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Journal articles on the topic 'Mean sea level rise'

Author: Grafiati

Published: 9 September 2021

Last updated: 29 July 2025

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1

Isiaka, Ibrahim, Kingsley Ndukwe, and Ufomba Chibuike. "Mean Sea Level: The Effect of the Rise in the Environment." Journal of Geoinformatics & Environmental Research 2, no. 2 (2022): 92–102. http://dx.doi.org/10.38094/jgier2235.

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Mean sea level is a significant phenomenon in geodetic science and oceanography. The sea level has experienced an unprecedented rise recently, and this increase can be attributed to the various human-induced activities (anthropogenic factors) ranging from deforestation to burning of fossil fuels and population increase. Several factors cause sea level rise, it has been identified that the thermal expansion of ocean water and the melting of glaciers add to the volume of water causing global sea level to rise, whereas phenomena such as ocean current, wind, pressure are responsible for the region

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2

Isiaka, Ibrahim, Kingsley Ndukwe, and Ufomba Chibuike. "Mean Sea Level: The Effect of the Rise in the Environment." Journal of Applied Science and Technology Trends 4, no. 2 (2023): 94–100. http://dx.doi.org/10.38094/jastt42178.

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Mean sea level is a significant phenomenon in geodetic science and oceanography. The sea level has experienced an unprecedented rise recently, and this increase can be attributed to various human-induced activities (anthropogenic factors) ranging from deforestation to the burning of fossil fuels and population increases. Several factors cause sea level rise. It has been identified that the thermal expansion of ocean water and the melting of glaciers add to the volume of water, causing global sea level to rise, whereas phenomena such as ocean current, wind, and pressure are responsible for the

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3

Hernández, M., C. A. Martínez, and O. Marzo. "Consequences of sea level variability and sea level rise for Cuban territory." Proceedings of the International Association of Hydrological Sciences 365 (March 2, 2015): 22–27. http://dx.doi.org/10.5194/piahs-365-22-2015.

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Abstract. The objective of the present paper was to determine a first approximation of coastal zone flooding by 2100, taking into account the more persistent processes of sea level variability and non-accelerated linear sea level rise estimation to assess the main impacts. The annual linear rate of mean sea level rise in the Cuban archipelago, obtained from the longest tide gauge records, has fluctuated between 0.005 cm/year at Casilda and 0.214 cm/year at Siboney. The main sea level rise effects for the Cuban coastal zone due to climate change and global warming are shown. Monthly and annual

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4

Tan, Willie. "The rise in mean sea level: A comment." Australian Surveyor 35, no. 4 (1990): 368–70. http://dx.doi.org/10.1080/00050326.1990.10438697.

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5

Kaczkowski, Stephen. "Mathematical Models for Global Mean Sea Level Rise." College Mathematics Journal 48, no. 3 (2017): 162–69. http://dx.doi.org/10.4169/college.math.j.48.3.162.

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6

Watson, Phil J. "Status of Mean Sea Level Rise around the USA (2020)." GeoHazards 2, no. 2 (2021): 80–100. http://dx.doi.org/10.3390/geohazards2020005.

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The potential threats to the USA from current and projected sea level rise are significant, with profound environmental, social and economic consequences. This current study continues the refinement and improvement in analysis techniques for sea level research beyond the Fourth US National Climate Assessment (NCA4) report by incorporating further advancements in the time series analysis of long tide gauge records integrated with an improved vertical land motion (VLM) assessment. This analysis has also been synthesised with an updated regional assessment of satellite altimetry trends in the sea

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Viv, Djanat Prasita, Asyiah Agustina Nur, and Supartono. "Sea Level Fluctuations and Rates in the Kenjeran Coast, Surabaya and Its Surroundings." Sea Level Fluctuations and Rates in the Kenjeran Coast, Surabaya and Its Surroundings 08, no. 11 (2022): 829–40. https://doi.org/10.5281/zenodo.7365070.

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Kenjeran is one of the famous tourist areas in the city of Surabaya with a population of 7,021 people, most of which are concentrated in the coastal area. The coastal area of Surabaya is an area that is affected by sea level rise. Therefore, the purpose of this study was to determine the types of tides that exist in the Kenjeran Region of Surabaya and how much sea level fluctuations and the rate of sea level rise were using real-time tidal data for 2014-2021 and Altrimetry satellite data in the period 2002-2021. The analytical method for tidal calculations was the Admiralty calculation and oth

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8

Elipot, Shane, Luca Centurioni, Bruce J. Haines, Rick Lumpkin, and Josh K. Willis. "Measuring Global-Mean Sea-Level Rise With Surface Drifting Buoys." Marine Technology Society Journal 55, no. 3 (2021): 66–67. http://dx.doi.org/10.4031/mtsj.55.3.12.

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Abstract We propose to establish a new ocean observing system for monitoring global and regional mean sea-level changes. This system will consist of a global array of thousands of water-following drifting buoys tracked by a global navigation satellite system—such as the Global Positioning System (GPS)—which will continuously provide the geographical positions and the height of the sea surface along the buoys' trajectories. The sea-level height data collected in this way, averaged over regional basins and the global ocean, will provide daily measures of regional and global mean sea levels. An e

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9

Grinsted, Aslak, and Jens Hesselbjerg Christensen. "The transient sensitivity of sea level rise." Ocean Science 17, no. 1 (2021): 181–86. http://dx.doi.org/10.5194/os-17-181-2021.

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Abstract. Recent assessments from the Intergovernmental Panel on Climate Change (IPCC) imply that global mean sea level is unlikely to rise more than about 1.1 m within this century but will increase further beyond 2100. Even within the most intensive future anthropogenic greenhouse gas emission scenarios, higher levels are assessed to be unlikely. However, some studies conclude that considerably greater sea level rise could be realized, and a number of experts assign a substantially higher likelihood of such a future. To understand this discrepancy, it would be useful to have scenario-indepen

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10

Gregory, J. M., J. A. Lowe, and S. F. B. Tett. "Simulated Global-Mean Sea Level Changes over the Last Half-Millennium." Journal of Climate 19, no. 18 (2006): 4576–91. http://dx.doi.org/10.1175/jcli3881.1.

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Abstract Simulations of the last 500 yr carried out using the Third Hadley Centre Coupled Ocean–Atmosphere GCM (HadCM3) with anthropogenic and natural (solar and volcanic) forcings have been analyzed. Global-mean surface temperature change during the twentieth century is well reproduced. Simulated contributions to global-mean sea level rise during recent decades due to thermal expansion (the largest term) and to mass loss from glaciers and ice caps agree within uncertainties with observational estimates of these terms, but their sum falls short of the observed rate of sea level rise. This disc

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11

Sergent, Philippe, Guirec Prevot, Giovanni Mattarolo, et al. "Adaptation of coastal structures to mean sea level rise." La Houille Blanche, no. 6 (December 2014): 54–61. http://dx.doi.org/10.1051/lhb/2014063.

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12

Dangendorf, Sönke, Marta Marcos, Guy Wöppelmann, Clinton P. Conrad, Thomas Frederikse, and Riccardo Riva. "Reassessment of 20th century global mean sea level rise." Proceedings of the National Academy of Sciences 114, no. 23 (2017): 5946–51. http://dx.doi.org/10.1073/pnas.1616007114.

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The rate at which global mean sea level (GMSL) rose during the 20th century is uncertain, with little consensus between various reconstructions that indicate rates of rise ranging from 1.3 to 2 mm⋅y−1. Here we present a 20th-century GMSL reconstruction computed using an area-weighting technique for averaging tide gauge records that both incorporates up-to-date observations of vertical land motion (VLM) and corrections for local geoid changes resulting from ice melting and terrestrial freshwater storage and allows for the identification of possible differences compared with earlier attempts. Ou

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13

Bouttes, N., J. M. Gregory, and J. A. Lowe. "The Reversibility of Sea Level Rise." Journal of Climate 26, no. 8 (2013): 2502–13. http://dx.doi.org/10.1175/jcli-d-12-00285.1.

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Abstract During the last century, global climate has been warming, and projections indicate that such a warming is likely to continue over coming decades. Most of the extra heat is stored in the ocean, resulting in thermal expansion of seawater and global mean sea level rise. Previous studies have shown that after CO2 emissions cease or CO2 concentration is stabilized, global mean surface air temperature stabilizes or decreases slowly, but sea level continues to rise. Using idealized CO2 scenario simulations with a hierarchy of models including an AOGCM and a step-response model, the authors s

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14

Guttorp, Peter, Alex Januzzi, Marie Novak, et al. "Assessing the Uncertainty in Projecting Local Mean Sea Level from Global Temperature." Journal of Applied Meteorology and Climatology 53, no. 9 (2014): 2163–70. http://dx.doi.org/10.1175/jamc-d-13-0308.1.

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AbstractThe process of moving from an ensemble of global climate model temperature projections to local sea level projections requires several steps. Sea level was estimated in Olympia, Washington (a city that is very concerned with sea level rise because parts of downtown are barely above mean highest high tide), by relating global mean temperature to global sea level; relating global sea level to sea levels at Seattle, Washington; and finally relating Seattle to Olympia. There has long been a realization that accurate assessment of the precision of projections is needed for science-based pol

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15

Rasquin, Caroline, Rita Seiffert, Benno Wachler, and Norbert Winkel. "The significance of coastal bathymetry representation for modelling the tidal response to mean sea level rise in the German Bight." Ocean Science 16, no. 1 (2020): 31–44. http://dx.doi.org/10.5194/os-16-31-2020.

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Abstract. Due to climate change an accelerated mean sea level rise is expected. One key question for the development of adaptation measures is how mean sea level rise affects tidal dynamics in shelf seas such as the North Sea. Owing to its low-lying coastal areas, the German Bight (located in the southeast of the North Sea) will be especially affected. Numerical hydrodynamic models help to understand how mean sea level rise changes tidal dynamics. Models cannot adequately represent all processes in overall detail. One limiting factor is the resolution of the model grid. In this study we invest

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16

Hadikusumah. "STUDY ON SEA LEVEL RISE IN THE WESTERN INDONESIA." Marine Research in Indonesia 29 (May 11, 2018): 31–40. http://dx.doi.org/10.14203/mri.v29i0.419.

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Study on mean sea level (MSL) rise has been done on tide data at some locations in the Western Indonesia. To account the effect of climate change, air temperature analyses from some weather stations are also performed. The results showed that air temperature has changed between 0.0 to 0.44°C per ten years. The sea level analysis showed that mean sea level at Western Indonesia rise between 3.10 to 9.27 mm per year. Based on the results, the prediction on mean sea level change in the years of 2000, 2030, 2050 and 2100 for Cirebon location are 17 cm, 39 cm, 55 cm, and 92 cm, respectively.

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17

Watson, Phil J., and Hak-Soo Lim. "An Update on the Status of Mean Sea Level Rise around the Korean Peninsula." Atmosphere 11, no. 11 (2020): 1153. http://dx.doi.org/10.3390/atmos11111153.

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The threat of sea level rise to the heavily populated Korean Peninsula, which contains around 15,000 km of coastline bordering open sea margins, has profound and far reaching implications. This study updates and extends previous detailed studies with the addition of a further 2 years of data to the end of 2019, providing renewed robustness to the identification of emerging threats associated with sea level rise within the warming sea margins around the Korean Peninsula. The study analyzes tide gauge records and satellite altimetry around the Republic of Korea using enhanced time series analysi

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18

Slangen, Aimée B. A., John A. Church, Cecile Agosta, Xavier Fettweis, Ben Marzeion, and Kristin Richter. "Anthropogenic forcing dominates global mean sea-level rise since 1970." Nature Climate Change 6, no. 7 (2016): 701–5. http://dx.doi.org/10.1038/nclimate2991.

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19

McLeman, Robert. "Migration and displacement risks due to mean sea-level rise." Bulletin of the Atomic Scientists 74, no. 3 (2018): 148–54. http://dx.doi.org/10.1080/00963402.2018.1461951.

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20

Kivioja, Lasse. "Is it just a rise in the mean sea level?" Eos, Transactions American Geophysical Union 84, no. 10 (2003): 90. http://dx.doi.org/10.1029/2003eo100010.

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21

Flick, Reinhard E., Kevin Knuuti, and Stephen K. Gill. "Matching Mean Sea Level Rise Projections to Local Elevation Datums." Journal of Waterway, Port, Coastal, and Ocean Engineering 139, no. 2 (2013): 142–46. http://dx.doi.org/10.1061/(asce)ww.1943-5460.0000145.

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22

Yi, Shuang, Kosuke Heki, and An Qian. "Acceleration in the Global Mean Sea Level Rise: 2005-2015." Geophysical Research Letters 44, no. 23 (2017): 11,905–11,913. http://dx.doi.org/10.1002/2017gl076129.

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23

Sadai, Shaina, Meghana Ranganathan, Alexander Nauels, et al. "Estimating the sea level rise responsibility of industrial carbon producers." Environmental Research Letters 20, no. 4 (2025): 044012. https://doi.org/10.1088/1748-9326/adb59f.

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Abstract Global mean sea levels have risen at an accelerating rate over the past century in response, primarily to greenhouse gas emissions from the combustion of fossil fuels. We use MAGICC7, a reduced complexity climate-carbon cycle model, to quantify how emissions traced to the Carbon Majors, the world’s 122 largest fossil fuel and cement producers, from 1854–2020 contributed to present-day surface air temperature rise, and sea level rise both historically and projected through 2300. We find that emissions traced to these industrial actors have contributed 37%–58% to present day surface air

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24

Antunes, Carlos. "Assessment of Sea Level Rise at West Coast of Portugal Mainland and Its Projection for the 21st Century." Journal of Marine Science and Engineering 7, no. 3 (2019): 61. http://dx.doi.org/10.3390/jmse7030061.

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Based on the updated relative sea level rise rates, 21st-century projections are made for the west coast of Portugal Mainland. The mean sea level from Cascais tide gauge and North Atlantic satellite altimetry data have been analyzed. Through bootstrapping linear regression and polynomial adjustments, mean sea level time series were used to calculate different empirical projections for sea level rise, by estimating the initial velocity and its corresponding acceleration. The results are consistent with an accelerated sea level rise, showing evidence of a faster rise than previous century estima

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25

Widlansky, Matthew J., Axel Timmermann, and Wenju Cai. "Future extreme sea level seesaws in the tropical Pacific." Science Advances 1, no. 8 (2015): e1500560. http://dx.doi.org/10.1126/sciadv.1500560.

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Global mean sea levels are projected to gradually rise in response to greenhouse warming. However, on shorter time scales, modes of natural climate variability in the Pacific, such as the El Niño–Southern Oscillation (ENSO), can affect regional sea level variability and extremes, with considerable impacts on coastal ecosystems and island nations. How these shorter-term sea level fluctuations will change in association with a projected increase in extreme El Niño and its atmospheric variability remains unknown. Using present-generation coupled climate models forced with increasing greenhouse ga

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26

Cha, Hyeonsoo, Jae-Hong Moon, Taekyun Kim, and Y. Tony Song. "Underlying drivers of decade-long fluctuation in the global mean sea-level rise." Environmental Research Letters 16, no. 12 (2021): 124064. http://dx.doi.org/10.1088/1748-9326/ac3d58.

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Abstract Natural climate variability can mask the background trend of global mean sea-level (GMSL) caused by global warming. Recent advances in satellite measurements and ocean heat-content estimates have enabled the monitoring of GMSL budget components and provide insights into ocean effects on the Earth’s energy imbalance and hydrology. We observed a decadal fluctuation in GMSL rise, which coincides with an increasing trend in the 2010s after the warming ‘hiatus’ during the 2000s, and demonstrated that the rate of sea-level rise can be attributed to climate-related decadal fluctuations in oc

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Gräwe, Ulf, Knut Klingbeil, Jessica Kelln, and Sönke Dangendorf. "Decomposing Mean Sea Level Rise in a Semi-Enclosed Basin, the Baltic Sea." Journal of Climate 32, no. 11 (2019): 3089–108. http://dx.doi.org/10.1175/jcli-d-18-0174.1.

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Abstract We analyzed changes in mean sea level (MSL) for the period 1950–2015 using a regional ocean model for the Baltic Sea. Sensitivity experiments allowed us to separate external from local drivers and to investigate individual forcing agents triggering basin-internal spatial variations. The model reveals a basin-average MSL rise (MSLR) of 2.08 ± 0.49 mm yr−1, a value that is slightly larger than the simultaneous global average of 1.63 ± 0.32 mm yr−1. This MSLR is, however, spatially highly nonuniform with lower than average increases in the southwestern part (1.71 ± 0.51 mm yr−1) and high

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Hieronymus, Magnus, Christian Dieterich, Helén Andersson, and Robinson Hordoir. "The effects of mean sea level rise and strengthened winds on extreme sea levels in the Baltic Sea." Theoretical and Applied Mechanics Letters 8, no. 6 (2018): 366–71. http://dx.doi.org/10.1016/j.taml.2018.06.008.

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29

Allison, Lesley C., Matthew D. Palmer, and Ivan D. Haigh. "Projections of 21st century sea level rise for the coast of South Africa." Environmental Research Communications 4, no. 2 (2022): 025001. http://dx.doi.org/10.1088/2515-7620/ac4a90.

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Abstract As a result of planetary heating, global mean sea level has increased since the end of the 19th century. Sea level rise is accelerating and will continue to rise over the 21st century and beyond. On top of the global mean signal there are large regional variations in the magnitude of sea level rise. At a local level, reliable projections of probable and possible future sea level change are vital for coastal management planning. In this work we present an observational analysis of recent sea level variations at locations around the coast of South Africa using tide gauge records and sat

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Khasanah, Isna Uswatun. "Sea Level Rise of Sumatera Waters based on Multi-Satellite Altimetry Data." Indonesian Journal of Geography 50, no. 2 (2018): 162. http://dx.doi.org/10.22146/ijg.27328.

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The information of sea level rise was needed in the Indonesia as archipelago country to management risk and development coastal area. This research study took in West Sumatra waters, because the majority people have lived in coastal area and some areas is located below 100 m above Mean Sea Level (MSL). The sea level data was taken from multi-satellite altimetry, they are Topex/Poseidon, Jason-1, and Jason-2. The period of data started from 1993 until 2015.Preliminary data processing of satellite altimetry was done by global test and post-processing of satellite altimetry data. The sea level ri

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31

Kim, A. Jeong, Myeong Hee Lee, and Seung Won Suh. "Effect of Summer Sea Level Rise on Storm Surge Analysis." Journal of Korean Society of Coastal and Ocean Engineers 33, no. 6 (2021): 298–307. http://dx.doi.org/10.9765/kscoe.2021.33.6.298.

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Typhoons occur intensively between July and October, and the sea level is the highest during this time. In particular, the mean sea level in summer in Korea is higher than the annual mean sea level about 14.5cm in the west coast, 9.0 to 14.5cm in the south coast, and about 9.0 cm in the east coast. When the rising the sea level and a large typhoon overlap in summer, it can cause surges and flooding in low-lying coastal areas. Therefore, accurate calculation of the surge height is essential when designing coastal structures and assessing stability in order to reduce coastal hazards on the lowla

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32

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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33

KIM, Jang-soo, and Dong-Ho JANG. "Vulnerability Assessment under the Sea Level Rise Considering Regional Mean sea-level in Taean-gun, Korea." Journal of Climate Research 8, no. 3 (2013): 253–65. http://dx.doi.org/10.14383/cri.2013.8.3.253.

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34

Perrette, M., F. Landerer, R. Riva, K. Frieler, and M. Meinshausen. "A scaling approach to project regional sea level rise and its uncertainties." Earth System Dynamics 4, no. 1 (2013): 11–29. http://dx.doi.org/10.5194/esd-4-11-2013.

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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 can strongly deviate from the global mean rise due to changes in wind and ocean currents. In addition, gravitational adjustments redistribute seawater away from shrinking ice masses. However, the land ice contribution to sea level rise (SLR) remains very challenging to model, and comprehensive regional sea level projections, which include appropriate gravitational adjustments, are still a nascent field (Katsm

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35

Mucova, Serafino Afonso Rui, Ulisses Miranda Azeiteiro, Walter Leal Filho, Carina Lurdes Lopes, João Miguel Dias, and Mário Jorge Pereira. "Approaching Sea-Level Rise (SLR) Change: Strengthening Local Responses to Sea-Level Rise and Coping with Climate Change in Northern Mozambique." Journal of Marine Science and Engineering 9, no. 2 (2021): 205. http://dx.doi.org/10.3390/jmse9020205.

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Mean sea-level is expected to rise significantly by 2100 in all scenarios, including those compatible with the objectives of the Paris Climate Agreement. Global sea level rise projections indicate devastating implications for populations, ecosystem services and biodiversity. The implications of the sea-level rise (SLR) on low-lying islands and coastal regions and communities are substantial and require deep-rooted coping measures. In the absence of adequate responses for coping, Mozambique is expected to record huge losses, with an impact on the economy and development in many sectors of its c

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36

Bâki Iz, H., L. Berry, and M. Koch. "Modeling regional sea level rise using local tide gauge data." Journal of Geodetic Science 2, no. 3 (2012): 188–99. http://dx.doi.org/10.2478/v10156-011-0039-2.

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AbstractCurrently regional mean sea level trends and variations are inferred from the analysis of several individual local tide gauge data that spanonly a long period of time at a given region. In this study, we propose using a model to merge various tide gauge data, regardless of theirtime span, in a single solution, to estimate parameters representative of regional mean sea level trends. The proposed model can accountfor the geographical correlations among the local tide gauge stations as well as serial correlations, if needed, for individual stations’ data.Such a vigorous regional solution

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37

Kelln, Jessica, SÃ¶nke Dangendorf, JÃ¼rgen Jensen, et al. "GEOCENTRIC MEAN SEA LEVEL FIELDS AT THE GERMAN NORTH SEA AND BALTIC COAST." Coastal Engineering Proceedings, no. 36 (December 30, 2018): 21. http://dx.doi.org/10.9753/icce.v36.currents.21.

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Global mean sea level has risen over the 20th century (Hay et al. 2015; Dangendorf et al. 2017) and under sustained greenhouse gas emissions it is projected to further accelerate throughout the 21st century (Church et al. 2013) with large spatial variations, significantly threatening coastal communities. Locally the effects of geocentric (sometimes also referred to absolute) sea level rise can further be amplified by vertical land motion (VLM) due to natural adjustments of the solid earth to the melting of the large ice-sheets during the last deglaciation (GIA) or local anthropogenic intervent

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Tkalich, P., M. T. Babu, and P. Vethamony. "Technical Note: Mean sea level variation in the Singapore Strait from long-term tide data." Ocean Science Discussions 9, no. 3 (2012): 2255–71. http://dx.doi.org/10.5194/osd-9-2255-2012.

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Abstract. Winds over the South China Sea (SCS) are primarily responsible for the observed variability in sea level anomalies (SLAs) in the Singapore Strait (SS). The present study focuses on remote forcing contributing to local mean sea level changes in the SS in seasonal and inter-annual scales, and relating the long term mean sea level variation to El Niño/ENSO. As Tanjong Pagar (TP) tide station in the SS has nearly 23.5 yr (1984–2007) of time series data with less data gaps, this data was subject to harmonic and sea level analyses. The mean sea level changes suggest that the fluctuations a

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Kim, Minwoo, Cheol-Ho Kim, and Chan Joo Jang. "Projection of future sea level rise in the East Asian Seas based on Global Ocean-Sea Ice Coupled Model with SRES A1B Scenario." Korea Society of Coastal Disaster Prevention 8, no. 4 (2021): 281–86. http://dx.doi.org/10.20481/kscdp.2021.8.4.281.

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To project the future sea level rise in the East Asian Seas due to global warming, regional sea level variations are downscaled from three climate system models (GFDL-CM2.1, ECHAM5/MPI-OM, MIROC3.2(hires)) using a global ocean-sea ice coupled model with non-Boussinesq approximation. Based on the SRES A1B Scenario, the projected ensemble mean sea level rise (rate of rise) for the East Sea, Yellow Sea and East China Sea from 1995 to 2050 is 15.60cm (2.84mm/year), 16.49cm (3.0mm/year) and 16.43cm (2.99mm/year), respectively. With the inclusion of the future change of land ice melting and land wat

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Kopp, Robert E., Gregory G. Garner, Tim H. J. Hermans, et al. "The Framework for Assessing Changes To Sea-level (FACTS) v1.0: a platform for characterizing parametric and structural uncertainty in future global, relative, and extreme sea-level change." Geoscientific Model Development 16, no. 24 (2023): 7461–89. http://dx.doi.org/10.5194/gmd-16-7461-2023.

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Abstract. Future sea-level rise projections are characterized by both quantifiable uncertainty and unquantifiable structural uncertainty. Thorough scientific assessment of sea-level rise projections requires analysis of both dimensions of uncertainty. Probabilistic sea-level rise projections evaluate the quantifiable dimension of uncertainty; comparison of alternative probabilistic methods provides an indication of structural uncertainty. Here we describe the Framework for Assessing Changes To Sea-level (FACTS), a modular platform for characterizing different probability distributions for the

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Khasanah, Isna Uswatun. "KENAIKAN MUKA AIR LAUT PERAIRAN SUMATERA BARAT BERDASARKAN DATA SATELIT ALTIMETRI JASON-2." JURNAL ILMIAH GEOMATIKA 23, no. 1 (2017): 1. http://dx.doi.org/10.24895/jig.2017.23-1.623.

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<p><em>The phenomenon of the sea level rise caused by many factors, one of which is global warming. Coastal areas are most vulnerable regions affected by sea level rise. Therefore, the information of sea level rise are used as consideration and policy-making on development plans for coastal areas like in West Sumatera Waters. The aims of this research are to identify the quality of Satelit Altimetry Jason-2 Data in West Sumatera Waters and to analysis the information of sea level rise of West Sumatera sea based on satelit altimetry Jason-2 data. Sea Level Rise in West Sumatera Wate

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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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Park, J., and W. Sweet. "Accelerated sea level rise and Florida Current transport." Ocean Science 11, no. 4 (2015): 607–15. http://dx.doi.org/10.5194/os-11-607-2015.

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Abstract. The Florida Current is the headwater of the Gulf Stream and is a component of the North Atlantic western boundary current from which a geostrophic balance between sea surface height and mass transport directly influence coastal sea levels along the Florida Straits. A linear regression of daily Florida Current transport estimates does not find a significant change in transport over the last decade; however, a nonlinear trend extracted from empirical mode decomposition (EMD) suggests a 3 Sv decline in mean transport. This decline is consistent with observed tide gauge records in Florid

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Park, J., and W. Sweet. "Accelerated sea level rise and Florida Current transport." Ocean Science Discussions 12, no. 2 (2015): 551–72. http://dx.doi.org/10.5194/osd-12-551-2015.

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Abstract. The Florida Current is the headwater of the Gulf Stream and is a component of the North Atlantic western boundary current from which a geostrophic balance between sea surface height and mass transport directly influence coastal sea levels along the Florida Straits. A linear regression of daily Florida Current transport estimates does not find a significant change in transport over the last decade, however, a nonlinear trend extracted from empirical mode decomposition suggests a 3 Sv decline in mean transport. This decline is consistent with observed tide gauge records in Florida Bay

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Blume, P. H. "The rise and rise of mean sea level and other natural phenomena at Sydney." Australian Surveyor 34, no. 8 (1989): 786–801. http://dx.doi.org/10.1080/00050326.1989.10438620.

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Nauels, Alexander, Johannes Gütschow, Matthias Mengel, Malte Meinshausen, Peter U. Clark, and Carl-Friedrich Schleussner. "Attributing long-term sea-level rise to Paris Agreement emission pledges." Proceedings of the National Academy of Sciences 116, no. 47 (2019): 23487–92. http://dx.doi.org/10.1073/pnas.1907461116.

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The main contributors to sea-level rise (oceans, glaciers, and ice sheets) respond to climate change on timescales ranging from decades to millennia. A focus on the 21st century thus fails to provide a complete picture of the consequences of anthropogenic greenhouse gas emissions on future sea-level rise and its long-term impacts. Here we identify the committed global mean sea-level rise until 2300 from historical emissions since 1750 and the currently pledged National Determined Contributions (NDC) under the Paris Agreement until 2030. Our results indicate that greenhouse gas emissions over t

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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 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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Li, Ying, Enshang Yang, Yun Pan, and Yun Gao. "Numerical Modeling of the Impact of Sea Level Rise on Tidal Asymmetry in Hangzhou Bay." Journal of Marine Science and Engineering 10, no. 10 (2022): 1445. http://dx.doi.org/10.3390/jmse10101445.

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The tidal asymmetry under the action of sea level rise in Hangzhou Bay. Coastlines dominated by the tide are not only directly affected by the rise of the mean sea level but also by the tidal dynamics. The computational domain of the hydrodynamic model covers the entire Hangzhou Bay and takes into account the feedback between the tidal motion and the erodible bottom. Its main application fields include: the simulation of different sea level rise (SLR) rates, the interaction between tidal duration and skewness and the interaction between tidal range and astronomical tide. The results on tidal a

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Watson, Christopher S., Neil J. White, John A. Church, Matt A. King, Reed J. Burgette, and Benoit Legresy. "Unabated global mean sea-level rise over the satellite altimeter era." Nature Climate Change 5, no. 6 (2015): 565–68. http://dx.doi.org/10.1038/nclimate2635.

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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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