Why is sea level rise worse in some places?
nautil.us
nautil.us
https://tidesandcurrents.noaa.gov/sltrends/
Sea levels have been monitored for over 100 years... because of commerce.
East coast US seems to be going up about 3mm/year, or a foot per century. That's on top of 7 foot tides.
West coast US is very steady, barely moving at all.
The sea level is dropping in Alaska by 10mm/year. Dropping in Scandinavia also.
Some cities show rising sea levels, but really the cities are sinking due to collapsing aquifers; New Orleans and Bangkok. And measurements made on river deltas are always going to be wild due to silt and all.
Most notably, I can't find an example in the NOAA data of the rate of sea level rise increasing due to industrialization. Anybody?
Because the sensors are mounted on that very land.
So tectonic movement will certainly have an effect. And you can see remnants of earthquakes in some of the data.
https://en.wikipedia.org/wiki/Last_Glacial_Period#Weichselia...
> As a result of melting ice, the land has continued to rise yearly in Scandinavia, mostly in northern Sweden and Finland, where the land is rising at a rate of as much as 8–9 mm per year, or 1 m in 100 years. This is important for archaeologists, since a site that was coastal in the Nordic Stone Age now is inland and can be dated by its relative distance from the present shore.
Don't know if local variations in gravity may have a measurable impact?
They've (NGS) been flying absolute gravity measurement equipment in planes with precision GPS and lidar since ~2005 as part of the GRAV-D program.
Additionally, slight 'variations' (ie deviations from the expected circular/elliptical) in the orbits of GPS satellites can be used to infer slight variations in the gravity below.
Separately, the military likely has had all of this measured and modeled for decades as part of ballistic missile targeting, but remains mostly classified at useful resolutions.
The transitions from NGVD27 to NAVD88 to the work-in-progress 22 datum is exactly because the idea of a simple "universal" sea-level doesn't exist in the manor you would expect it to.
But even with the GRAV-D based datums, the actual observed water levels will occur at slightly different datum heights in different locations, for various geophysical reasons.
Another reason (but not due to weather) is that when land somewhere goes up, it will displace water everywhere else. And so, for example, if the land is still recovering from the ice age we should see ocean levels going up everywhere except for the pieces of land that are recovering from the weight of the glacier that is no longer there.
Mind that Arctic is not causing sea level rise. Any ice that is floating on water will not cause any water level change when it melts. (I know this is somewhat unintuitive but it comes directly from Archimedes principle)
So we are talking basically Antarctic ice and Greenland because these are by far the largest bodies of frozen water that are supported by land rather than floating on the ocean.
I think it should be pretty easy to observe how much of that water melted or slipped into the sea.
I also think that currently, coastal erosion is mostly caused by changing weather patterns. Basically this comes down to wind blowing in different directions, speed and variety and these changing patterns mean coasts are eroding in different places than before.
https://www.jpl.nasa.gov/edu/learn/project/how-warming-water....
First of all, most of the temperature rise only happening close to the surface with average surface temperature rise being only about 1.5F or 1C since 1901.
This article says deep ocean water is projected to warm up by only 0.2C during next 50 years: https://www.openaccessgovernment.org/deep-ocean-warming-subt...
Furthermore, at around 4C which is what deep ocean water is close to (everything below 200m is essentially 4C), thermal expansion is almost nil. For colder water thermal expansion is actually negative.
4C is when water is at its densest. It is not an accident that all oceans are 4C, because 4C water sinks to the bottom and anything colder or hotter than 4C floats up. This remarkable property of water is what causes even shallow water to be fantastically stable in temperature -- a lake that has more than couple tens of meters in depth is likely to be 4C at the bottom throughout the year whether it is frosty winter or hot summer above it, unless some kind of powerful event is able to mix the water in the lake.
Now, the small temperature differences will definitely have outsize effects on water circulation, ocean currents, life and weather. But I doubt they will cause meaningful sea rise unless somebody can calculate otherwise?
Plenty of people have, in fact, calculated otherwise.
Roughly half of the current, ongoing sea level rise is from expansion of water. The effect is small, but there is a lot of water that is expanding.
Question: How does the salinity and pressure of deep sea water affect that 4C point?
The important thing to remember is even a 1 part in 1,000 decrease in density * 2km of depth = 2m of expansion. Ballpark estimates aren’t enough you really need fairly detailed simulations to get any significant accuracy. Actually doing such simulations shows meaningful sea level rise from thermal expansion at ~0.07 inches per year or roughly half the current rate of increase. This might not sound like much, but consider that volume of sand you need to replace to maintain beaches etc etc.
No, that is mostly inaccurate. Thermal expansion is small, but there is an awful lot of water. As you point out yourself, thermal expansion contributes about half the sea level rise. Oceans absorb energy just like the atmosphere does and this effect has been known for quite a while (e.g. https://www.nature.com/articles/330127a0 ).
Thermal expansion of surface water is not negligible.
Not to rant but this is one of those threads again. The majority of comments contain misinformation.
Ice is about 91% the density of water. If you have water at 0 height, and you put in water equivalent to +1 unit of height. If it's in liquid form, obviously height goes up by +1. If it's in ice form, there is +1.09 height worth of ice (because it expands when it freezes), but it only displaces water up to +1 unit of height in order to support its weight through buoyancy. The overall change in height is +1 unit regardless of whether it's liquid or ice
You can fill a glass of ice-water right up to the brim, and it won't spill over as the ice melts. But only if the ice is floating in the water. It's because the ice's mass pushes down on the liquid water, displacing a fixed amount relative to the weight of the ice.
You can look at the graph on the NOAA site here and see the acceleration visually: https://www.climate.gov/news-features/understanding-climate/...
The notes to the left of the table say 1.4mm/yr for much of 20th Century to 3.6mm/yr now.
There is also evidence of acceleration of sea level rise just from satellite data, 0.08mm/y^2:
https://www.sciencedaily.com/releases/2018/02/180212150739.h...
So after roughly 100 years, we can look forward to the terrible catastrophe of sea levels (in some places only, not in others) rising by.. just over a foot. A problem for many really flat coastal areas, sure, but hardly the picture of global coastal flooding much of the alarmism has put forward. And if that one-foot rise happens across a full century, there will be many measures that can be taken to counter it even if the rise itself is unstoppable.
I'm not arguing against human-caused climate change, but some of the hyperbole i've seen said with deep certainty goes well beyond the scope of known evidence, realized events or even many scientific assessments.
With such things, it's not hard to see why some people find good reasons for being skeptical of yet another worst-case prediction.
Subsidence is a thing in Silicon Valley. San Jose has sunk some feet since the aquifer was drawn, fist for agriculture and now urbanization.
Also that assumes the scientists are completely accurate and don't make any mistakes. As recently as 5 years ago they discovered that the measured rise for almost all of the 90s was wrong and revised it by 3mm/year +- 1.7mm/year - the error was the same amount as the imputed level of rise!
This is no knock on the scientists, because measuring the height of a moving ocean from orbit to a level of accuracy that lets you see mm level changes is inevitably going to be very hard. But we should bear in mind that they're heavily biased towards wanting to believe the data is accurate. Their decade long inability to get the measurements correct didn't seem to have any impact on their confidence that they're currently getting it right, and why would it? Those who seize the data, seize the day.
Citation for this? There are always improvements to our understanding of past data, but you seem to be implying that the uncertainty exceeds the signal. That's simply not the case [1].
[1] — https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6... pp.1291-1292
They have shown that there was a drift in the GMSL record over the period 1993-1998. This drift is caused by an erroneous on-board calibration correction on TOPEX altimeter side-A (noted TOPEX-A). TOPEX-A was operated from launch in October 1992 to the end of January 1999. Then TOPEX side-B altimeter (noted TOPEX-B) took over in February 1999 (Beckley et al., 2017). The impact on the GMSL changes is -1.0 mm/yr between January 1993 and July 1995, 120 and +3.0 mm/yr between August 1995 and February 1999, with an uncertainty of ±1.7 mm/yr (within a 90%CL, (Ablain, 2017)).
https://essd.copernicus.org/articles/11/1189/2019/essd-11-11...
Yes they did. From the paper I just cited:
The six main groups that provide satellite-altimetry-based GMSL estimates (AVISO/CNES, SL_cci/ESA, University of Colorado, CSIRO, NASA/GSFC, NOAA) use 1 Hz altimetry measurements from the T/P, Jason-1, Jason-2 and Jason-3 missions from 1993 to 2018 (1993–2015 for SL_cci/ESA). The differences among the GMSL estimates from several groups arise from data editing, from differences in the geophysical corrections and from differences in the used method to spatially average individual measurements during the orbital cycles
The apparently independent time series are actually computed from the same raw data sources, as there isn't an abundance of redundant satellites measuring sea level.
But isn't this goalpost shifting? At first you said I was wrong that uncertainty has been the same size as the measurements in the past, citing the IPCC as proof which of course doesn't mention any of this, saying only that they have high confidence in these numbers (the IPCC is not trustworthy). Then it became that the error isn't big enough for you, and nobody relied on a single satellite. Now I show that they did indeed rely on a single satellite.
The core issue here remains the same: how do they know they're getting it right now? A calibration error so large it invalidated their entire time-series lasted for the entire lifetime of the TOPEX-1 mission, and it then took 20 years for the problem to actually be detected and corrected for. They've only been measuring sea level with satellites for 30 years, and the discrepancy between tide gauges and satellites has never been properly reconciled even though they theoretically measure the same thing.
As you quoted from the paper:
> The six main groups that provide satellite-altimetry-based GMSL estimates ...
1) You're restricting your attention to groups producing satellite-derived estimates.
2) Several of those groups, e.g. CSIRO, are using data assimilation to combine satellite estimates with gauges [1].
3) There are multiple satellites, often overlapping in time, often of totally different design/orbit/etc... [2]
4) Up to the most recent IPCC report (AR6), assessments were based on tide gauges alone [3]. For many of the reasons that you bring up. Hence "Nobody relies on estimates from a single satellite alone." Reconstruction of historical sea level is a huge scientific discipline and you would benefit from doing some more reading before beating a dead horse. The estimated uncertainty is large for a reason, but it does not encapsulate any scenarios where the observed change has been insignificant. If you think otherwise, I'd be happy to take your money for 2100 options on coastal real estate in about 90% of the world's coastline.
[1] — https://research.csiro.au/slrwavescoast/sea-level/measuremen... and https://link.springer.com/article/10.1007/s10712-011-9119-1
[2] — https://research.csiro.au/slrwavescoast/sea-level/measuremen...
[3] — https://www.ipcc.ch/report/ar6/wg1/downloads/report/IPCC_AR6... p.1287
- Uncertainty exceeding signal in satellite data is "simply not the case"
to
- OK maybe it was the case but it doesn't matter and nobody relies on one satellite anyway
to
- OK maybe some groups relied on one satellite but this is flogging a dead horse everyone already knows about
That's a big distance in a short thread! Also, note that you said "nobody relies" and now you're arguing "not everyone relies", which is different.
I won't be alive in 2100 but if you've got some nice seafront property you'd like to sell me below market price I'd definitely consider it. Maybe in Tuvalu? (see other post).
Not sure I can help someone who willfully misreads my comments! Give chapter 9 of the AR6 a read and then we can talk.
https://sealevel.colorado.edu/index.php/presentation/what-gl...
currently some land surfaces are rising and some ocean bottoms are falling relative to the center of the Earth (the center of the reference frame of the satellite altimeter).
since the ocean basins are getting larger due to GIA, this will reduce by a very small amount the relative sea level rise that is seen along the coasts.
We apply a correction for GIA because we want our sea level time series to reflect purely oceanographic phenomena. In essence, we would like our GMSL time series to be a proxy for ocean water volume changes. This is what is needed for comparisons to global climate models, for example
This is nonsense, of course. Volume isn't measured in millimeters, that's a measurement of distance. GMSL when talking about satellites is defined as the average distance of the surface of the ocean from the center of the Earth, and the reason people care about it is because if it gets too high then things we care about end up flooded. Changing the definition of GMSL half way through from sea level to sea depth is the kind of slippyness that pervades this space.
That's the average rise it you average all data going back to the 1950s.
Unfortunately, looking back to the 50s is only really useful if interested in how much sea levels have already risen. Otherwise it presents an unrealistically optimistic view, as the rate has accelerated since.
Per the article, the east coast (North Carolina) is currently experiencing an increase of about a third of an inch per year, which is an increase of one foot per 36 years, or close to a meter per century.
If current trends continue, this will accelerate, not decelerate.
https://www.theguardian.com/environment/ng-interactive/2018/...
On the other side, a lot of land is sinking because the soil is drying out due to years of droughts and water mismanagement (farmers like to keep the water table lower. I live in NL where we have the water management infrastructure to tweak the water table)
Shockingly fast, too, in some spots.
https://www.nytimes.com/2021/05/25/us/corcoran-california-si...
"Over the past 14 years, the town has sunk as much as 11.5 feet in some places..."
If you look at the "NOAA Tides and Currents" data, and go to Maryland, and click two points across the Chesapeake bay from each other. Go to More Data > Datum, you can see just across a 20 mile stretch of bay, Bishops Head MD MHHW (Mean Higher High Water, when there are two daily high tides, this is the elevation of the higher of the two) is 2.06 Feet over the vertical datum, while 20 miles away at Solomons Island MD it's a half foot lower, 1.48 Ft.
Water density table - https://www.usgs.gov/special-topics/water-science-school/sci...
If the temperature of the ocean changed by 10°F that would result in a .1% change in overall volume. Obviously that does make a difference because the ocean is so big, but it's a lot less consequential than ice, which is above the water, melting into the water and ice.
Of course, if the ice is on land and melting into the ocean, that's different.
https://nsidc.org/news-analyses/news-stories/melting-floatin...
My understanding is that water expands quite a bit less in the range between 32°F and 212°F than it does when it freezes.
It seems like floating ice melting and decreasing in volume 9% is notably more significant than the volume increase from a couple degree temperature increase. There also certainly way more liquid water than solid to contend with.
I'd be curious to know the effect of melting ice decreasing the volume versus the temperature rising increasing the volume.
That's part of the runaway effect we are freaked out about.
1. Global temperature is rising. Any water that used to be above 4°C (or the equivalent for salt water) now takes more volume. But what about water that's below 4°C? Wouldn't that water compress? What portion of the ocean is colder than 4°C? I'd imagine all of the Arctic zone and near Antarctica is, which is an awful lot of water to offset the tropical water. An even more nuanced perspective would be to look at the actual temperature distribution and use it to weight the dV/dT of water at different temperatures.
2. Global temperature is rising. Ice is melting into water. This is new mass entering the ocean. Why can't the sea bed, which is under more pressure due to extra mass, expand? The sea bed isn't a steel utensil, it's sand and rocks. And it's constantly shifting. And it's composition is different in different regions.
Has anyone done a detailed computer simulation of the whole earth's geology under rising temperatures? There might be feedback loops that might amplify or negate some effects so it's quite important to account for all variables. And obviously there's a lot of variables to account for.
(It's sometimes scary how little we know about our own planet. I'm not talking about the things in my comment because I'm sure it's just my ignorance.)
It might marginally, but the amount of water compressed will be a lot smaller than the amount of water "uncompressed", both due to the larger range of temperatures above 4°C (below is only a bit, and then ice) and due to the fact that the densest water is at the bottom, meaning that it's easier for everything else to heat up.
> 2. Global temperature is rising. Ice is melting into water. This is new mass entering the ocean. Why can't the sea bed, which is under more pressure due to extra mass, expand?
Expand where? It can't just rise since there is gravity, and the pressure above increases with more water. It can't go down because there is already other stuff there.
Think of the ocean bed as a trampoline. Obviously much more rigid, but that's the image in my head.
>It can't go down because there is already other stuff there.
Why not? Rocks and sand can be compressed with sufficient pressure.
You say it because of the extra volume on top of it?
If that's the case, not because of heating. The volume increases, the water still weights the same.
(Note that the 4°C number is only for pure water.)
> water still weights the same
Weight has nothing to do with my first point. It's the increase in volume that spills into land.
But well, water being water, I imagine this doesn't happen at pressure; just for surface water. Is that the case?
It's incredibly expensive though.
Scott Alexander estimated it would "reverse one year worth of global-warming induced sea-level rise" here: https://slatestarcodex.com/2016/04/15/links-416-they-cant-li...
We are depleting our aquifers at a rate of about 280 km^3 per year. US is down over 1000 km^3 since ~1900. I'm not sure how much of that ends up in the ocean, but reducing that number and taking it negative would go a long way toward slowing sea level rise.
I guess depleting aquifers can lower land levels in those areas. I hear Jakarta has sunk 4 meters from that effect. But it's a separate thing from rising sea levels.
That doesn’t sound right. I think it is common knowledge that water expands as it freezes (hence, burst pipes), not when it warms up.
https://www.usgs.gov/special-topics/water-science-school/sci...
Ice in water doesn't change the waters height. If you put an ice cube in a cup, the water will be the same height after the ice has melted [1], since the "excess" is lifted out of the water. For some numbers, in 2020, it looks like total sea ice peaked at 18,785 km3, with the oceans volume being 130,000,000, so 0.014% [2].
The thermal expansion of water, as liquid form, is going to be much more important [3].
Related, every time I try to look into climate numbers, I get the sense that there's a gap between grade school explanations and research papers. There's not much between. Asking ChatGPT just reinforces this view. It treats me like a kid, or wraps unsolicited disclaimers/summaries around everything.
1. https://physics.stackexchange.com/questions/110645/why-does-...
2. https://arctic.noaa.gov/Report-Card/Report-Card-2020/ArtMID/...
3 https://physics.stackexchange.com/questions/506759/how-much-...
Re the tides: when Charles ame Diana visited NB in 1983, they disembarked at high tide in the Saint John harbour. The gangplank was at about 45 degrees, slopes down to the dock. A few hours later, it was 45 degrees down to the royal yacht. Some of the sailors, many of whom had long experience, having served in the falklands, among other places, had never seen anything like it.
The amount of water that comes in an out twice a day is, well, nuts. Yes, that's the technical term.
(Summer ferry crossings between Digby Neck and Saint John are 2.5 hours, 3.0 hours in the winter (slower due to rougher water), but I do know people who took ~12 one February: the water was so rough they hugged as close to the shores of NB and NS as they dared, just to make things a little calmer. There have also been cases of transport trailers falling over in the hold. Yes, they were lashed down.)
(I once spent a terrible several hours sprawled on a lounge chair staring out the window on the opposite side of the boat: For seven seconds I could see nothing but sea, the ship swung, and for seven more, nothing but sky. Repeat. Ad nauseam. The swings took about a second. When I finally did get up to head to the heads to unload that nausea, let's just say planning was involved in every step.)
(Another trip, I also spent an uncomfortable few minutes on the observation deck bow-ward of that lounge, because young and dumb: It was fall, I was heading back to Uni, it was cold (duh), I was wearing a hoodie and shorts, and I'd stepped out for fresh air. Got talking to American tourists in long slacks and sweaters. Felt expansive and loquacious, kept them out there as long as I could. They finally excused themselves on account of the cold, very polite, and I turned to and leaned upon the bow rail until I felt enough time had gone by that I could return to the lounge. Man, it was cold. Ah, youth. :->)
Also mentioned by Tom Scott: https://www.youtube.com/watch?v=nCrTsWtPVIY
Hey; if they can handle 52ft tides, they can handle anything.
In my experience, the first order adjustment effects are not widely known even among physical oceanographers. I remember describing it to a preeminent expert on El Nino, and him being incredulous that local sea level fall near the source of meltwater could be the first-order effect beyond accounting for rebound. "The first-order response is a Kelvin wave — you've surely been misinformed."
[1] - One example lecture: https://www.youtube.com/watch?v=s_rGksRoG9A
[2] - Another, shorter summary talk https://www.youtube.com/watch?v=yj7JIxU9Af4
But they are generally rising, just not more than compared with pre-industrial era.
A best you could say "a few, in areas that are losing glaciers, which is expected due to basic physics"
Fun fact: the slowest its been in the last century was when we did a crap-ton of dam projects in the 50s-70s, still rose, but very little.