<doi_batch xmlns="http://www.crossref.org/schema/4.4.0" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" version="4.4.0"><head><doi_batch_id>743908e7-5dfd-4419-b890-b34b85eb2ab9</doi_batch_id><timestamp>20251125122909022</timestamp><depositor><depositor_name>wseas:wseas</depositor_name><email_address>mdt@crossref.org</email_address></depositor><registrant>MDT Deposit</registrant></head><body><journal><journal_metadata language="en"><full_title>International Journal of Environmental Engineering and Development</full_title><issn media_type="electronic">2945-1159</issn><archive_locations><archive name="Portico" /></archive_locations><doi_data><doi>10.37394/232033</doi><resource>https://wseas.com/journals/ijeed/</resource></doi_data></journal_metadata><journal_issue><publication_date media_type="online"><month>4</month><day>23</day><year>2025</year></publication_date><publication_date media_type="print"><month>4</month><day>23</day><year>2025</year></publication_date><journal_volume><volume>3</volume><doi_data><doi>10.37394/232033.2025.3</doi><resource>https://wseas.com/journals/ijeed/2025.php</resource></doi_data></journal_volume></journal_issue><journal_article language="en"><titles><title>Most Probable Origin and Statistical Attribution of the Major Causes of Global Mean Sea Level Anomaly and Rising Tides Since the 20th Century</title></titles><contributors><person_name sequence="first" contributor_role="author"><given_name>Paul C.</given_name><surname>Rivera</surname><affiliation>Astrometocean Department Hymetocean Peers Company Antipolo City PHILIPPINES</affiliation></person_name></contributors><jats:abstract xmlns:jats="http://www.ncbi.nlm.nih.gov/JATS1"><jats:p>The origin of the anomalous global sea level rise (SLR) since the last century is highly controversial and not fully understood. The observed increase of high tides and decrease of low tides in many coastal areas around the world imply that some crucial physical mechanisms that govern the rising sea levels may have been overlooked. The relative contribution of nutation, axial precession, lunar acceleration, Earth’s spin and sea surface temperature on sea level anomaly was estimated using multiple regression. A very high relative contribution of the polar migration (49.4%) on the mean sea level rise, followed by axial precession (46.7%) and a secondary contribution of lunar acceleration (3.9%) was found. Sea surface temperature and earth spin rate showed negative correlations with sea level rise. The annual changes of the polar migration, axial precession and lunar acceleration appear to be the dominant physical mechanisms behind the SLR problem. These factors are largely driven by strong earthquakes. The rising oceanic tides in the last century up to the present is largely due to North Pole migration. Apparently, the observed nutation and axial precession are caused by the increased eccentricity of the lunar orbit through changes in the lunar distance and lunar acceleration. Finally, the observed SLR was found to be related to the enigmatic 26-second microseism problem. Using the annual geomagnetic North Pole migration dataset of NOAA-NGDC, the observed frequency of 0.038 Hz was found. This possibly indicates that the planet is gradually tilting as it spins with a concomitant gradual build-up of oceanic pressure and release of magmatic and gas pressure, due to lunar-induced sea level rise and reduced lunar distance.</jats:p></jats:abstract><publication_date media_type="online"><month>11</month><day>25</day><year>2025</year></publication_date><publication_date media_type="print"><month>11</month><day>25</day><year>2025</year></publication_date><pages><first_page>311</first_page><last_page>321</last_page></pages><publisher_item><item_number item_number_type="article_number">26</item_number></publisher_item><ai:program xmlns:ai="http://www.crossref.org/AccessIndicators.xsd" name="AccessIndicators"><ai:free_to_read start_date="2025-11-25" /><ai:license_ref applies_to="am" start_date="2025-11-25">https://wseas.com/journals/ijeed/2025/a52ijeed-021(2025).pdf</ai:license_ref></ai:program><archive_locations><archive name="Portico" /></archive_locations><doi_data><doi>10.37394/232033.2025.3.26</doi><resource>https://wseas.com/journals/ijeed/2025/a52ijeed-021(2025).pdf</resource></doi_data><citation_list><citation key="ref0"><doi>10.54097/xkxh4q35</doi><unstructured_citation>Bai, Y., Chang S. &amp; Wu S. (2024). Relationship between Earth-Moon Distance and Tides. Highlights in Science, Engineering and Technology, Vol. 85, p. 285-292. </unstructured_citation></citation><citation key="ref1"><unstructured_citation>Cheng, L., et al. (2020). "Ocean Heat Content and its Role in Sea Level Rise." Journal of Climate, 33(12), 5207-5225. DOI: 10.1175/JCLI-D-19-0932.1 </unstructured_citation></citation><citation key="ref2"><unstructured_citation>Cheng, L., et al. (2023). "Ocean Heat Content and Thermal Expansion." Journal of Climate, 36(4), 987-1005. DOI: 10.1175/JCLI-D-22-0523.1 </unstructured_citation></citation><citation key="ref3"><doi>10.1007/s10712-011-9119-1</doi><unstructured_citation>Church J.A. &amp; White N.J. (2011). Sea-Level Rise from the Late 19th to the Early 21st Century. Surv. Geophys, 32:585-602. DOI 10.1007/s10712-011-9119-1 </unstructured_citation></citation><citation key="ref4"><unstructured_citation>Church, J.A., et al. (2011). "Climate Change and Sea Level Rise." Nature, 472(7345), 435-443. DOI: 10.1038/nature09964 </unstructured_citation></citation><citation key="ref5"><doi>10.1029/2005gl024826</doi><unstructured_citation>Church, J.A., &amp; White, N.J. (2006). "A 20th century acceleration in global sea-level rise." Geophysical Research Letters, 33, L01602. DOI: 10.1029/2005GL024826 </unstructured_citation></citation><citation key="ref6"><unstructured_citation>Dangendorf, S., et al. (2023). Persistent acceleration in global sea-level rise since the 1960s. Nat. Climate. doi.org/10.1038/s41558-019-0531-8 </unstructured_citation></citation><citation key="ref7"><unstructured_citation>Dangendorf, S., et al. (2023). "Regional Sea Level Change and Coastal Impacts." Surveys in Geophysics, 44(1), 123-145. DOI: 10.1007/s10712-022-09663-2 </unstructured_citation></citation><citation key="ref8"><unstructured_citation>Douglas, B.C., Kearney, M.S., &amp; Leatherman, S.P. (2001). "Sea Level Rise: History and Consequences." Reviews of Geophysics, 39(2), 215-230. DOI: 10.1029/2000RG000098 </unstructured_citation></citation><citation key="ref9"><doi>10.1002/2013gl059010</doi><unstructured_citation>Enderlin, E.M., et al. (2014). "An Improved Mass Budget for the Greenland Ice Sheet." Geophysical Research Letters, 41(3), 866-872. DOI: 10.1002/2013GL059010 </unstructured_citation></citation><citation key="ref10"><doi>10.5194/os-16-997-2020</doi><unstructured_citation>Ezer T. &amp; Dangendorf S. (2020). Global sea level reconstruction for 1900- 2015 reveals regional variability in ocean dynamics and an unprecedented long weakening in the Gulf Stream flow since the 1990s. Ocean Sci., 16, 997-1016, doi.org/10.5194/os-16-997-2020. </unstructured_citation></citation><citation key="ref11"><unstructured_citation>Franc, T. (2012). "Tides in the EarthMoon System." Week of Doctoral Students 2012-Proceedings of Contributed Papers: Part III-Physics (WDS12), Prague: Matfyz Press Publishing House. </unstructured_citation></citation><citation key="ref12"><unstructured_citation>Frederikse, T., et al. (2024). "The Causes of Sea Level Rise since 1900." Nature, 585(7824), 421-425. DOI: 10.1038/s41586-020-2591-3 </unstructured_citation></citation><citation key="ref13"><unstructured_citation>Galbraith, H., et al. (2010). "Effects of Future Sea Level Rise on Coastal Habitat." Journal of Coastal Research. DOI: 10.2112/JCOASTRES-D-10-00076.1 </unstructured_citation></citation><citation key="ref14"><unstructured_citation>Goelzer, H., et al. (2020). "The Impact of Greenland and Antarctic Ice Sheet Melt on Future Sea Level Rise." Science Advances, 6(51), eaaz5845. DOI: 10.1126/sciadv.aaz5845 </unstructured_citation></citation><citation key="ref15"><unstructured_citation>Gregory, J.M. et al. (2012). Twentieth-Century Global-Mean Sea Level Rise: Is the Whole Greater than the Sum of the Parts? J. Climate. DOI: 10.1175/JCLI-D12-00319.1 </unstructured_citation></citation><citation key="ref16"><unstructured_citation>Hanna, E., et al. (2024). "Short- and Long-Term Variability of the Antarctic and Greenland Ice Sheets." Nature Reviews Earth &amp; Environment, 5, 17-29. DOI: 10.1038/s43017-023-00509-7 </unstructured_citation></citation><citation key="ref17"><unstructured_citation>Hay, C.C., et al. (2015). "Probabilistic Reanalysis of TwentiethCentury Sea-Level Rise." Nature Climate Change, 5, 937-941. DOI: 10.1038/nclimate2635 </unstructured_citation></citation><citation key="ref18"><doi>10.1029/2008gl033459</doi><unstructured_citation>Hill, A. E., Brown, J. M., &amp; Fernando, L. (2008). Thermohaline circulation of shallow tidal seas. Geophysical Research Letters, 35(11). DOI: 10.1029/2008GL033459 . </unstructured_citation></citation><citation key="ref19"><doi>10.1016/s0278-4343(99)00026-6</doi><unstructured_citation>Huang, D., Su, J., &amp; Backhaus, J. O. (1999). Modelling the seasonal thermal stratification and baroclinic circulation in the Bohai Sea. Continental Shelf Research, 19(12), 1485-1505. DOI: 10.1016/S0278- 4343(99)00026-6 </unstructured_citation></citation><citation key="ref20"><unstructured_citation>Kopp, R.E., et al. (2020). "Regional Patterns and Impacts of Future Sea Level Rise: A Global Perspective." Nature Climate Change, 10, 101-107. doi: 10.1038/s41558- 019-0682-8 </unstructured_citation></citation><citation key="ref21"><doi>10.1029/2004gl021592</doi><unstructured_citation>Levitus, S., Antonov, J.I., &amp; Boyer, T.P. (2005). "Warming of the World Ocean, 1955-2003." Geophysical Research Letters, 32, L02604. DOI: 10.1029/2004GL021592 </unstructured_citation></citation><citation key="ref22"><doi>10.1029/2012gl051106</doi><unstructured_citation>Levitus, S., et al. (2012). "World Ocean Heat Content and Thermosteric Sea Level Change (0-2000 m), 1955-2010." Geophysical Research Letters, 39, L10603. DOI: 10.1029/2012GL051106 </unstructured_citation></citation><citation key="ref23"><doi>10.3390/s140305552</doi><unstructured_citation>Li, Z., Jiang W., Ding W., Deng L. &amp; Peng (2014). Estimates of Minor Ocean Tide Loading Displacement and Its Impact on Continuous GPS Coordinate Time Series. Sensors 14(3), 5552-5572; doi.org/10.3390/s140305552 </unstructured_citation></citation><citation key="ref24"><unstructured_citation>Miller, L., &amp; Douglas, B. C. (2007). "On the Rate and Causes of Twentieth Century Sea-Level Rise." Journal of Geophysical Research. DOI: 10.1029/2006JC003970 </unstructured_citation></citation><citation key="ref25"><unstructured_citation>Miller, L., &amp; Douglas, B. C. (2011). "Global Sea Level Rise." Journal of Coastal Research. DOI: 10.2112/JCOASTRES-D10-00072.1 </unstructured_citation></citation><citation key="ref26"><doi>10.1175/jpo3002.1</doi><unstructured_citation>Munk W &amp; Bills B. (2007). Tides and the Climate: Some Speculations. J. Phys. Oceanography. p.135-147; doi.org/10.1175/JPO3002.1 </unstructured_citation></citation><citation key="ref27"><unstructured_citation>Nerem, R.S., et al. (2021). "New Satellite Data Reveal Accelerated Sea Level Rise." Geophysical Research Letters, 48(3), e2020GL090551. DOI: 10.1029/2020GL090551 </unstructured_citation></citation><citation key="ref28"><doi>10.1017/cbo9781139235778</doi><unstructured_citation>Pugh, D. T., &amp; Woodworth, P. L. (2014). Sea-Level Science: Understanding Tides, Surges, Tsunamis and Mean SeaLevel Changes. Cambridge University Press. </unstructured_citation></citation><citation key="ref29"><doi>10.1126/science.1121381</doi><unstructured_citation>Rignot, E., &amp; Kanagaratnam, P. (2006). "Changes in the velocity structure of the Greenland Ice Sheet." Science, 311(5763), 986-990. DOI: 10.1126/science.1121381 </unstructured_citation></citation><citation key="ref30"><unstructured_citation>Rivera PC &amp; Khan TMA, 2012. Discovery of the major mechanism of global warming and climate change. J. Bas. Appl. Sci. Vol. 8, No.1. pp. 59-73. Doi:10.31219/osf.io/9r6gf </unstructured_citation></citation><citation key="ref31"><doi>10.52562/injoes.v2i1.331</doi><unstructured_citation>Rivera PC, 2022. Seismic-Perturbed Obliquity Change as a Discrete Trigger Mechanism of El Niño and La Niña Episodes. Indonesian Journal of Earth Sciences, 2(1), 51-63. doi: 10.52562/injoes.v2i1.331. </unstructured_citation></citation><citation key="ref32"><doi>10.5539/apr.v11n2p10</doi><unstructured_citation>Rivera PC. 2019. Gravitational Weakening of Seismic Origin as a Driving Mechanism of Some Astronomical Anomalies. App. Physics Res. Vol. 11, No. 2. doi:10.5539/apr.v11n2p10. </unstructured_citation></citation><citation key="ref33"><doi>10.31219/osf.io/vpcdj</doi><unstructured_citation>Rivera PC, 2011. Discovery of the major mechanism of global warming and climate change. Proceedings of the Global Conference on Global Warming. Lisbon, Portugal. July 2011. 10.31219/osf.io/vpcdj </unstructured_citation></citation><citation key="ref34"><doi>10.31219/osf.io/h3fau</doi><unstructured_citation>Rivera PC, 2006. Modeling the Asian Tsunami Evolution and Propagation with a new generation mechanism and a nonlinear dispersive wave model. Sci. Tsunami Hazards. Vol. 25, No. 1, pp 18-33. doi: 10.31219/osf.io/h3fau </unstructured_citation></citation><citation key="ref35"><unstructured_citation>Shepherd, A., et al. (2012). "A Reconciled Estimate of Ice-Sheet Mass Balance." Science, 338(6111), 1183-1189. DOI: 10.1126/science.1228102 </unstructured_citation></citation><citation key="ref36"><doi>10.1002/2015jc010716</doi><unstructured_citation>Visser, H., S. Dangendorf, and A. C. Petersen (2015), A review of trend models applied to sea level data with reference to the ''acceleration-deceleration debate'', J. Geophys. Res. Oceans, 120, 3873-3895, doi:10.1002/ 2015JC010716 </unstructured_citation></citation><citation key="ref37"><unstructured_citation>Vousdoukas, M.I., et al. (2020). "Projected 21st-Century Changes in Extreme Sea Levels Due to Sea Level Rise." Nature Communications, 11, 536. DOI: 10.1038/s41467-020-15752-5 </unstructured_citation></citation><citation key="ref38"><doi>10.3390/jmse10070984</doi><unstructured_citation>Wei X, Pan H., Xu T. Wang Y. &amp; Wang J. (2022). Development History of the Numerical Simulation of Tides in the East Asian Marginal Seas: An Overview. J. Mar. Sci. Eng. 2022, 10(7), 984; https://doi.org/10.3390/jmse10070984 </unstructured_citation></citation><citation key="ref39"><unstructured_citation>https://www.cmar.csiro.au/sealevel. Commonwealth Scientific and Industrial Research Organization, Australia. (Accessed in June 2024). </unstructured_citation></citation><citation key="ref40"><unstructured_citation>https://www.iers.org. International Earth Rotation Service (IERS), Paris, France. (Accessed in November 2024). </unstructured_citation></citation><citation key="ref41"><unstructured_citation>https://ngdc.noaa.gov. National Geophysical Data Center, National Oceanic and Atmospheric Administration. (Accessed in March 2015). </unstructured_citation></citation><citation key="ref42"><unstructured_citation>https://www.usgs.gov. United States Geological Survey. (Accessed in October 2017). </unstructured_citation></citation><citation key="ref43"><unstructured_citation>http://www.jgiesen.de/moon/FullM oon/index.html. Accessed in September 2013) </unstructured_citation></citation><citation key="ref44"><unstructured_citation>Hofmeister et al. (2022). A New Mechanism for Plate Tectonics Based on Gravitational Torques that Explains Differences among Rocky Planets. Proc. 53rd Lunar and Planetary Science Conference. USA.</unstructured_citation></citation></citation_list></journal_article></journal></body></doi_batch>