Comments by "" (@pwillis1589) on "‘Climate change’ now means rather than dams dying up they will be ‘really wet’" video.

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  2. Sea level is the base level for measuring elevation and depth on Earth. Because the ocean is one continuous body of water, its surface tends to seek the same level throughout the world. However, winds, currents, river discharges, and variations in gravity and temperature prevent the sea surface from being truly level. So the surface of the ocean can be used as a base for measuring elevations, the concept of "local mean sea level" has been developed. In the United States and its territories, local mean sea level is determined by taking hourly measurements of sea levels over a period of 19 years at various locations, and then averaging all of the measurements. The 19-year period is called a Metonic cycle. It enables scientists to account for the long-term variations in the moon's orbit. It also averages out the effects of local weather and oceanographic conditions. Sea level is measured in relation to the adjacent land. Just like the ocean, the elevation of land may rise and fall over time. For example, the tremendous weight of a glacier on land pushes the land down, closer to sea level. That same land bounces back (a process called postglacial rebound) if the ice retreats, or melts, and its weight is removed. Local mean sea-level measurements are a combination of sea-level variations and movement of the land. Again I hope this helps as this is common public knowledge. If you wish, I could reference you thousands of published peer reviewed scientific papers that show this is an observable phenomenon. Or remain ignorant,your choice.
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  9.  @chrismo2922  Average global sea levels have been rising since 1880 (the earliest available robust estimates), largely in response to increasing concentrations of greenhouse gases in the atmosphere and the consequent changes in the global climate. Global average sea levels have risen by around 25 cm since the late 19th century. Half of this rise has occurred since 1970. There are two main processes behind long-term sea-level rises that are a direct result of a warming climate. Firstly, as the ocean has warmed, the total volume of the ocean has increased through the thermal expansion of water. Thermal expansion has contributed about one third of the sea-level rise observed globally. Secondly, water has been added to the oceans as a result of melting land-based ice. Ice loss from glaciers and polar ice sheets, together with changes in the amount of water stored on the land, contribute two thirds of global sea-level rise. The rate of sea-level rise since the mid-19th century has been larger than the average rate during the previous 2,000 years. Global-average sea levels are currently (from 1993 to 2019) rising at around 3.5 mm per year, faster than the 1.5 mm per year during the 20th century. Rates of sea-level rise are not uniform around the globe and vary from year to year. Since 1993, the rates of sea-level rise to the north and southeast of Australia have been significantly higher the global average, and rates of sea-level rise on other coasts of the continent have been closer to the global average. Melting ice from Greenland, Antarctica and glaciers due to anthropogenic climate change has been the main cause of global sea-level rise since the early 1990s. Natural variability of the climate system also contributes to variations in sea level. For example, global sea level fell during the intense La Niña event of 2010–2011, partly due to the exceptionally high rainfall over land that resulted in floods in Australia, northern South America, and Southeast Asia. This was compounded by the long-term storage of water across inland Australia. However, recent observations show that sea levels have rebounded in line with the long-term trend in rising sea levels.
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