- For the effects of global warming on sea levels, see global warming
The sea level is the average height of the ocean (informally called the sea). The word 'average' must be used because the height of the sea changes with the tides. The height of mountains, countries, and so on, is almost always given as "above sea level".
Technical details[change | change source]
MSL is a type of standardised geodetic reference point. It is used, for example, as a geodetic datum in cartography and marine navigation. In aviation it is the standard sea level at which atmospheric pressure is measured. This is used to calibrate altitude, which influences aircraft flight levels. A common mean sea-level standard is the midpoint between a mean low and mean high tide at a particular place.
Sea levels can be affected by many factors. They have varied greatly over geological time scales. The careful measurement of variations in MSL offers insights into ongoing climate change. The present slight rise in sea levels is offered as proof of ongoing global warming.
Long-term changes in sea level[change | change source]
In Earth's long history, the continents and sea floor have changed due to plate tectonics. This affects global sea level because it alters the depths of various ocean basins, and also changes the distribution of glaciers.
Over most of geologic time, the long-term mean sea level has been higher than today (see graph). Only at the Permian-Triassic boundary ~250 million years ago was the long-term mean sea level lower than today. This included the Permian–Triassic extinction event, though this may not be relevant to the concept of sea level.
Rapid changes in sea level[change | change source]
Rapid changes may happen by huge lakes breaking through into seas. This has happened on a number of occasions. When the latest ice age was ending, melting caused huge lakes in central North America. This eventually broke through into the Atlantic. Melting ice in the North Sea are also broke through into the English Channel. The largest known example of marine flooding was when the Atlantic breached the Strait of Gibraltar about 5.2 million years ago. This restored Mediterranean sea levels, which had dried up.
References[change | change source]
- What is "Mean Sea Level"? (Proudman Oceanographic Laboratory).
- Solomon et al 1997. Technical Summary, Section 3.4 Consistency among observations Archived 2018-11-02 at the Wayback Machine in IPCC AR4 WG1 2007 harv error: no target: CITEREFIPCC_AR4_WG12007 (help); Hegerl et al., Executive summary, Section 1.3: Consistency of changes in physical and biological systems with warming Archived 2017-05-14 at the Wayback Machine in IPCC AR4 SYR 2007 harv error: no target: CITEREFIPCC_AR4_SYR2007 (help).
- Müller, R. Dietmar 2008.; et al. "Long-term sea-level fluctuations driven by ocean basin dynamics". Science. 319 (5868): 1357–1362. Bibcode:2008Sci...319.1357M. doi:10.1126/science.1151540. PMID 18323446.
- Gautier F. et al 1994. Age and duration of the Messinian salinity crisis. C.R. Acad. Sci., Paris (IIA) 318, 1103–1109.
- Krijgsman W. et al 1996. "A new chronology for the middle to late Miocene continental record in Spain". Earth and Planetary Science Letters. 142 (3–4): 367–380. Bibcode:1996E&PSL.142..367K. doi:10.1016/0012-821X(96)00109-4. Retrieved 2008-03-01.
- GRID-Arendal. "Climate change 2001: the scientific basis. Can 20th century sea level changes be explained?". Archived from the original on 2011-05-14. Retrieved 2005-12-19.
Other websites[change | change source]
- Flooding, food and climate change in Bangladesh
- Sea level rise - How much and how fast will sea level rise over the coming centuries? Past Archived 2012-11-09 at the Wayback Machine
- Sea level rise - How much and how fast will sea level rise over the coming centuries? Present Archived 2012-11-09 at the Wayback Machine