Have I made this too difficult for WouldBe to understand? Do you think he is being deliberately obstuse?
originally by tangentlama said:
- Tectonic uplift - changes in ground levels caused by tectonic plate movement
- Melting of non-polar ice (i.e. ice on the land) which causes isostatic uplift
- Isostatic uplift (glacial rebound) - rise in level of land caused by loss of mass in land glaciers that result in one land region to rise and another to be pushed down.
- Melting/freezing of ice-caps in Antarctic/Greenland
That affects land level
not sea level.
!!!
Oh dear. You have a broken packet again.
If the land level rises due to isostatic uplift (through glacial rebound and tectonic activity the land is pushed up or down) then the Local Mean Sea Level (LMSL - see 1) in sea-level glossary below) will change, because the land-benchmark which we measure 'sea level' against will have changed.
Your original question, based on the premise that 'water finds it's own level', was:
WouldBe said:
Water finds it's own level so how the hell can you have an uneven sea level rise around the globe?
I explained in post 725 how we can have an uneven sea level rise around the globe, but you've then stated :
That affects land level not sea level.
I've already described to you the many ways in which variations of sea-level occur.
I've now requoted my original post below, and added disambiguations.
Furthermore, the measurement known as 'sea level' (at zero metres) is relative:
1) Local Mean sea level: (LMSL) the height of the surface of the sea in relation to a land-benchmark.
2) Mean Sea level: (MSL) the height of the surface of the sea above which the heights of geographical features are measured. Mean sea level (MSL) is calculated from the average level of the sea between high and low tide.
3) Sea level: the base point against which land elevation and sea depth are measured; the height of the land above the sea.
4) Eustatic sea level: Global sea level can alter in the ways listed in the list I gave you (see below for repeat list where 'eustatic' has been added for disambiguation, and salinity has been added as an additional cause of sea-level change). Eustatic levels are influenced by: a) temperature (volume of sea dependent on sea temperature); b) mass of water on land i.e rivers, lakes, glaciers, ice-caps, sea-ice; plus c) changing shape of oceanic basins due to tectonic activity
6) Local/regional sea level: local sea level can alter in all the ways listed in above with the addition of a) salinity changes.
Of course, a rise in sea level will still make the mean sea level (MSL) at 0 metres, because we measure sea level as relative to the mean level (i.e. between high and low tide) as it touches landmass.
However, the coastal land that sinks below sea level or is submerged by a volume increase in the local ocean will fall below sea level.
If you want to read more:
Steric sea level :
http://www.google.com/search?hl=en&q=Steric+sea+level&btnG=Search
Eustatic sea level:
http://www.google.com/search?hl=en&q=Eustatic+sea+level&btnG=Search
Remember - sea level change is relative
Here's the disambiguated list:
Sea level is not globally uniform.
Sea level variations and changes are caused by:
- Thermal expansion/contraction of regional oceans (oceanic temp changes) [Disambiguation: Steric]
- Ocean basins changing size due to tectonic activity along ocean ridges [Disambiguation: Eustatic] and sediment transfer from land to ocean [Disambiguation: Isostatic]
- Tectonic uplift - changes in ground levels caused by tectonic plate movement [Disambiguation: Isostatic]
- Melting of non-polar ice (i.e. ice on the land) which causes isostatic uplift [Disambiguation: Isostatic (land uplift) and Eustatic (ice-melt water added to ocean)]
- Isostatic uplift (glacial rebound) - rise in level of land caused by loss of mass in land glaciers that result in one land region to rise and another to be pushed down. [Disambiguation: Eustatic (glacial melt entering ocean) and Isostatic (land uplift)]
- Melting/freezing of landmass ice-sheets, e.g. ice-caps in Antarctic/Greenland, continental ice-sheets, glaciers [Disambiguation: Eustatic, Hydroisostatic]. Ice lost to ocean results in depression of oceanic crust. Ice gone from land results in isostatic uplift (land rise). This creates global sea level change AND local sea level change
- Changes in salinity [Disambiguation: Steric]
Some of the changes in that list affect global sea levels, others affect local sea levels.
NB: I won't claim that the list above is all the reasons for changes in sea level at local and global levels.
If you want to read more, search for 'eustatic sea level' and 'local sea level'
e2a: This is a fairly easy to understand exposition:
http://geology.uprm.edu/Morelock/eustatic.htm