/9/1/25.

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4

Warrick, R. A., and E. M. Barrow. "Climate and Sea Level Change: A Perspective." Outlook on Agriculture 19, no. 1 (1990): 5–8. http://dx.doi.org/10.1177/003072709001900103.

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5

Long, Antony. "Late Holocene sea-level change and climate." Progress in Physical Geography: Earth and Environment 24, no. 3 (2000): 415–23. http://dx.doi.org/10.1177/030913330002400307.

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6

Schofield, Clive. "Climate Change and Changing Coasts." Korean Journal of International and Comparative Law 5, no. 1 (2017): 36–60. http://dx.doi.org/10.1163/22134484-12340078.

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Sea level rise has provoked widespread concerns that low-lying parts of coastal States including parts or even the entirety of small island developing States face a looming threat of erosion and inundation. Concerns over the potential impacts of sea level rise on the location of baselines along the coast and therefore on the scope of national claims to maritime jurisdiction have also been raised. The article outlines climate change impacts on the oceans before briefly reviewing projections of sea level rise. A number of the complexities and uncertainties which make prediction of the scale and

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7

Muhammad, Zikra*. "IMPACTS OF GLOBAL CLIMATE CHANGE ON INDONESIA OCEAN ENVIRONMENT." INTERNATIONAL JOURNAL OF ENGINEERING SCIENCES & RESEARCH TECHNOLOGY 4, no. 5 (2017): 79–85. https://doi.org/10.5281/zenodo.801287.

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The problems in coastal and ocean area related with climate change have continued to receive a high level of attention. Elevate average of sea level, variation in significant wave height and increased ocean temperature are linked to global climate in many ways. Thus, climate variability and future climate change should become a major interest for engineer, stakeholders, and decision makers, especially for developing strategies for mitigation and adaptation for future coastal development. The objective of this paper is to analyze the impacts of global climate change to Indonesian ocean environm

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8

Hansen, James, Makiko Sato, Gary Russell, and Pushker Kharecha. "Climate sensitivity, sea level and atmospheric carbon dioxide." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 371, no. 2001 (2013): 20120294. http://dx.doi.org/10.1098/rsta.2012.0294.

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Cenozoic temperature, sea level and CO 2 covariations provide insights into climate sensitivity to external forcings and sea-level sensitivity to climate change. Climate sensitivity depends on the initial climate state, but potentially can be accurately inferred from precise palaeoclimate data. Pleistocene climate oscillations yield a fast-feedback climate sensitivity of 3±1 ° C for a 4 W m −2 CO 2 forcing if Holocene warming relative to the Last Glacial Maximum (LGM) is used as calibration, but the error (uncertainty) is substantial and partly subjective because of poorly defined LGM global t

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Priestley, Rebecca K., Zoë Heine, and Taciano L. Milfont. "Public understanding of climate change-related sea-level rise." PLOS ONE 16, no. 7 (2021): e0254348. http://dx.doi.org/10.1371/journal.pone.0254348.

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Sea-level rise resulting from climate change is impacting coasts around the planet. There is strong scientific consensus about the amount of sea-level rise to 2050 (0.24–0.32 m) and a range of projections to 2100, which vary depending on the approach used and the mitigation measures taken to reduce carbon emissions. Despite this strong scientific consensus regarding the reality of climate change-related sea-level rise, and the associated need to engage publics in adaptation and mitigation efforts, there is a lack of empirical evidence regarding people’s understanding of the issue. Here we inve

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Koppe, Baerbel, and Lena Lankenau. "GERMAN SEAPORTS AND CLIMATE CHANGE – RECOMMENDATIONS FOR CLIMATE CHANGE ADAPTATION MEASURES." Coastal Engineering Proceedings, no. 38 (May 29, 2025): 83. https://doi.org/10.9753/icce.v38.management.83.

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The German seaports, with their location at the interface between sea and land, will be particularly affected by the effects of climate change. In addition to sea level rise and its impact on tidal and morpho-dynamics, these include the increase in extreme temperature and precipitation events as well as possible changes in storm intensity or storm activity and water chemistry.

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Hoseini, S. Mahya, Mohsen Soltanpour, Mohammad R. Zolfaghari, and Ioan Nistor. "PROJECTING FUTURE CASPIAN SEA LEVEL CHANGES IN RESPONSE TO CLIMATE CHANGE." Coastal Engineering Proceedings, no. 38 (May 29, 2025): 124. https://doi.org/10.9753/icce.v38.management.124.

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The Caspian Sea (CS), the world's largest lake, is a hydrologically sensitive water body, with a water level that has been experiencing significant fluctuations. Between 1930 and 1977, the Caspian Sea level (CSL) decreased dramatically by more than 3 m, reaching 29 m below sea level (Baltic datum). Subsequently, from 1977 to 1995, an unexpected CSL rise of approximately 2.5 m (reaching -26.5 m) led to extensive flooding and various challenges in neighboring countries. Following this sharp increase, the CSL gradually decreased, with the current value of about -27.8 m in 2023. The decline in CSL

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12

D’Arcy, Eleanor, Jonathan A. Tawn, and Dafni E. Sifnioti. "Accounting for Climate Change in Extreme Sea Level Estimation." Water 14, no. 19 (2022): 2956. http://dx.doi.org/10.3390/w14192956.

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Extreme sea level estimates are fundamental for mitigating coastal flooding as they provide insight for defence engineering. As the global climate changes, rising sea levels combined with increases in storm intensity and frequency pose an increasing risk to coastline communities. We present a new method for estimating extreme sea levels that accounts for the effects of climate change on extreme events that are not accounted for by mean sea level trends. We follow a joint probabilities methodology, considering skew surge and peak tides as the only components of sea levels. We model extreme skew

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13

Fang, Hui-Ming, Po-Han Chang, and Hsing-Yu Wang. "Analysis of Sea Level Changes in Eastern Taiwan Coast—Case of Yilan Area." International Journal of Environmental Science and Development 14, no. 4 (2023): 259–64. http://dx.doi.org/10.18178/ijesd.2023.14.4.1442.

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This study considers the impact of extreme climates on most of the world’s land and seas, which may cause the average sea level to rise due to global climate change. Affected by the rise of sea level, it will change the distribution characteristics of sea tides, waves and currents. When the distribution of tides, waves and currents in the sea area changes, it may cause changes in the overall environmental characteristics of the estuary and coastal areas, and further affects the function of coastal protection facilities. This study takes the sea area of Yilan as an example, and analyzes the pro

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14

Weller, Gunter. "Detecting Global Change In The Arctic." Annals of Glaciology 14 (1990): 362. http://dx.doi.org/10.3189/s026030550000940x.

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Numerical models have predicted global temperature increases due to rising atmospheric CO2 levels, which should be detectable by now, but have not yet been identified in an unambiguous manner. This detection is complicated by inadequate data and by the fact that climate can be changed by factors other than CO2 increases. A systematic monitoring strategy is therefore needed to assess global change. In the Arctic, cryospheric parameters, including sea ice, snow cover, glaciers and permafrost are sensitive indicators of climate change and their monitoring by satellites and surface observations is

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15

Weller, Gunter. "Detecting Global Change In The Arctic." Annals of Glaciology 14 (1990): 362. http://dx.doi.org/10.1017/s026030550000940x.

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Numerical models have predicted global temperature increases due to rising atmospheric CO2 levels, which should be detectable by now, but have not yet been identified in an unambiguous manner. This detection is complicated by inadequate data and by the fact that climate can be changed by factors other than CO2 increases. A systematic monitoring strategy is therefore needed to assess global change. In the Arctic, cryospheric parameters, including sea ice, snow cover, glaciers and permafrost are sensitive indicators of climate change and their monitoring by satellites and surface observations is

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Vermeersen, Bert L. A., Aimée B. A. Slangen, Theo Gerkema, et al. "Sea-level change in the Dutch Wadden Sea." Netherlands Journal of Geosciences 97, no. 3 (2018): 79–127. http://dx.doi.org/10.1017/njg.2018.7.

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AbstractRising sea levels due to climate change can have severe consequences for coastal populations and ecosystems all around the world. Understanding and projecting sea-level rise is especially important for low-lying countries such as the Netherlands. It is of specific interest for vulnerable ecological and morphodynamic regions, such as the Wadden Sea UNESCO World Heritage region.Here we provide an overview of sea-level projections for the 21st century for the Wadden Sea region and a condensed review of the scientific data, understanding and uncertainties underpinning the projections. The

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17

Slangen, Aimée B. A., Benoit Meyssignac, Cecile Agosta, et al. "Evaluating Model Simulations of Twentieth-Century Sea Level Rise. Part I: Global Mean Sea Level Change." Journal of Climate 30, no. 21 (2017): 8539–63. http://dx.doi.org/10.1175/jcli-d-17-0110.1.

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Sea level change is one of the major consequences of climate change and is projected to affect coastal communities around the world. Here, global mean sea level (GMSL) change estimated by 12 climate models from phase 5 of the World Climate Research Programme’s Climate Model Intercomparison Project (CMIP5) is compared to observational estimates for the period 1900–2015. Observed and simulated individual contributions to GMSL change (thermal expansion, glacier mass change, ice sheet mass change, landwater storage change) are analyzed and compared to observed GMSL change over the period 1900–2007

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18

Ramkumar Krishnamoorthy. "Performance Analysis of Machine Learning Techniques for Predicting Sea Level Rise." Journal of Information Systems Engineering and Management 10, no. 36s (2025): 640–46. https://doi.org/10.52783/jisem.v10i36s.6543.

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Climate science is a study of the earth's climate system, it was originated in the year nineteenth century, the purpose of climate science is to understand the weather patterns, ocean currents and the change climatic shifts. The field of climate changes it involves the contributions from a diverse range of professionals, including scientists, historians and sociologists. the efforts of the human to understand the natural forces which control the climate. In the recent research it was highlighted the impact of human activities like emission of gases etc. The ocean’s surface is increased by the

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19

Royston, Sam, Rory J. Bingham, and Jonathan L. Bamber. "Attributing decadal climate variability in coastal sea-level trends." Ocean Science 18, no. 4 (2022): 1093–107. http://dx.doi.org/10.5194/os-18-1093-2022.

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Abstract. Decadal sea-level variability masks longer-term changes due to natural and anthropogenic drivers in short-duration records and increases uncertainty in trend and acceleration estimates. When making regional coastal management and adaptation decisions, it is important to understand the drivers of these changes to account for periods of reduced or enhanced sea-level change. The variance in decadal sea-level trends about the global mean is quantified and mapped around the global coastlines of the Atlantic, Pacific, and Indian oceans from historical CMIP6 runs and a high-resolution ocean

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20

Slangen, Aimée B. A., John A. Church, Xuebin Zhang, and Didier P. Monselesan. "The Sea Level Response to External Forcings in Historical Simulations of CMIP5 Climate Models*." Journal of Climate 28, no. 21 (2015): 8521–39. http://dx.doi.org/10.1175/jcli-d-15-0376.1.

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Abstract Changes in Earth’s climate are influenced by internal climate variability and external forcings, such as changes in solar radiation, volcanic eruptions, anthropogenic greenhouse gases (GHG), and aerosols. Although the response of surface temperature to external forcings has been studied extensively, this has not been done for sea level. Here, a range of climate model experiments for the twentieth century is used to study the response of global and regional sea level change to external climate forcings. Both the global mean thermosteric sea level and the regional dynamic sea level patt

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21

Howard, T., J. Ridley, A. K. Pardaens, et al. "The land-ice contribution to 21st century dynamic sea-level rise." Ocean Science Discussions 11, no. 1 (2014): 123–69. http://dx.doi.org/10.5194/osd-11-123-2014.

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Abstract. Climate change has the potential to locally influence mean sea level through a number of processes including (but not limited to) thermal expansion of the oceans and enhanced land ice melt. These lead to departures from the global mean sea level change, due to spatial variations in the change of water density and transport, which are termed dynamic sea level changes. In this study we present regional patterns of sea-level change projected by a global coupled atmosphere–ocean climate model forced by projected ice-melt fluxes from three sources: the Antarctic ice sheet, the Greenland i

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22

Perrette, M., F. Landerer, R. Riva, K. Frieler, and M. Meinshausen. "Probabilistic projection of sea-level change along the world's coastlines." Earth System Dynamics Discussions 3, no. 1 (2012): 357–89. http://dx.doi.org/10.5194/esdd-3-357-2012.

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Abstract. Climate change causes global mean sea level to rise due to thermal expansion of seawater and loss of land ice from mountain glaciers, ice caps and ice-sheets. Locally, sea-level changes can strongly deviate from the global mean due to ocean dynamics. In addition, gravitational adjustments redistribute seawater away from shrinking ice masses, an effect currently not incorporated in climate models. Here, we provide probabilistic projections of sea level changes along the world's coastlines for the end of the 21st century under the new RCP emission scenarios, taking into account uncerta

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23

Zhu, Hengyi. "Mechanisms and Modeling of Sea Level Rise in the Context of Global Warming." Theoretical and Natural Science 86, no. 1 (2025): 145–49. https://doi.org/10.54254/2753-8818/2025.20241.

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Sea level rise due to global warming is an important topic in current climate change research. In this study, we explore how complex natural processes triggered by global warming drive sea level change by analyzing climate models. We focus on the main drivers of sea level rise, including ice sheet melting and ocean thermal expansion. In addition, the article discusses in detail how positive feedback mechanisms and negative feedback mechanisms work together to influence the climate change process. In order to predict the future trend of sea level rise, this article models and simulates the glob

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24

Goelzer, Heiko, Philippe Huybrechts, Marie-France Loutre, and Thierry Fichefet. "Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model." Climate of the Past 12, no. 12 (2016): 2195–213. http://dx.doi.org/10.5194/cp-12-2195-2016.

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Abstract. As the most recent warm period in Earth's history with a sea-level stand higher than present, the Last Interglacial (LIG, ∼ 130 to 115 kyr BP) is often considered a prime example to study the impact of a warmer climate on the two polar ice sheets remaining today. Here we simulate the Last Interglacial climate, ice sheet, and sea-level evolution with the Earth system model of intermediate complexity LOVECLIM v.1.3, which includes dynamic and fully coupled components representing the atmosphere, the ocean and sea ice, the terrestrial biosphere, and the Greenland and Antarctic ice sheet

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25

Meehl, Gerald A., Warren M. Washington, Benjamin D. Santer, et al. "Climate Change Projections for the Twenty-First Century and Climate Change Commitment in the CCSM3." Journal of Climate 19, no. 11 (2006): 2597–616. http://dx.doi.org/10.1175/jcli3746.1.

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Abstract Climate change scenario simulations with the Community Climate System Model version 3 (CCSM3), a global coupled climate model, show that if concentrations of all greenhouse gases (GHGs) could have been stabilized at the year 2000, the climate system would already be committed to 0.4°C more warming by the end of the twenty-first century. Committed sea level rise by 2100 is about an order of magnitude more, percentage-wise, compared to sea level rise simulated in the twentieth century. This increase in the model is produced only by thermal expansion of seawater, and does not take into a

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Ahmad Affandi, Muhammad Luqman, Ami Hassan Md Din, and Abd Wahid Rasib. "A Short Review on Causes of Sea Level Rise for Climate Monitoring." IOP Conference Series: Earth and Environmental Science 1051, no. 1 (2022): 012003. http://dx.doi.org/10.1088/1755-1315/1051/1/012003.

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Abstract Sea level rise has currently become a major issue for climate change. It has globally drawn attention because as time passes, global sea levels will continue to rise at an accelerating rate in the 21st century. It will cause a serious impact on environmental problems such as coastal inundation, salt intrusion, coastal erosion, and other phenomena. These scenarios lead to earth problems in which land and oceans continue shifting due to climate change, posing a threat to the very existence of all living beings in the coming years. As a result, climate monitoring is critical for tracking

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27

Griggs, Gary, and Borja G. Reguero. "Coastal Adaptation to Climate Change and Sea-Level Rise." Water 13, no. 16 (2021): 2151. http://dx.doi.org/10.3390/w13162151.

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The Earth’s climate is changing; ice sheets and glaciers are melting and coastal hazards and sea level are rising in response. With a total population of over 300 million people situated on coasts, including 20 of the planet’s 33 megacities (over 10 million people), low-lying coastal areas represent one of the most vulnerable areas to the impacts of climate change. Many of the largest cities along the Atlantic coast of the U.S. are already experiencing frequent high tide flooding, and these events will increase in frequency, depth, duration and extent as sea levels continue to rise at an accel

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28

Zulaiha Binti Zolkaply, Siti, Lubna Alam, Ahmad Abas Kutty, Firoz Khan, and Mazlin Mokhtar. "A Review on Climate Change, Sea Level Change and Paleoclimate History." Journal of Engineering and Applied Sciences 14, no. 2 (2019): 423–29. http://dx.doi.org/10.36478/jeasci.2019.423.429.

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29

Cheye, Stephen, Adejumo Azeez Adewale, and Osho Moses Ademola. "Harnessing Artificial Intelligence for Climate Resilience: Analysing the Impact of Climate Change on Sea Level Rise and Precipitation Patterns." International Journal of Research Publication and Reviews 5, no. 9 (2024): 2875–93. http://dx.doi.org/10.55248/gengpi.5.0924.2662.

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30

Lee, Baeg, Min-Kyu Jung, and Hyun-Han Kwon. "Climate Change Impacts of Sea Level Rise on the Saemangeum Sea Dike." Korea Society of Coastal Disaster Prevention 9, no. 1 (2022): 13–21. http://dx.doi.org/10.20481/kscdp.2022.9.1.13.

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The Saemangeum Sea Dike, completed in 2011 in South Korea, is the longest sea dike in the world. One of the most pressing issues of today, climate change leads to sea-level rise that could increase the risk of sea dike overflow. However, what impact climate change will have on the Saemangeum Sea Dike has not been verified yet. Here, we estimate the impacts of sea-level rise on the Saemangeum Sea Dike, using the Linear Regression Analysis method, the Continuous Wavelet Transform (CWT) method, and the Ensemble Empirical Mode Decomposition (EEMD) method. The sea level data of the Saemangeum area

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31

Nie, Lizhen. "Analysis of the influence of the climate change on sea level." Applied and Computational Engineering 3, no. 1 (2023): 109–15. http://dx.doi.org/10.54254/2755-2721/3/20230363.

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Rising sea levels are not a direct result of climate change but rather an indirect influence. When ice melts, it releases water into the ocean, which causes it to rise. As the planet warms and glaciers continue to melt, sea levels rise and land elevations increase. As a result of all of these shifts, sea levels are increasing worldwide. Sea level change refers to the increase or decrease in sea level. Meters above a standard, like the geoid or mean sea level, are used to describe the height of the water (MSL). This research uses a literature review approach to investigate the spatial and tempo

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32

Hollin, John T., R. A. Warrick, E. M. Barrow, and T. M. L. Wigley. "Climate and Sea Level Change: Observations, Projections and Implications." Arctic and Alpine Research 26, no. 1 (1994): 95. http://dx.doi.org/10.2307/1551886.

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33

Rowland, M. J. "Climate Change, Sea-Level Rise And The Archaeological Record." Australian Archaeology 34, no. 1 (1992): 29–33. http://dx.doi.org/10.1080/03122417.1992.11681449.

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34

Anderson, J. B. "CLIMATE CHANGE: Ice Sheet Stability and Sea-Level Rise." Science 315, no. 5820 (2007): 1803–4. http://dx.doi.org/10.1126/science.1140766.

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35

Kassam, Amir. "Climate change, sea-level rise and development in Bangladesh." International Journal of Environmental Studies 72, no. 2 (2015): 346–50. http://dx.doi.org/10.1080/00207233.2015.1019300.

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36

Nijkamp, Peter. "Climate change, sea-level rise and Dutch defense strategies." Project Appraisal 6, no. 3 (1991): 143–48. http://dx.doi.org/10.1080/02688867.1991.9726811.

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37

Sierro, Francisco J., Nils Andersen, Maria A. Bassetti, et al. "Phase relationship between sea level and abrupt climate change." Quaternary Science Reviews 28, no. 25-26 (2009): 2867–81. http://dx.doi.org/10.1016/j.quascirev.2009.07.019.

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38

Barrage, Lint, and Jacob Furst. "Housing investment, sea level rise, and climate change beliefs." Economics Letters 177 (April 2019): 105–8. http://dx.doi.org/10.1016/j.econlet.2019.01.023.

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39

Patwardhan, Anand. "Climate and sea level change: Observations, projections and implications." Global Environmental Change 5, no. 1 (1995): 75–76. http://dx.doi.org/10.1016/0959-3780(95)90007-1.

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40

Ranasinghe, Roshanka, and Ruben Jongejan. "Climate Change, Coasts and Coastal Risk." Journal of Marine Science and Engineering 6, no. 4 (2018): 141. http://dx.doi.org/10.3390/jmse6040141.

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Ramos Ribeiro, Rodrigo Rudge, and Celeste Oliveira Alves Coelho. "The social perception of natural hazards risk: Portugal and Tuvalu." Investigaciones Geográficas, no. 57 (June 15, 2012): 195. http://dx.doi.org/10.14198/ingeo2012.57.09.

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The effects of climate change and sea-level change should cause serious problems for the inhabitants of some small islands such as Tuvalu in the future. As a result of a combination of natural processes and anthropogenic action, the sea-level change creates different impacts. This research investigates the perception of natural risk and climate change in Portugal and Tuvalu. The perception of the some natural risk, like sea-level rise, can be different of each place. The perception of climate changes in Tuvalu is little known for academic community from University of Aveiro, and they believe t

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Nerem, R. S., B. D. Beckley, J. T. Fasullo, B. D. Hamlington, D. Masters, and G. T. Mitchum. "Climate-change–driven accelerated sea-level rise detected in the altimeter era." Proceedings of the National Academy of Sciences 115, no. 9 (2018): 2022–25. http://dx.doi.org/10.1073/pnas.1717312115.

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Using a 25-y time series of precision satellite altimeter data from TOPEX/Poseidon, Jason-1, Jason-2, and Jason-3, we estimate the climate-change–driven acceleration of global mean sea level over the last 25 y to be 0.084 ± 0.025 mm/y2. Coupled with the average climate-change–driven rate of sea level rise over these same 25 y of 2.9 mm/y, simple extrapolation of the quadratic implies global mean sea level could rise 65 ± 12 cm by 2100 compared with 2005, roughly in agreement with the Intergovernmental Panel on Climate Change (IPCC) 5th Assessment Report (AR5) model projections.

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Howard, T., J. Ridley, A. K. Pardaens, et al. "The land-ice contribution to 21st-century dynamic sea level rise." Ocean Science 10, no. 3 (2014): 485–500. http://dx.doi.org/10.5194/os-10-485-2014.

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Abstract. Climate change has the potential to influence global mean sea level through a number of processes including (but not limited to) thermal expansion of the oceans and enhanced land ice melt. In addition to their contribution to global mean sea level change, these two processes (among others) lead to local departures from the global mean sea level change, through a number of mechanisms including the effect on spatial variations in the change of water density and transport, usually termed dynamic sea level changes. In this study, we focus on the component of dynamic sea level change that

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44

Elneel, Leena, M. Sami Zitouni, Husameldin Mukhtar, Paolo Galli, and Hussain Al-Ahmad. "Exploring Key Aspects of Sea Level Rise and Their Implications: An Overview." Water 16, no. 3 (2024): 388. http://dx.doi.org/10.3390/w16030388.

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Sea level rise (SLR) is one of the most pressing challenges of climate change and has drawn noticeable research interest over the past few decades. Factors induced by global climate change, such as temperature increase, have resulted in both direct and indirect changes in sea levels at different spatial scales. Various climatic and non-climatic events contribute to sea level changes, posing risks to coastal and low-lying areas. Nevertheless, changes in sea level are not uniformly distributed globally due to several regional factors such as wave actions, storm surge frequencies, and tectonic la

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45

Norris, K., and P. W. Atkinson. "Declining populations of coastal birds in Great Britain: victims of sea-level rise and climate change?" Environmental Reviews 8, no. 4 (2000): 303–23. http://dx.doi.org/10.1139/a00-011.

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Is sea-level rise and (or) climate change responsible for current declines in important coastal bird populations in Great Britain, and how might these processes affect bird populations in future? We review the current status of coastal bird populations in Britain and identify two important species, Common Redshank (Tringa totanus) and Twite (Carduelis flavirostris), whose populations are currently declining. We then review the evidence relating to the causes of these declines. There is evidence that habitat loss, driven by sea-level rise and climate change (e.g., an increase in wind and wave e

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Wan, Qiang. "Coupling Mechanisms Between Biosphere and Atmosphere Affecting Sea Level Rise." Theoretical and Natural Science 84, no. 1 (2025): 124–29. https://doi.org/10.54254/2753-8818/2025.22317.

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Since the industrial revolution, human activities have significantly contributed to the Earth's pollution, in particular the continued emission of greenhouse gases (e.g., carbon dioxide and methane). These emissions are contributing to climate change, with accelerated melting of glaciers, increased acidification of the oceans, an increase in extreme weather events and, ultimately, rising sea levels. Climate change, however, is not just a change in temperature, but involves changes in a number of complex interacting systems within the Earth, of which the biosphere is an important part. The bios

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Scussolini, Paolo, Job Dullaart, Sanne Muis, et al. "Modeled storm surge changes in a warmer world: the Last Interglacial." Climate of the Past 19, no. 1 (2023): 141–57. http://dx.doi.org/10.5194/cp-19-141-2023.

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Abstract. The Last Interglacial (LIG; ca. 125 ka) is a period of interest for climate research as it is the most recent period of the Earth's history when the boreal climate was warmer than at present. Previous research, based on models and geological evidence, suggests that the LIG may have featured enhanced patterns of ocean storminess, but this remains hotly debated. Here, we apply state-of-the-art climate and hydrodynamic modeling to simulate changes in sea level extremes caused by storm surges, under LIG and pre-industrial climate forcings. Significantly higher seasonal LIG sea level extr

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Sk, Mustak Hossain. "About Climate Change." International Journal of Advance and Applied Research 4, no. 10 (2023): 114–15. https://doi.org/10.5281/zenodo.7820647.

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Global warming and long-term changes in weather conditions are called climate change. As a result of this climate change, people as well as the world's living things are facing various problems. The main causes of this climate change are air pollution, deforestation, population growth, global warming etc.

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Lu, Wei-Shiun, Chi-Hsiang Tseng, Shih-Chun Hsiao, Wen-Son Chiang, and Kai-Cheng Hu. "Future Projection for Wave Climate around Taiwan Using Weather-Type Statistical Downscaling Method." Journal of Marine Science and Engineering 10, no. 12 (2022): 1823. http://dx.doi.org/10.3390/jmse10121823.

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Taiwan is surrounded by sea; therefore, coastal hazards might become severe due to climate change. The analysis of wave climate characteristics at different time scales (long-term historical period, seasonal prediction, and future prediction) can be used as a reference for the impact of climate change on coastal environments. This model associates the significant wave height with the atmospheric predictor defined by the sea level pressure (SLP) field. We applied SLP based on the outputs of a global climate model (GCM) under two possible future scenarios (RCP4.5 and RCP8.5) in the Fifth Assessm

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Vaidya, Hanna N., Robert D. Breininger, Marisela Madrid, Steven Lazarus, and Nezamoddin N. Kachouie. "Generalized Additive Models for Predicting Sea Level Rise in Coastal Florida." Geosciences 13, no. 10 (2023): 310. http://dx.doi.org/10.3390/geosciences13100310.

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Within the last century, the global sea level has risen between 16 and 21 cm and will likely accelerate into the future. Projections from the Intergovernmental Panel on Climate Change (IPCC) show the global mean sea level (GMSL) rise may increase to up to 1 m (1000 mm) by 2100. The primary cause of the sea level rise can be attributed to climate change through the thermal expansion of seawater and the recession of glaciers from melting. Because of the complexity of the climate and environmental systems, it is very difficult to accurately predict the increase in sea level. The latest estimate o

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